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1999 Pacific typhoon season

The 1999 Pacific typhoon season was the last Pacific typhoon season to use English names as storm names. It was a very inactive season, featuring the lowest number of typhoons on record, five. It had no official bounds; it ran year-round in 1999, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.

1999 Pacific typhoon season
Season summary map
Seasonal boundaries
First system formedJanuary 3, 1999
Last system dissipatedDecember 16, 1999
Strongest storm
NameBart
 • Maximum winds165 km/h (105 mph)
(10-minute sustained)
 • Lowest pressure930 hPa (mbar)
Seasonal statistics
Total depressions45
Total storms20
Typhoons5 (record low)
Super typhoons1 (unofficial)
Total fatalities976
Total damage$18.36 billion (1999 USD)
Related articles
Pacific typhoon seasons
1997, 1998, 1999, 2000, 2001

Tropical Storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. Tropical cyclones that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.

Season summary edit

Typhoon Bart (1999)Tropical Storm YorkTropical Storm Wendy (1999)Hurricane Dora (1999)Tropical Storm Sam (1999)Typhoon Olga (1999)Typhoon Maggie

Systems edit

In the storm information below, the Joint Typhoon Warning Center (JTWC) wind-speed advisories differ than that of the Japan Meteorological Agency (JMA) because the JTWC uses the United States criteria of 1-minute sustained winds to designate a tropical cyclone's maximum sustained winds, whereas the JMA uses 10-minute sustained winds to determine maximum sustained winds. Consequently, in most cases, the JTWC maximum winds for a cyclone appear higher than the JMA's estimated maximum winds for the same system.

Tropical Depression Hilda (Auring) edit

Tropical depression (JMA)
Tropical storm (SSHWS)
   
DurationJanuary 3 – January 8
Peak intensity55 km/h (35 mph) (10-min);
1000 hPa (mbar)

The JTWC issued a Tropical Cyclone Formation Alert (TCFA) for a developing broad circulation that stretched out from the northwest Borneo coast early on January 4. This developed into a tropical depression and moved slowly to the north away from Borneo, becoming Tropical Storm Hilda early on January 6. Soon after reaching its peak strength of 65 km/h (40 mph) Hilda drifted further north into an area of increased wind shear, which caused the storm to dissipate the next day.[1] Both JMA and PAGASA tracked this system, but considered it a tropical depression. PAGASA named the storm Auring.[2]

Malaysia reported to the World Meteorological Organization (WMO) Typhoon Committee that Tropical Storm Hilda brought heavy rain to Sabah. The rain caused flooding and landslides, and was responsible for five deaths.[3] The mudslides caused about $1.3 million in damage (1999 USD, 15 million 1999 MYR) to roads throughout the country.[4]

Tropical Depression Iris (Bebeng) edit

Tropical depression (JMA)
Tropical storm (SSHWS)
   
DurationFebruary 14 – February 19
Peak intensity55 km/h (35 mph) (10-min);
1000 hPa (mbar)

A monsoon depression began to develop between Pohnpei and Chuuk on February 10 as it moved west.[5] The JTWC issued a TCFA as the depression formed and passed near Palau on February 13. The storm slowly consolidated as it moved towards the Philippines, becoming Tropical Storm Iris on February 17, but did not intensify any further. As the storm turned northwards under the influence of a subtropical ridge to the east it entered a high shear environment and rapidly degenerated, dissipating on February 19 220 km (140 mi) to the east of Luzon.[6]

PAGASA considered this storm to have been a tropical depression and named it Bebeng.[5]

Tropical Depression Jacob (Karing) edit

Tropical depression (JMA)
Tropical storm (SSHWS)
   
DurationApril 6 – April 9
Peak intensity55 km/h (35 mph) (10-min);
1006 hPa (mbar)

A low pressure area 220 km (140 mi) to the west of Yap developed into a tropical depression on April 6. It gradually developed as it moved to the west, becoming a strong depression with 55 km/h (34 mph) winds. It then began to accelerate to the northwest, becoming a minimal tropical storm as it did so. However, this northwards motion brought it into a region of increased shear, which weakened it back into a tropical depression. The low level circulation became completely exposed and the weakening system made landfall on southern Luzon on April 10.[7] PAGASA named the system Karing and considered it a tropical depression.[8]

The rainfall from Jacob ranged from 80 mm (3.1 in) up to 400 mm (16 in) in some places in the Philippines, but only minor damage was recorded on land.[9]

Severe Tropical Storm Kate (Diding) edit

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
   
DurationApril 21 – April 28
Peak intensity100 km/h (65 mph) (10-min);
980 hPa (mbar)

On April 22, a tropical disturbance which had developed in the Philippine Sea moved over Mindanao and intensified into a tropical depression whilst it was still overland. The depression soon moved overwater again as it tracked north to the east of the Philippines, becoming Tropical Storm Kate the next day. The JTWC initially forecast that the storm would only intensify slightly, as they predicted it to move north-northeast into an unfavorable environment. However, Kate instead moved on a more northerly route and entered an area with minimal wind shear. On April 26 Kate became a typhoon, the first of the season, and reached its peak strength with 140 km/h (87 mph) soon after. Later that day, the typhoon's motion accelerated to the northeast and it passed 9 km (5.6 mi) to the north of Iwo Jima. Kate then began to lose its convection and became an extratropical on April 28 to the northeast of Iwo Jima.[10]

Both JMA and PAGASA considered Kate to have been a tropical storm at its peak, in both cases considering this the first tropical storm of the season. PAGASA named the depression Diding soon after it formed and upgraded it to a tropical storm before the JTWC.[8] Kate brought torrential rain to the east-central Philippines, with amounts as high as 360 mm (14 in) falling in places.[11] The peak winds recorded on Iwo Jima were 95 km/h (59 mph), with gusts of up to 126 km/h (78 mph).[12]

Typhoon Leo edit

Typhoon (JMA)
Category 3 typhoon (SSHWS)
   
DurationApril 27 – May 2
Peak intensity120 km/h (75 mph) (10-min);
970 hPa (mbar)

In late April a circulation began to develop within a monsoon depression in the South China Sea, forming into a tropical depression on April 27 when it was 710 km (440 mi) to the west of Manila. It strengthened as it moved to the west and became Tropical Storm Leo the next day. The storm then performed a cyclonic loop off the Vietnamese coast and began to intensify, becoming a typhoon as it moved to the northeast. As it moved towards China under a high-level ridge Typhoon Leo rapidly intensified to its peak with 205 km/h (127 mph) winds. However, it did not sustain this for long as it then moved northeast into a high shear environment and it weakened as it moved to the north. Leo made landfall on May 2 as a tropical depression. By this time, its convection had become separated from its circulation. Shortly afterwards, Leo dissipated overland.[13]

As Typhoon Leo was developing, its outer rainbands brought up to 130 mm (5.1 in) to regions of Vietnam.[14] High waves caused by the typhoon sank a ship to the south of Hong Kong and only 7 of the 21 people on board were rescued. Peak sustained winds of 90 km/h (56 mph) were recorded on Waglan Island as Typhoon Leo passed to the south of Hong Kong and the storm dropped over 100 mm (3.9 in) of rain on the territory. There was only light damage in Hong Kong as a result of Typhoon Leo, but the rainfall was responsible for 14 injuries, mostly in traffic accidents.[15]

Typhoon Maggie (Etang) edit

Typhoon (JMA)
Category 3 typhoon (SSHWS)
   
DurationJune 1 – June 9
Peak intensity140 km/h (85 mph) (10-min);
955 hPa (mbar)

The sixth tropical depression of the season formed in the monsoon trough to the east of the Philippines on June 1. The system intensified as it moved to the north, becoming Typhoon Maggie 36 hours after it had formed. The typhoon intensified further as it began to head to the northwest into the Luzon Strait and it reached its peak with 195 km/h (121 mph) winds on June 5. The typhoon turned further to the west as it began to interact with Taiwan and started to weaken slowly. Maggie made landfall as a 150 km/h (93 mph) typhoon in southeastern China, to the east of Hong Kong on June 6. The storm then moved along the Chinese coast weakening as it did so. Maggie passed just to the north of Hong Kong before it turned into the mouth of the Pearl River and dissipated inland on June 8.[16] Both the JMA and PAGASA considered Maggie a typhoon, and PAGASA named this storm Etang.[17]

The rainfall from Typhoon Maggie caused landslides in the Philippines that killed three people.[18] The storm killed at least two people, with another five reported missing on Taiwan. The electricity supply to over 100,000 homes was cut off and there was over $18 million of agricultural damage on the island. Maggie brought sustained winds of up to 80 km/h (50 mph) and 85 mm (3.3 in) of rain to Hong Kong. Two oil barges docked in the territory sank, one fully laden with oil which polluted a nearby beach. There were five injuries resulting from Maggie in the territory and the total damages were approximately $100,000. The typhoon killed four people and damaged over 3000 homes in Guangdong. At least 120 vessels were also damaged and there was more than $150 million of direct economic damage in the province.[18] Maggie also brought rain of up to 100 mm (3.9 in) to northern Vietnam, causing some localised flooding.[19]

Tropical Storm 07W edit

Tropical storm (JMA)
Tropical depression (SSHWS)
   
DurationJuly 14 – July 18
Peak intensity65 km/h (40 mph) (10-min);
996 hPa (mbar)

An area of disturbed weather to the northeast of Guam slowly developed as it moved to the west, becoming a tropical depression on July 14. Soon after it formed the depression reached its peak strength with 10-minute winds of 65 km/h (40 mph), which it maintained for two days as it moved towards Honshū. Although the JMA classified the depression as a tropical storm, the JTWC did not follow suit. Not long after peak intensity, increased wind shear began to expose the low level circulation and the depression began to weaken as it turned to the northeast. The depression dissipated on July 18 to the southeast of Honshū.[20]

Tropical Depression 08W edit

Tropical depression (SSHWS)
   
DurationJuly 19 – July 23
Peak intensity55 km/h (35 mph) (1-min);
1004 hPa (mbar)

A tropical disturbance moving north to the east of Okinawa, Japan gradually developed as it moved to the north towards the Japanese mainland. On July 21 it began to intensify, becoming Tropical Depression 08W to the northeast of Okinawa. The depression strengthened slightly in the East China Sea before it made landfall near Changhung, South Korea on July 22. The storm became extratropical as it moved over the Korean Peninsula and it entered the Sea of Japan, where it dissipated.[21]

Severe Tropical Storm Neil (Helming) edit

Severe tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationJuly 22 – July 28
Peak intensity95 km/h (60 mph) (10-min);
980 hPa (mbar)

On July 23, a disturbance began to form in the Philippine Sea within the monsoon trough. The convection gradually consolidated as the disturbance moved north and the ninth tropical depression of the season formed on July 25 south of Okinawa. The depression passed near to the Japanese island and soon strengthened into Tropical Storm Neil. The storm turned slightly westward towards the Korean peninsula and reached its peak strength with 75 km/h (47 mph) winds on July 26. Neil made landfall to the southwest of Suncheon the next day as a minimal tropical storm and soon reemerged over the Yellow Sea as a tropical depression. There it interacted with a mid-latitude trough, that redirected back towards South Korea and it made a second landfall 35 km (22 mi) southwest of Seoul on July 28. Neil then quickly dissipated overland.[22]

Both the JMA and PAGASA considered Neil a tropical storm, with PAGASA naming it Helming. Unusually, PAGASA assessed the storm as having reached a peak on July 22, when the JTWC still considered it a developing disturbance. This difference was due to a difference in opinion between the two centers as to where the storm's center was.[23] There were reports of damage from flooding and winds gusts from Tropical Storm Neil in Japan, with a ferry running aground near Kannoura. Neil caused a fishing boat off the Korean coast to capsize, killing its crew of eight. There were wind gusts of up to 95 km/h (59 mph) on Cheju Island and the peak rainfall reported from the storm was over 200 mm (7.9 in).[24] As the storm dissipated over Korea, it caused flash floods that killed at least seven and left 7,000 homeless.[25]

Tropical Storm 10W edit

Tropical storm (JMA)
Tropical depression (SSHWS)
   
DurationJuly 23 – July 28
Peak intensity75 km/h (45 mph) (10-min);
985 hPa (mbar)

A tropical disturbance began to develop in the South China Sea on July 23. It formed the same monsoon trough that Tropical Storm Neil developed from to the east. The disturbance became a tropical depression late on July 25 as it turned to the north towards the Chinese coast. It did not strengthen any further and made landfall near Shanwei as a minimal tropical depression on July 27. The depression then moved inland and dissipated.[26] The JMA considered Tropical Depression 10W to be a tropical storm, with peak 10-minute winds of 75 km/h (47 mph), making 10W the second storm in 1999 that the JMA considered a tropical storm but the JTWC considered a depression.[23]

As the depression passed near Hong Kong, it dropped 31 mm (1.2 in) of rain on the territory and sustained winds of 72 km/h (45 mph) were recorded on Waglan Island. There was no significant damage over land in the territory, though 18 swimmers were injured in the strong seas associated with the storm.[27]

Typhoon Olga (Ising) edit

Typhoon (JMA)
Category 1 typhoon (SSHWS)
   
DurationJuly 29 – August 3
Peak intensity120 km/h (75 mph) (10-min);
970 hPa (mbar)

On July 26, a disturbance began to develop at the eastern end of a well-defined monsoon trough well to the east of the Philippines. The convection within the disturbance increased as it moved to the north and Tropical Depression 11W formed on July 29. The system continued to intensify, becoming Typhoon Olga two days later as it approached Okinawa. On August 1 Olga made landfall on the Japanese island as a typhoon, weakening slightly as it passed over the island. As it moved to the north-northwest it intensified to its peak with 150 km/h (93 mph) winds as it approached Korea. The storm was beginning to weaken as it passed to the west of Cheju Island on August 3 and it made a second brief landfall on the T'aean Peninsula before moving north in the Yellow Sea. The storm made its final landfall in North Korea as a strong tropical storm later that day with 100 km/h (62 mph) winds and became extratropical soon after.[28] Both the JMA and PAGASA considered Olga a typhoon, with PAGASA naming the storm Ising before the JTWC issued its first warning on the developing system.[23]

Although Typhoon Olga never approached the Philippines closely, it was responsible for heavy rains over much of Luzon that killed 160 people and displaced 80,000.[29] Olga passed over Okinawa, with winds of 80 km/h (50 mph) recorded at Kadena Air Base, causing minimal damage.[28] Torrential rain of up to 600 mm (24 in) fell on the Korean Peninsula, with the highest totals falling near the border between North and South Korea.[30] The resulting floods and landslides caused 64 fatalities in South Korea and wind gusts of 96 km/h (60 mph) were reported near Seoul.[28] The flooding in South Korea destroyed about 400 km2 (150 sq mi) of rice paddies and 8,500 homes, leaving 25,000 people homeless.[23] The Red Cross reported a further 42 deaths and 40,000 were made homeless from flooding in North Korea. That same flooding worsened the ongoing food shortages across the country.[31] Typhoon Olga brought the heaviest rains recorded in Korea for 25 years and caused a total of $657 million of damage in South Korea.[29]

Tropical Storm Paul edit

Tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationAugust 3 – August 9
Peak intensity85 km/h (50 mph) (10-min);
980 hPa (mbar)

Early in August, a low-level circulation center formed within a monsoon gyre to the southwest of Guam. On August 2 the JTWC issued a TCFA for the developing disturbance as it moved to the northwest, and it became Tropical Depression 12W the next day. On August 4 the depression became Tropical Storm Paul and began to merge with the gyre from which it had formed. As it began merging, Paul strengthened to its peak with 95 km/h (59 mph) winds, to the east of Okinawa. After the two systems had merged, Paul turned briefly to the northeast and weakened to back into a tropical depression. The depression moved to the west, brushing the south coast of Kyūshū on August 6 before dissipating in the Yellow Sea.[32]

Tropical Storm Paul was highly unusual in that it formed from a monsoon gyre and then merged with it. Mergers of such systems rarely occur, it is much more common for tropical cyclones which form in this manner to move independently of the non-tropical system. Paul was also considered a tropical storm by the JMA, who reported that the rainfall from the storm caused landslides and flooding in western Japan.[32]

Tropical Storm Rachel edit

Tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationAugust 5 – August 11
Peak intensity65 km/h (40 mph) (10-min);
992 hPa (mbar)

A tropical disturbance formed within a monsoon trough just off the Chinese coast on August 6. The disturbance strengthened and became Tropical Storm Rachel as it moved east towards Taiwan. Rachel weakened back into a depression before it made landfall on the island and it dissipated over the Chungyang mountains on August 7. The remnants moved northeast into the East China Sea and the system redeveloped into a tropical depression the next day as it approached Okinawa. Rachel briefly became a minimal tropical storm for a second time as it approached the Japanese island, before it turned to the northwest. The storm entered an increasingly unfavorable environment and rapidly weakened on August 9.[33]

Tropical Depression 14W edit

Tropical depression (SSHWS)
   
DurationAugust 8 – August 10
Peak intensity45 km/h (30 mph) (1-min);
1000 hPa (mbar)

Tropical Depression 14W formed 120 km (75 mi) to the north of Iwo Jima on August 8. The depression, which had an exposed circulation center, moved to the north under the influence of a subtropical ridge over northern Japan. On August 9 it turned to the northwest and accelerated before its landfall near Owase the next day, with 45 km/h (28 mph) winds. The depression weakened as it passed north over Honshū and dissipated shortly after moving over the Sea of Japan.[34]

Tropical Depression 15W edit

Tropical depression (SSHWS)
   
DurationAugust 16 – August 18
Peak intensity45 km/h (30 mph) (1-min);
1002 hPa (mbar)

A tropical disturbance developed in the East China Sea on August 15 and gradually drifted towards Kyūshū. It intensified as it did so, becoming Tropical Depression 15W the next day. The fourth warning from the JTWC repositioned the cyclone much closer to the Kyūshū coast, where it made landfall near Ushibuka on August 17. The depression then drifted over Kyūshū and entered the Sea of Japan later that day, where it weakened. The storm became extratropical on August 18, but its remnants were recognizable for a further two days.[35]

Severe Tropical Storm Sam (Luding) edit

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
   
DurationAugust 17 – August 24
Peak intensity100 km/h (65 mph) (10-min);
980 hPa (mbar)

On August 17, an area of circulation within the monsoon trough located in the Philippine Sea became more organized and the JTWC issued a TCFA. The developing cyclone slowly moved to the northwest, becoming Tropical Depression 16W nine hours after the TCFA was first issued. As the cyclone continued to intensify, it became Tropical Storm Sam on August 19. Around this time, the subtropical ridge to Sam's north shifted its track in a westwards direction towards Luzon. The storm passed over the north of the island on August 20 and entered the South China Sea reaching typhoon strength the next day. Sam gradually intensified further as it approached the Chinese coast and it made landfall about 19 km (12 mi) to the northeast of Hong Kong at its peak with 140 km/h (87 mph) winds on August 22. Sam continued to move to the northwest over China dissipating about 24 hours later.[36] PAGASA named the developing storm Luding shortly before the JTWC began to issue advisories.[37]

Typhoon Sam was responsible for seven deaths in the Philippines.[36] In addition, flooding from its rainfall displaced over 4000 people, and many major roads were closed due to landslides near Baguio.[37] Sam became the wettest tropical cyclone to affect Hong Kong since records began in 1884, dropping over 616 mm (24.3 in) of rain, exceeding the previous record set in 1926. Peak sustained winds of 96 km/h (60 mph) were recorded on Waglan Island as the typhoon passed over the territory. The heavy rain led to many instances of flooding and over 150 landslides throughout Hong Kong, killing 1 person and forcing the evacuation of about 1,000. A total of 328 people were injured in various incidents relating to the storm, and total losses in Hong Kong totaled to approximately $17 million.[38] In addition to the direct casualties from the storm, China Airlines Flight 642, using an MD-11 aircraft, crashed while attempting to land at Hong Kong International Airport, killing three on board and injuring 219. At the time of the crash wind gusts in excess of 65 km/h (40 mph) were recorded at the airport.[39] After moving into China, Sam killed at least 17[36] and injured 100 people in Guangdong. Direct economic losses in the province were about $18 million.[38]

Severe Tropical Storm Tanya edit

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
   
DurationAugust 19 – August 24
Peak intensity95 km/h (60 mph) (10-min);
1000 hPa (mbar)

On August 19, Tropical Depression 17-W formed at a usually high latitude of over 30°N from a westwards moving low pressure area. The compact system intensified as it moved west under the influence of the subtropical ridge to the north, with the JTWC upgrading it to Tropical Storm Tanya early the next day. Tanya continued to slowly intensify, reaching its peak as a 130 km/h (81 mph) typhoon on August 22. The next day Tanya began to recurve through a weakness in the ridge to its north and increasing wind shear weakened the storm. The storm weakened further as it began to transition into an extratropical storm and the JTWC issued the final warning on the cyclone on August 24.[40]

The JMA also monitored Tanya and made it a severe tropical storm at its peak. Post-season analysis increased the initial intensity of the system, making it a tropical storm before the JTWC began to issue full advisories on Tanya. Typhoon Tanya had no effects on land.[40]

Severe Tropical Storm Dora edit

Severe tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationAugust 20 (Entered basin) – August 23
Peak intensity95 km/h (60 mph) (10-min);
990 hPa (mbar)

Hurricane Dora, the strongest storm of the 1999 Pacific hurricane season, crossed the International Date Line and entered the western Pacific on August 19. The final advisory from the Central Pacific Hurricane Center was written while Dora was still in the eastern Pacific as a minimal hurricane. As the storm crossed the Date Line, the JTWC assumed responsibility for the storm and downgraded it to a tropical storm on its first advisory. Once in the West Pacific, Tropical Storm Dora turned towards the northwest and weakened further as wind shear increased. Dora weakened to a tropical depression on August 22 well to the north of Wake Island and drifted to the north before dissipating the next day.[41]

Dora became the first storm since 1994's John to have existed in all three Pacific basins, and no significant damage was caused by the system anywhere along its path.[42]

Tropical Depression 18W edit

Tropical depression (SSHWS)
   
DurationAugust 21 – August 24
Peak intensity55 km/h (35 mph) (1-min);
1000 hPa (mbar)

On August 21, a small tropical cyclone developed at the southern end of a westward moving shearline about 1,200 km (750 mi) to the east of Tokyo. The depression strengthened slightly to its peak with 55 km/h (34 mph) the next day, before increasing vertical shear took its toll on the system. The increasingly exposed low level circulation of the storm accelerated to the north, towards the frontal system from which it had formed. Finally, Tropical Depression 18W became extratropical on August 24 to the east of Japan.[43]

Severe Tropical Storm Virgil edit

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
   
DurationAugust 23 – August 29
Peak intensity95 km/h (60 mph) (10-min);
994 hPa (mbar)

A tropical disturbance developed at the end of a shear line to the north of Iwo Jima on August 23. Vertical shear began to weaken and the JTWC began to issue advisories on Tropical Depression 19W the next day. The storm turned to the southwest and rapidly intensified on August 25, strengthening from a tropical depression to its peak as a 130 km/h (81 mph) typhoon in 12 hours. Virgil maintained typhoon strength for over a day before it entered a highly sheared environment in which it began to weaken again. Under the influence of a passing frontal system, the motion of the dissipating cyclone turned clockwise to the northeast. The storm dissipated on August 29 over water having never approached land.[44] The JMA monitored Typhoon Virgil and made it a minimal severe tropical storm at its peak.[45]

Tropical Storm Wendy (Mameng) edit

Tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationSeptember 1 – September 4
Peak intensity65 km/h (40 mph) (10-min);
996 hPa (mbar)

Late in August, a broad area of convection developed over a low pressure area in the Philippine Sea to the east of Luzon. The JTWC issued a TCFA for the developing system on August 31, and the disturbance developed into Tropical Depression 20W on September 1 as it moved to the west. The depression did not intensify as it moved to the northwest, brushing the northeast tip of Luzon on September 2. After entering the South China Sea, the system turned more to the west and reached its peak as a 75 km/h (47 mph) tropical storm. It maintained this intensity until it made landfall in China 220 km (140 mi) east-northeast of Hong Kong on September 3. The storm moved inland and dissipated soon after.[46] Both the JMA and PAGASA monitored Tropical Storm Wendy, with PAGASA naming this storm Mameng. PAGASA considered Wendy to have stronger winds than the JTWC, despite the fact that PAGASA uses a 10-minute averaging period to measure sustained winds, which generally results in a lower speed.[37]

Tropical Storm Wendy fueled severe rain over much of southern China in the week after it made landfall, with amounts as high as 500 mm (20 in) recorded in northern Jiangxi and southern Zhejiang. At least 118 people were killed [47] and over 2,600 people were injured; the province of Wenzhou was significantly impacted by Wendy's effects. Over 500,000 people had to be evacuated, over 2.2 million people had been affected by the storm and a local government spokesman called it "the most serious storm in a century". The direct economic damage in the region exceeded $275 million (1999 USD).[47] Whilst mainland China was severely affected by Wendy, the storm only had a minimal impact in Hong Kong.[46]

Severe Tropical Storm York (Neneng) edit

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
   
DurationSeptember 10 – September 17
Peak intensity100 km/h (65 mph) (10-min);
980 hPa (mbar)

A tropical disturbance developed on September 10, in the western Philippine Sea but initially failed to develop as it interacted with Luzon. The disturbance passed over Luzon and entered the South China Sea, where it became more organized and developed into Tropical Depression 21W late on September 11. The system gradually strengthened as it moved northwest towards the Chinese coastline, reaching its peak as a 130 km/h (81 mph) typhoon as it turned towards Hong Kong on September 16. York made landfall to the west of Hong Kong soon after and dissipated into a low pressure area over China the next day.[48] Both the JMA and PAGASA monitored York as a tropical storm, with PAGASA naming the system Neneng.[49]

As the developing depression was crossing the Philippines, it brought heavy showers of up to 400 mm (16 in), which caused some flooding in the Cagayan Valley[50] Eighteen people were killed in landslides in northern Luzon. As Typhoon York approached and landed on Hong Kong's Lantau Island, the Hong Kong Observatory (HKO) raised the No. 10 warning for the first time since 1983 and maintained it for 11 hours, the longest hoisting period on record. The peak sustained winds of 150 km/h (93 mph) were recorded on Waglan Island and the peak gusts of 234 km/h (145 mph) were the highest on record there. A total of 300 mm (12 in) of rain fell on the territory as York passed directly over it and the resulting floods had a severe effect on agriculture throughout Hong Kong. Two people died in the storm and over 500 were injured, 11 seriously. Some 18,000 homes lost power in the wake of the storm and 4,000 trees were uprooted. Damage from York in Hong Kong exceeded $10 million (USD), and economic losses from the storm reached several billion Hong Kong dollars (HKD). Transport in the territory was severely disrupted, with 470 flights cancelled and 80,000 passengers affected.[51]

Two ships ran aground and a cargo ship sank, but all the crew were successfully rescued. One person was injured in Macau and 120 incidents related to the storm were reported there. After passing over Hong Kong, York killed 15 and injured 700 in Guangdong, with economic losses there exceeding $24 million (USD).[51] Ten thousand people were left stranded by flooding in China after the storm and more than 10,000 trees were uprooted in Shenzhen.[52]

Tropical Storm Zia edit

Tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationSeptember 11 – September 15
Peak intensity85 km/h (50 mph) (10-min);
985 hPa (mbar)

The JTWC began to track a disturbance in a monsoon trough to the west of the Marianas Islands on September 11. The disturbance moved to the north without any significant development until September 13, when the outflow of the system markedly improved and it soon developed into a tropical depression to the east of Okinawa. The depression strengthened further becoming Tropical Storm Zia later that day as it approached Kyūshū. Zia peaked with 85 km/h (53 mph) winds as it made landfall on the island on September 14. The storm turned to the northeast and tracked over Japan and dissipated over central Honshū the next day.[53]

Tropical Storm Zia brought heavy rain to western Japan, which exceeded 500 mm (20 in) in places. The resulting flooding and landslides prompted evacuations of over 14,000 people and stranded over 1,300 tourists in a Japanese mountain resort. Nine people died in Japan as a result of Tropical Storm Zia.[49]

Severe Tropical Storm Ann edit

Severe tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationSeptember 14 – September 19
Peak intensity95 km/h (60 mph) (10-min);
985 hPa (mbar)

Tropical Depression 23W formed about 165 km (103 mi) to the east of Okinawa on September 15, from a disturbance moving to the northwest under the influence of a subtropical high located on the eastern side of a monsoon trough.[49] As the system developed it turned first to the northwest and then to the west, becoming Tropical Storm Ann a day after forming. As Ann approached the Chinese coast to the north of Shanghai on September 18, it reached its peak with 85 km/h (53 mph) winds and began to recurve to the northwest. The storm started to weaken as it entered a higher shear environment. Ann captured by a mid-level trough moving through the region and turned to the east, rapidly weakening as it crossed the Yellow Sea. The system dissipated just off the South Korean coast near Mokpo early on September 20.[54]

Tropical Storm Ann brought moderate rain of up to 100 mm (3.9 in) to Anhui, Jiangsu and Shandong on September 18.[55] Rains of up to 200 mm (7.9 in) from Ann and Typhoon Bart saturated South Korea and southwestern Japan, causing flooding and damage to rice paddies.[56]

Typhoon Bart (Oniang) edit

Very strong typhoon (JMA)
Category 5 super typhoon (SSHWS)
   
DurationSeptember 17 – September 25
Peak intensity165 km/h (105 mph) (10-min);
930 hPa (mbar)

Tropical Depression 24W developed on September 17, to the east of Taiwan. The storm drifted to the northwest, becoming Tropical Storm Bart on September 19 and reaching typhoon strength the next day. Bart intensified further as it turned to the northeast under the influence of an upper-level anticyclone.[49] Typhoon Bart reached its peak on September 22 with 260 km/h (160 mph) winds when it passed 75 km (47 mi) to the west of Okinawa, becoming the only super typhoon during the 1999 Pacific typhoon season. Afterwards, Bart began to weaken slowly as it continued north towards Kyūshū, Japan, which it struck on September 23 with 185 km/h (115 mph) winds. After crossing Kyūshū and western Honshū, the storm accelerated to the northeast in the Sea of Japan, becoming extratropical shortly before it reached northern Hokkaidō.[57] As Typhoon Bart formed in PAGASA's area of responsibility, it was named Oniang by PAGASA before moving to the north.[49]

Typhoon Bart claimed at least two lives on Okinawa and brought over 710 mm (28 in) of rain to the island.[57] Kadena Air Base was badly damaged by the typhoon with over $5 million of damage on the base.[58] Heavy flooding and landslides led to total of a 30 deaths and over 1,000 injuries in Japan. Over 800,000 homes lost power and 80,000 damaged in the aftermath of the storm. The worst damage was in Kumamoto Prefecture on Kyūshū, where 16 people died and over 45,000 homes were damaged. Bart affected the whole of Japan, with some minor damages occurring in Hokkaidō shortly after the storm became extratropical.[59] A large crane in Hiroshima collapsed killing three and injuring four people in the Mitsubishi plant there and the Itsukushima Shrine was also damaged.[60] Damage from the storm amounted to ¥16.31 billion (US$155 million); insurance payouts reached ¥31.47 billion (US$299 million).[61] An additional $5 million (1999 USD) in damage occurred to the Japanese economy.[62]

Tropical Storm Cam edit

Tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationSeptember 22 – September 26
Peak intensity85 km/h (50 mph) (10-min);
992 hPa (mbar)

A disturbed area of weather to the south of Hong Kong in the South China Sea became more organized early on September 23, and the JTWC issued a TCFA for the system. It developed into the 25th depression of the season per the JTWC a few hours later and began to track to the northeast, under the influence of a mid-level ridge to the east. The depression gradually intensified, becoming Tropical Storm Cam on September 24. Later that day, the storm reached its peak winds of 75 km/h (47 mph). Around this time, Cam's motion gradually turned towards the north. As it neared the Chinese coast a strong ridge to the north turned Cam abruptly to the west, towards Hong Kong and it began to weaken. The JTWC issued its last warning while the storm was still at sea, shortly before it made landfall over Hong Kong with 35 km/h (22 mph) winds. The storm dissipated over China on September 26.[63]

As Tropical Storm Cam approached Hong Kong, the HKO hoisted the No. 8 Signal for the fifth time in the year; the last time this had occurred was in 1964. The highest gust recorded on land was 121 km/h (75 mph) on Tai Mo Shan, and 41 mm (1.6 in) of rain fell on Hong Kong. Cam was responsible for 23 injuries in Hong Kong and one death in a ship off Stonecutters Island. There was limited flooding in the region and about 150 people were evacuated to emergency shelters. There was some disruption to air travel into the territory, with 100 flights cancelled or delayed.[64]

Typhoon Dan (Pepang) edit

Typhoon (JMA)
Category 3 typhoon (SSHWS)
   
DurationOctober 2 – October 10
Peak intensity150 km/h (90 mph) (10-min);
955 hPa (mbar)

Tropical Depression 26W developed over the Philippine Sea on October 1 about 750 km (470 mi) to the east of Luzon. The system intensified as it moved west-northwest, becoming Tropical Storm Dan on October 3 before reaching typhoon strength the next day. Typhoon Dan reached its peak with 205 km/h (127 mph) early on October 5 and hit northern Luzon at that strength. The typhoon weakened as it entered the South China Sea, but re-intensified as it turned towards the north. Typhoon Dan made its second landfall near Xiamen, China on October 9 and weakened overland. Dan turned to the northeast and weakened to a tropical depression before it moved over the Yellow Sea late on October 10. The depression was absorbed by a frontal system over the Yellow Sea early the next day.[65] Both the JMA and PAGASA treated this storm as a typhoon, with PAGASA naming it Pepang.[66]

Typhoon Dan brought torrential rain of up to 500 mm (20 in) to both northern Luzon and southern Taiwan.[67] Flooding in the Philippines affected 2,600 homes and killed at least five people. There was more than $2 million of damage to agriculture in the Philippines.[68] Southern Taiwan was still recovering from the Chi-Chi earthquake of the previous month, and Dan delayed the recovery efforts. The typhoon burst a dike in Kaohsiung and another in Tainan, that had been damaged by the earthquake. Dan knocked down a large number of trees on Kinmen, which led to the disruption of 70% of the island's power supply. Several fishing boats were sunk and house damaged on Penghu.[69] Thirty-four died and 1,400 people were injured as a result of the storm in Fujian. 1,500 houses were destroyed and $240 million of damage occurred in the province.[68] Dan was the worst typhoon to hit Xiamen in 46 years, killing five and injuring over 100 in the city.[65]

Tropical Storm Eve (Rening) edit

Tropical storm (JMA)
Tropical storm (SSHWS)
   
DurationOctober 15 – October 20
Peak intensity85 km/h (50 mph) (10-min);
990 hPa (mbar)

A broad area of convection to the northeast of Mindanao over the Philippine Sea began to develop on October 15 as it moved to the west, becoming Tropical Depression 27W. The depression made landfall on Samar Island the same day and moved to the northwest across the central Philippines throughout October 6. The depression turned to the west after it emerged into the South China Sea, and turned to the southwest on October 18 in response to increasing mid-level ridging over southeastern China. As it neared the Vietnamese coast the depression strengthened slightly and became Tropical Storm Eve. Eve made landfall 110 km (68 mi) southeast of Da Nang as a minimal tropical storm on October 19 and quickly dissipated overland.[70] Both the JMA and PAGASA considered Eve a tropical storm, with PAGASA naming it Rening.[66]

Tropical Storm Eve brought torrential rain to much of central Vietnam, with about 290 mm (11 in) falling on Huế City and as much as 470 mm (19 in) of rain falling in parts of Hà Tĩnh Province.[71] Eve was the first in a series of storms to bring torrential rain to the region, and the resulting floods killed over 590 people, and they also caused nearly $235 million of damage directly.[70]

Tropical Depression 28W edit

Tropical depression (JMA)
Tropical depression (SSHWS)
   
DurationNovember 5 – November 6
Peak intensity55 km/h (35 mph) (10-min);
1000 hPa (mbar)

A tropical disturbance began to develop 45 km (28 mi) to the southeast of Agrihan, an island of the Northern Mariana Islands, early on November 5, from the tail end of shear line connected to a front that ran to Japan. It strengthened into Tropical Depression 28W early the next day and moved to the northeast along the shear line, reaching its peak with 55 km/h (34 mph) winds. The depression did not develop further, but its motion accelerated and it became an extratropical low 18 hours after forming.[72]

Tropical Depression Frankie (Sendang) edit

Tropical depression (JMA)
Tropical storm (SSHWS)
   
DurationNovember 6 – November 10
Peak intensity55 km/h (35 mph) (10-min);
994 hPa (mbar)

A disturbance to the northeast of Koror in the Philippine Sea developed as it moved to the west on November 6, becoming Tropical Depression 29W. The depression moved rapidly to the west under the influence of the subtropical ridge to the north, crossing Samar early on November 8. The system strengthened over the central Philippines, becoming Tropical Storm Frankie. The influence of a developing ridge to the southeast led to Frankie becoming quasi-stationary over the Sibuyan Sea. The storm soon weakened due to increasing wind shear and interaction with land, and it dissipated on November 11.[73] PAGASA tracked Frankie as a tropical storm, naming it Sendang. The JMA considered this storm to have been a tropical depression.[74]

Tropical Storm Frankie brought heavy rain of up to 300 mm (12 in) to the central Philippines, that disrupted the rice harvest.[75] Flooding from the storm forced the evacuation of 300 families in Calbayog.[76]

Severe Tropical Storm Gloria (Trining) edit

Severe tropical storm (JMA)
Category 1 typhoon (SSHWS)
   
DurationNovember 13 – November 16
Peak intensity95 km/h (60 mph) (10-min);
980 hPa (mbar)

In mid-November, a persistent area of circulation developed at the end of a shear line to the east of Samar. It began to become more organized as it moved to the north on November 12 and became a tropical depression the next day. The cyclone continued to slowly intensify, becoming Tropical Storm Gloria as it turned the northeast, when it was well to the east of Luzon. Gloria began to accelerate to the northeast under the influence of an upper level flow and maintained its strength. The storm passed east of Okinawa on November 15, when the shear markedly reduced and allowed a rapid intensification to typhoon strength. Gloria briefly peaked as a 120 km/h (75 mph) typhoon later that day, before weakening as it started to become extratropical. Typhoon Gloria became fully extratropical on November 16, having weakened back into a tropical storm.[77]

Both the JMA and PAGASA monitored Gloria, with PAGASA naming the storm Trining. The JMA assessed Gloria as being a severe tropical storm at its peak strength on November 15.[74] Typhoon Gloria did not approach land closely. Gloria is the last name to use English names in the basin.

Tropical Depression 31W edit

Tropical depression (SSHWS)
   
DurationDecember 1 – December 4 (Exited basin)
Peak intensity55 km/h (35 mph) (1-min);
1000 hPa (mbar)

An area of low pressure just off Palawan became more organized as it moved to the northwest, away from the island, becoming Tropical Depression 31W early on December 1. A subtropical ridge to the north of the system caused it to move southwest through the South China Sea and off the Vietnamese coast. Winds from the depression peaked at 55 km/h (34 mph). Early on, December 3, when the storm was to the south of Vietnam, it turned to the northwest and headed towards the Malay Peninsula. The depression made landfall in Thailand to the northeast of Phuket on December 4, and the JTWC ceased advisories as the storm weakened overland. The remnants entered the Andaman Sea but redevelopment did not occur.[78]

Tropical Depression 32W edit

Tropical depression (SSHWS)
   
DurationDecember 9 – December 11
Peak intensity55 km/h (35 mph) (1-min);
1000 hPa (mbar)

Tropical Depression 32W developed on December 9 in the South China Sea, between Palawan and Borneo and slowly moved to the west. After the depression reached its peak with 55 km/h (34 mph) winds it began to accelerate to the west. By December 11, when the storm was to the south of Vietnam, it became more sheared and the low-level circulation became exposed. The system dissipated soon afterwards, having never approached land.[79]

Tropical Depression 33W edit

Tropical depression (HKO)
Tropical depression (SSHWS)
   
DurationDecember 14 – December 16
Peak intensity55 km/h (35 mph) (10-min);
1000 hPa (mbar)

On December 14, Tropical Depression 33W formed within a persistent trough about 425 km (264 mi) to the east of Cam Ranh Bay, Vietnam. A high level of wind shear restricted the storm's strength to 55 km/h (34 mph), which it maintained as it moved west towards Vietnam. The storm turned to the north shortly before it made landfall on December 16 and dissipated soon after over Vietnam under the influence of increased wind shear and interaction with land. It is unknown if the storm had any effects on land.[80]

Other systems edit

On October 21, an area of convection formed in the Sulu Sea and emerged over the South China Sea on the next day. Thunderstorm activity started to increase and the Joint Typhoon Warning Center issued a Tropical Cyclone Formation Alert (TCFA) on the system. However, the low failed to develop further and this caused the cancellation of the TCFA. On October 24, the low crossed the Malay Peninsula and emerged into the North Indian Ocean. On the next day, while over the Andaman Sea, the low became a tropical depression, which became the deadly 1999 Odisha cyclone.

Storm names edit

During the season 21 named tropical cyclones developed in the Western Pacific and were named by the Joint Typhoon Warning Center, when it was determined that they had become tropical storms. These names were contributed to a revised list from 1996. However, the agency stopped naming cyclones after this season as the Japan Meteorological Agency started naming systems. Consequently, this was the last year the following lists were used.

Hilda Iris Jacob Kate Leo Maggie Neil Olga Paul Rachel Sam Tanya
Virgil Wendy York Zia Ann Bart Cam Dan Eve Frankie Gloria

Philippines edit

Auring Bebeng Karing Diding Etang
Gening Helming Ising Luding Mameng
Neneng Oniang Pepang Rening Sendang
Trining Ulding (unused) Warling (unused) Yayang (unused)
Auxiliary list
Ading (unused)
Barang (unused) Krising (unused) Dadang (unused) Erling (unused) Goying (unused)

The Philippine Atmospheric, Geophysical and Astronomical Services Administration uses its own naming scheme for tropical cyclones in their area of responsibility. PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility. Should the list of names for a given year prove to be insufficient, names are taken from an auxiliary list, the first 10 of which are published each year before the season starts. This is the same list used for the 1995 season. PAGASA uses its own naming scheme that starts in the Filipino alphabet, with names of Filipino female names ending with "ng" (A, B, K, D, etc.). Because PAGASA started a new naming scheme in 2001, therefore, this naming list would not be used in the 2003 season. Names that were not assigned/going to use are marked in gray.

Season effects edit

This table summarizes all the systems that developed within or moved into the North Pacific Ocean, to the west of the International Date Line during 1999. The tables also provide an overview of a systems intensity, duration, land areas affected and any deaths or damages associated with the system.

Name Dates Peak intensity Areas affected Damage
(USD)
Deaths Refs
Category Wind speed Pressure
Hilda (Auring) January 3 – 8 Tropical depression 55 km/h (34 mph) 1000 hPa (29.53 inHg) Malaysia $1.3 million 5
TD February 9 – 10 Tropical depression Not specified 1004 hPa (29.65 inHg) None None None
Iris (Bebeng) February 14 – 19 Tropical depression 55 km/h (34 mph) 1000 hPa (29.53 inHg) None None None
Jacob (Karing) April 7 – 10 Tropical depression 55 km/h (34 mph) 1006 hPa (29.71 inHg) Philippines None None
Kate (Diding) April 21 – 28 Severe tropical storm 100 km/h (62 mph) 980 hPa (28.94 inHg) Philippines None None
Leo April 27 – May 2 Strong typhoon 120 km/h (75 mph) 970 hPa (28.64 inHg) South China None None
Maggie (Etang) June 1 – 9 Strong typhoon 120 km/h (75 mph) 970 hPa (28.64 inHg) Philippines, Taiwan, South China $168 million 9
TD June 1 – 2 Tropical depression Not specified 1004 hPa (29.65 inHg) None None None
Gening June 3 – 6 Tropical depression 55 km/h (34 mph) 996 hPa (29.41 inHg) None None None
TD July 9 – 15 Tropical depression 55 km/h (34 mph) 996 hPa (29.41 inHg) Japan None None
07W July 14 – 18 Tropical storm 65 km/h (40 mph) 996 hPa (29.41 inHg) None None None
08W July 19 – 23 Tropical depression Not specified 1004 hPa (29.65 inHg) None None None
Neil (Heling) July 22 – 28 Severe tropical storm 95 km/h (59 mph) 980 hPa (28.94 inHg) Japan, Korea None 15
10W July 23 – 28 Tropical storm 75 km/h (47 mph) 985 hPa (29.09 inHg) China None None
Olga (Ising) July 29 – August 3 Strong typhoon 120 km/h (75 mph) 970 hPa (28.64 inHg) Caroline Islands, Ryukyu Islands, Korea $657 million 106
Paul August 3 – 9 Tropical storm 85 km/h (53 mph) 980 hPa (28.94 inHg) Mariana Islands, Japan, South Korea, China None None
Rachel August 5 – 11 Tropical storm 65 km/h (40 mph) 992 hPa (29.29 inHg) Taiwan, Ryukyu Islands, China None None
14W August 7 – 11 Tropical depression Not specified 1004 hPa (29.65 inHg) Japan None None
TD August 9 – 11 Tropical depression Not specified 1000 hPa (29.53 inHg) None None None
TD August 11 Tropical depression Not specified 1000 hPa (29.53 inHg) None None None
TD August 11 – 16 Tropical depression Not specified 1000 hPa (29.53 inHg) Japan None None
15W August 14 – 20 Tropical depression Not specified 1000 hPa (29.53 inHg) Japan None None
TD August 16 – 17 Tropical depression Not specified 1010 hPa (29.83 inHg) None None None
Sam (Luding) August 18 – 24 Severe tropical storm 100 km/h (62 mph) 980 hPa (28.94 inHg) Philippines, South China $35 million 20
Tanya August 19 – 24 Severe tropical storm 95 km/h (59 mph) 1000 hPa (29.53 inHg) Wake Island None None
Dora August 20 – 26 Severe tropical storm 95 km/h (59 mph) 990 hPa (29.23 inHg) Wake Island None None
18W August 21 – 24 Tropical depression Not specified 1010 hPa (29.83 inHg) None None None
Virgil August 23 – 29 Severe tropical storm 95 km/h (59 mph) 1000 hPa (29.53 inHg) None None None
TD August 30 Tropical depression Not specified 1008 hPa (29.77 inHg) None None None
Wendy (Mameng) September 1 – 7 Tropical storm 65 km/h (40 mph) 990 hPa (29.23 inHg) Philippines, China $309 million 133
York (Neneng) September 9 – 17 Severe tropical storm 100 km/h (62 mph) 980 hPa (28.94 inHg) Philippines, South China $34 million 35
Zia September 11 – 15 Tropical storm 65 km/h (40 mph) 990 hPa (29.23 inHg) Philippines, China None None
Ann September 14 – 19 Severe tropical storm 95 km/h (59 mph) 985 hPa (29.09 inHg) East China None None
Bart (Oniang) September 17 – 25 Very strong typhoon 165 km/h (103 mph) 930 hPa (27.46 inHg) Japan $155 million 36
TD September 21 Tropical depression Not specified 1008 hPa (29.77 inHg) None None None
Cam September 22 – 26 Tropical storm 85 km/h (53 mph) 992 hPa (29.29 inHg) South China None 1
Dan (Pepang) October 2 – 10 Strong typhoon 150 km/h (93 mph) 955 hPa (28.20 inHg) Philippines, Taiwan, China, South Korea $242 million 44
Eve (Rening) October 15 – 20 Tropical storm 85 km/h (53 mph) 990 hPa (29.23 inHg) Philippines, Vietnam $235 million 590
TD October 23 – 24 Tropical depression Not specified 1004 hPa (29.65 inHg) Vietnam, Thailand None None
TD November 5 Tropical depression Not specified 1002 hPa (29.59 inHg) Vietnam None None
28W November 5 – 8 Tropical depression 55 km/h (34 mph) 1000 hPa (29.53 inHg) Mariana Islands None None
Frankie (Sendang) November 6 – 11 Tropical depression 55 km/h (34 mph) 994 hPa (29.35 inHg) Philippines None None
Gloria (Trining) November 13 – 16 Severe tropical storm 95 km/h (59 mph) 980 hPa (28.94 inHg) None None None
31W December 1 – 4 Tropical depression 55 km/h (34 mph) 1004 hPa (29.65 inHg) Thailand None None
32W December 8 – 10 Tropical depression 55 km/h (34 mph) 1002 hPa (29.59 inHg) None None None
33W December 14 – 16 Tropical depression 55 km/h (34 mph) 1000 hPa (29.53 inHg) Vietnam None None
Season aggregates
46 systems January 3 – December 16, 1999 165 km/h (103 mph) 930 hPa (27.46 inHg) $1.84 billion 976

See also edit

References edit

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  4. ^ Borneo Bulletin (1999-01-11). "Hilda causes RM15 mil in road damages in Sabah".
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External links edit

  • Japan Meteorological Agency
  • Joint Typhoon Warning Center 2010-03-01 at the Wayback Machine.
  • National Weather Service Guam
  • Hong Kong Observatory
  • Macau Meteorological Geophysical Services
  • Philippine Atmospheric, Geophysical and Astronomical Services Administration
  • Satellite movie of 1999 Pacific typhoon season

1999, pacific, typhoon, season, last, pacific, typhoon, season, english, names, storm, names, very, inactive, season, featuring, lowest, number, typhoons, record, five, official, bounds, year, round, 1999, most, tropical, cyclones, tend, form, northwestern, pa. The 1999 Pacific typhoon season was the last Pacific typhoon season to use English names as storm names It was a very inactive season featuring the lowest number of typhoons on record five It had no official bounds it ran year round in 1999 but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean 1999 Pacific typhoon seasonSeason summary mapSeasonal boundariesFirst system formedJanuary 3 1999Last system dissipatedDecember 16 1999Strongest stormNameBart Maximum winds165 km h 105 mph 10 minute sustained Lowest pressure930 hPa mbar Seasonal statisticsTotal depressions45Total storms20Typhoons5 record low Super typhoons1 unofficial Total fatalities976Total damage 18 36 billion 1999 USD Related articles1999 Atlantic hurricane season 1999 Pacific hurricane season 1999 North Indian Ocean cyclone seasonPacific typhoon seasons1997 1998 1999 2000 2001Tropical Storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center Tropical depressions in this basin have the W suffix added to their number Tropical cyclones that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric Geophysical and Astronomical Services Administration or PAGASA This can often result in the same storm having two names Contents 1 Season summary 2 Systems 2 1 Tropical Depression Hilda Auring 2 2 Tropical Depression Iris Bebeng 2 3 Tropical Depression Jacob Karing 2 4 Severe Tropical Storm Kate Diding 2 5 Typhoon Leo 2 6 Typhoon Maggie Etang 2 7 Tropical Storm 07W 2 8 Tropical Depression 08W 2 9 Severe Tropical Storm Neil Helming 2 10 Tropical Storm 10W 2 11 Typhoon Olga Ising 2 12 Tropical Storm Paul 2 13 Tropical Storm Rachel 2 14 Tropical Depression 14W 2 15 Tropical Depression 15W 2 16 Severe Tropical Storm Sam Luding 2 17 Severe Tropical Storm Tanya 2 18 Severe Tropical Storm Dora 2 19 Tropical Depression 18W 2 20 Severe Tropical Storm Virgil 2 21 Tropical Storm Wendy Mameng 2 22 Severe Tropical Storm York Neneng 2 23 Tropical Storm Zia 2 24 Severe Tropical Storm Ann 2 25 Typhoon Bart Oniang 2 26 Tropical Storm Cam 2 27 Typhoon Dan Pepang 2 28 Tropical Storm Eve Rening 2 29 Tropical Depression 28W 2 30 Tropical Depression Frankie Sendang 2 31 Severe Tropical Storm Gloria Trining 2 32 Tropical Depression 31W 2 33 Tropical Depression 32W 2 34 Tropical Depression 33W 3 Other systems 4 Storm names 4 1 Philippines 5 Season effects 6 See also 7 References 8 External linksSeason summary editThis section is empty You can help by adding to it December 2019 Systems editIn the storm information below the Joint Typhoon Warning Center JTWC wind speed advisories differ than that of the Japan Meteorological Agency JMA because the JTWC uses the United States criteria of 1 minute sustained winds to designate a tropical cyclone s maximum sustained winds whereas the JMA uses 10 minute sustained winds to determine maximum sustained winds Consequently in most cases the JTWC maximum winds for a cyclone appear higher than the JMA s estimated maximum winds for the same system Tropical Depression Hilda Auring edit Tropical depression JMA Tropical storm SSHWS nbsp nbsp DurationJanuary 3 January 8Peak intensity55 km h 35 mph 10 min 1000 hPa mbar The JTWC issued a Tropical Cyclone Formation Alert TCFA for a developing broad circulation that stretched out from the northwest Borneo coast early on January 4 This developed into a tropical depression and moved slowly to the north away from Borneo becoming Tropical Storm Hilda early on January 6 Soon after reaching its peak strength of 65 km h 40 mph Hilda drifted further north into an area of increased wind shear which caused the storm to dissipate the next day 1 Both JMA and PAGASA tracked this system but considered it a tropical depression PAGASA named the storm Auring 2 Malaysia reported to the World Meteorological Organization WMO Typhoon Committee that Tropical Storm Hilda brought heavy rain to Sabah The rain caused flooding and landslides and was responsible for five deaths 3 The mudslides caused about 1 3 million in damage 1999 USD 15 million 1999 MYR to roads throughout the country 4 Tropical Depression Iris Bebeng edit Tropical depression JMA Tropical storm SSHWS nbsp nbsp DurationFebruary 14 February 19Peak intensity55 km h 35 mph 10 min 1000 hPa mbar A monsoon depression began to develop between Pohnpei and Chuuk on February 10 as it moved west 5 The JTWC issued a TCFA as the depression formed and passed near Palau on February 13 The storm slowly consolidated as it moved towards the Philippines becoming Tropical Storm Iris on February 17 but did not intensify any further As the storm turned northwards under the influence of a subtropical ridge to the east it entered a high shear environment and rapidly degenerated dissipating on February 19 220 km 140 mi to the east of Luzon 6 PAGASA considered this storm to have been a tropical depression and named it Bebeng 5 Tropical Depression Jacob Karing edit Tropical depression JMA Tropical storm SSHWS nbsp nbsp DurationApril 6 April 9Peak intensity55 km h 35 mph 10 min 1006 hPa mbar A low pressure area 220 km 140 mi to the west of Yap developed into a tropical depression on April 6 It gradually developed as it moved to the west becoming a strong depression with 55 km h 34 mph winds It then began to accelerate to the northwest becoming a minimal tropical storm as it did so However this northwards motion brought it into a region of increased shear which weakened it back into a tropical depression The low level circulation became completely exposed and the weakening system made landfall on southern Luzon on April 10 7 PAGASA named the system Karing and considered it a tropical depression 8 The rainfall from Jacob ranged from 80 mm 3 1 in up to 400 mm 16 in in some places in the Philippines but only minor damage was recorded on land 9 Severe Tropical Storm Kate Diding edit Severe tropical storm JMA Category 1 typhoon SSHWS nbsp nbsp DurationApril 21 April 28Peak intensity100 km h 65 mph 10 min 980 hPa mbar On April 22 a tropical disturbance which had developed in the Philippine Sea moved over Mindanao and intensified into a tropical depression whilst it was still overland The depression soon moved overwater again as it tracked north to the east of the Philippines becoming Tropical Storm Kate the next day The JTWC initially forecast that the storm would only intensify slightly as they predicted it to move north northeast into an unfavorable environment However Kate instead moved on a more northerly route and entered an area with minimal wind shear On April 26 Kate became a typhoon the first of the season and reached its peak strength with 140 km h 87 mph soon after Later that day the typhoon s motion accelerated to the northeast and it passed 9 km 5 6 mi to the north of Iwo Jima Kate then began to lose its convection and became an extratropical on April 28 to the northeast of Iwo Jima 10 Both JMA and PAGASA considered Kate to have been a tropical storm at its peak in both cases considering this the first tropical storm of the season PAGASA named the depression Diding soon after it formed and upgraded it to a tropical storm before the JTWC 8 Kate brought torrential rain to the east central Philippines with amounts as high as 360 mm 14 in falling in places 11 The peak winds recorded on Iwo Jima were 95 km h 59 mph with gusts of up to 126 km h 78 mph 12 Typhoon Leo edit Typhoon JMA Category 3 typhoon SSHWS nbsp nbsp DurationApril 27 May 2Peak intensity120 km h 75 mph 10 min 970 hPa mbar In late April a circulation began to develop within a monsoon depression in the South China Sea forming into a tropical depression on April 27 when it was 710 km 440 mi to the west of Manila It strengthened as it moved to the west and became Tropical Storm Leo the next day The storm then performed a cyclonic loop off the Vietnamese coast and began to intensify becoming a typhoon as it moved to the northeast As it moved towards China under a high level ridge Typhoon Leo rapidly intensified to its peak with 205 km h 127 mph winds However it did not sustain this for long as it then moved northeast into a high shear environment and it weakened as it moved to the north Leo made landfall on May 2 as a tropical depression By this time its convection had become separated from its circulation Shortly afterwards Leo dissipated overland 13 As Typhoon Leo was developing its outer rainbands brought up to 130 mm 5 1 in to regions of Vietnam 14 High waves caused by the typhoon sank a ship to the south of Hong Kong and only 7 of the 21 people on board were rescued Peak sustained winds of 90 km h 56 mph were recorded on Waglan Island as Typhoon Leo passed to the south of Hong Kong and the storm dropped over 100 mm 3 9 in of rain on the territory There was only light damage in Hong Kong as a result of Typhoon Leo but the rainfall was responsible for 14 injuries mostly in traffic accidents 15 Typhoon Maggie Etang edit Typhoon JMA Category 3 typhoon SSHWS nbsp nbsp DurationJune 1 June 9Peak intensity140 km h 85 mph 10 min 955 hPa mbar Main article Typhoon Maggie The sixth tropical depression of the season formed in the monsoon trough to the east of the Philippines on June 1 The system intensified as it moved to the north becoming Typhoon Maggie 36 hours after it had formed The typhoon intensified further as it began to head to the northwest into the Luzon Strait and it reached its peak with 195 km h 121 mph winds on June 5 The typhoon turned further to the west as it began to interact with Taiwan and started to weaken slowly Maggie made landfall as a 150 km h 93 mph typhoon in southeastern China to the east of Hong Kong on June 6 The storm then moved along the Chinese coast weakening as it did so Maggie passed just to the north of Hong Kong before it turned into the mouth of the Pearl River and dissipated inland on June 8 16 Both the JMA and PAGASA considered Maggie a typhoon and PAGASA named this storm Etang 17 The rainfall from Typhoon Maggie caused landslides in the Philippines that killed three people 18 The storm killed at least two people with another five reported missing on Taiwan The electricity supply to over 100 000 homes was cut off and there was over 18 million of agricultural damage on the island Maggie brought sustained winds of up to 80 km h 50 mph and 85 mm 3 3 in of rain to Hong Kong Two oil barges docked in the territory sank one fully laden with oil which polluted a nearby beach There were five injuries resulting from Maggie in the territory and the total damages were approximately 100 000 The typhoon killed four people and damaged over 3000 homes in Guangdong At least 120 vessels were also damaged and there was more than 150 million of direct economic damage in the province 18 Maggie also brought rain of up to 100 mm 3 9 in to northern Vietnam causing some localised flooding 19 Tropical Storm 07W edit Tropical storm JMA Tropical depression SSHWS nbsp nbsp DurationJuly 14 July 18Peak intensity65 km h 40 mph 10 min 996 hPa mbar An area of disturbed weather to the northeast of Guam slowly developed as it moved to the west becoming a tropical depression on July 14 Soon after it formed the depression reached its peak strength with 10 minute winds of 65 km h 40 mph which it maintained for two days as it moved towards Honshu Although the JMA classified the depression as a tropical storm the JTWC did not follow suit Not long after peak intensity increased wind shear began to expose the low level circulation and the depression began to weaken as it turned to the northeast The depression dissipated on July 18 to the southeast of Honshu 20 Tropical Depression 08W edit Tropical depression SSHWS nbsp nbsp DurationJuly 19 July 23Peak intensity55 km h 35 mph 1 min 1004 hPa mbar A tropical disturbance moving north to the east of Okinawa Japan gradually developed as it moved to the north towards the Japanese mainland On July 21 it began to intensify becoming Tropical Depression 08W to the northeast of Okinawa The depression strengthened slightly in the East China Sea before it made landfall near Changhung South Korea on July 22 The storm became extratropical as it moved over the Korean Peninsula and it entered the Sea of Japan where it dissipated 21 Severe Tropical Storm Neil Helming edit Severe tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationJuly 22 July 28Peak intensity95 km h 60 mph 10 min 980 hPa mbar On July 23 a disturbance began to form in the Philippine Sea within the monsoon trough The convection gradually consolidated as the disturbance moved north and the ninth tropical depression of the season formed on July 25 south of Okinawa The depression passed near to the Japanese island and soon strengthened into Tropical Storm Neil The storm turned slightly westward towards the Korean peninsula and reached its peak strength with 75 km h 47 mph winds on July 26 Neil made landfall to the southwest of Suncheon the next day as a minimal tropical storm and soon reemerged over the Yellow Sea as a tropical depression There it interacted with a mid latitude trough that redirected back towards South Korea and it made a second landfall 35 km 22 mi southwest of Seoul on July 28 Neil then quickly dissipated overland 22 Both the JMA and PAGASA considered Neil a tropical storm with PAGASA naming it Helming Unusually PAGASA assessed the storm as having reached a peak on July 22 when the JTWC still considered it a developing disturbance This difference was due to a difference in opinion between the two centers as to where the storm s center was 23 There were reports of damage from flooding and winds gusts from Tropical Storm Neil in Japan with a ferry running aground near Kannoura Neil caused a fishing boat off the Korean coast to capsize killing its crew of eight There were wind gusts of up to 95 km h 59 mph on Cheju Island and the peak rainfall reported from the storm was over 200 mm 7 9 in 24 As the storm dissipated over Korea it caused flash floods that killed at least seven and left 7 000 homeless 25 Tropical Storm 10W edit Tropical storm JMA Tropical depression SSHWS nbsp nbsp DurationJuly 23 July 28Peak intensity75 km h 45 mph 10 min 985 hPa mbar A tropical disturbance began to develop in the South China Sea on July 23 It formed the same monsoon trough that Tropical Storm Neil developed from to the east The disturbance became a tropical depression late on July 25 as it turned to the north towards the Chinese coast It did not strengthen any further and made landfall near Shanwei as a minimal tropical depression on July 27 The depression then moved inland and dissipated 26 The JMA considered Tropical Depression 10W to be a tropical storm with peak 10 minute winds of 75 km h 47 mph making 10W the second storm in 1999 that the JMA considered a tropical storm but the JTWC considered a depression 23 As the depression passed near Hong Kong it dropped 31 mm 1 2 in of rain on the territory and sustained winds of 72 km h 45 mph were recorded on Waglan Island There was no significant damage over land in the territory though 18 swimmers were injured in the strong seas associated with the storm 27 Typhoon Olga Ising edit Typhoon JMA Category 1 typhoon SSHWS nbsp nbsp DurationJuly 29 August 3Peak intensity120 km h 75 mph 10 min 970 hPa mbar Main article Typhoon Olga 1999 On July 26 a disturbance began to develop at the eastern end of a well defined monsoon trough well to the east of the Philippines The convection within the disturbance increased as it moved to the north and Tropical Depression 11W formed on July 29 The system continued to intensify becoming Typhoon Olga two days later as it approached Okinawa On August 1 Olga made landfall on the Japanese island as a typhoon weakening slightly as it passed over the island As it moved to the north northwest it intensified to its peak with 150 km h 93 mph winds as it approached Korea The storm was beginning to weaken as it passed to the west of Cheju Island on August 3 and it made a second brief landfall on the T aean Peninsula before moving north in the Yellow Sea The storm made its final landfall in North Korea as a strong tropical storm later that day with 100 km h 62 mph winds and became extratropical soon after 28 Both the JMA and PAGASA considered Olga a typhoon with PAGASA naming the storm Ising before the JTWC issued its first warning on the developing system 23 Although Typhoon Olga never approached the Philippines closely it was responsible for heavy rains over much of Luzon that killed 160 people and displaced 80 000 29 Olga passed over Okinawa with winds of 80 km h 50 mph recorded at Kadena Air Base causing minimal damage 28 Torrential rain of up to 600 mm 24 in fell on the Korean Peninsula with the highest totals falling near the border between North and South Korea 30 The resulting floods and landslides caused 64 fatalities in South Korea and wind gusts of 96 km h 60 mph were reported near Seoul 28 The flooding in South Korea destroyed about 400 km2 150 sq mi of rice paddies and 8 500 homes leaving 25 000 people homeless 23 The Red Cross reported a further 42 deaths and 40 000 were made homeless from flooding in North Korea That same flooding worsened the ongoing food shortages across the country 31 Typhoon Olga brought the heaviest rains recorded in Korea for 25 years and caused a total of 657 million of damage in South Korea 29 Tropical Storm Paul edit Tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationAugust 3 August 9Peak intensity85 km h 50 mph 10 min 980 hPa mbar Early in August a low level circulation center formed within a monsoon gyre to the southwest of Guam On August 2 the JTWC issued a TCFA for the developing disturbance as it moved to the northwest and it became Tropical Depression 12W the next day On August 4 the depression became Tropical Storm Paul and began to merge with the gyre from which it had formed As it began merging Paul strengthened to its peak with 95 km h 59 mph winds to the east of Okinawa After the two systems had merged Paul turned briefly to the northeast and weakened to back into a tropical depression The depression moved to the west brushing the south coast of Kyushu on August 6 before dissipating in the Yellow Sea 32 Tropical Storm Paul was highly unusual in that it formed from a monsoon gyre and then merged with it Mergers of such systems rarely occur it is much more common for tropical cyclones which form in this manner to move independently of the non tropical system Paul was also considered a tropical storm by the JMA who reported that the rainfall from the storm caused landslides and flooding in western Japan 32 Tropical Storm Rachel edit Tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationAugust 5 August 11Peak intensity65 km h 40 mph 10 min 992 hPa mbar A tropical disturbance formed within a monsoon trough just off the Chinese coast on August 6 The disturbance strengthened and became Tropical Storm Rachel as it moved east towards Taiwan Rachel weakened back into a depression before it made landfall on the island and it dissipated over the Chungyang mountains on August 7 The remnants moved northeast into the East China Sea and the system redeveloped into a tropical depression the next day as it approached Okinawa Rachel briefly became a minimal tropical storm for a second time as it approached the Japanese island before it turned to the northwest The storm entered an increasingly unfavorable environment and rapidly weakened on August 9 33 Tropical Depression 14W edit Tropical depression SSHWS nbsp nbsp DurationAugust 8 August 10Peak intensity45 km h 30 mph 1 min 1000 hPa mbar Tropical Depression 14W formed 120 km 75 mi to the north of Iwo Jima on August 8 The depression which had an exposed circulation center moved to the north under the influence of a subtropical ridge over northern Japan On August 9 it turned to the northwest and accelerated before its landfall near Owase the next day with 45 km h 28 mph winds The depression weakened as it passed north over Honshu and dissipated shortly after moving over the Sea of Japan 34 Tropical Depression 15W edit Tropical depression SSHWS nbsp nbsp DurationAugust 16 August 18Peak intensity45 km h 30 mph 1 min 1002 hPa mbar A tropical disturbance developed in the East China Sea on August 15 and gradually drifted towards Kyushu It intensified as it did so becoming Tropical Depression 15W the next day The fourth warning from the JTWC repositioned the cyclone much closer to the Kyushu coast where it made landfall near Ushibuka on August 17 The depression then drifted over Kyushu and entered the Sea of Japan later that day where it weakened The storm became extratropical on August 18 but its remnants were recognizable for a further two days 35 Severe Tropical Storm Sam Luding edit Severe tropical storm JMA Category 1 typhoon SSHWS nbsp nbsp DurationAugust 17 August 24Peak intensity100 km h 65 mph 10 min 980 hPa mbar Main article Tropical Storm Sam 1999 On August 17 an area of circulation within the monsoon trough located in the Philippine Sea became more organized and the JTWC issued a TCFA The developing cyclone slowly moved to the northwest becoming Tropical Depression 16W nine hours after the TCFA was first issued As the cyclone continued to intensify it became Tropical Storm Sam on August 19 Around this time the subtropical ridge to Sam s north shifted its track in a westwards direction towards Luzon The storm passed over the north of the island on August 20 and entered the South China Sea reaching typhoon strength the next day Sam gradually intensified further as it approached the Chinese coast and it made landfall about 19 km 12 mi to the northeast of Hong Kong at its peak with 140 km h 87 mph winds on August 22 Sam continued to move to the northwest over China dissipating about 24 hours later 36 PAGASA named the developing storm Luding shortly before the JTWC began to issue advisories 37 Typhoon Sam was responsible for seven deaths in the Philippines 36 In addition flooding from its rainfall displaced over 4000 people and many major roads were closed due to landslides near Baguio 37 Sam became the wettest tropical cyclone to affect Hong Kong since records began in 1884 dropping over 616 mm 24 3 in of rain exceeding the previous record set in 1926 Peak sustained winds of 96 km h 60 mph were recorded on Waglan Island as the typhoon passed over the territory The heavy rain led to many instances of flooding and over 150 landslides throughout Hong Kong killing 1 person and forcing the evacuation of about 1 000 A total of 328 people were injured in various incidents relating to the storm and total losses in Hong Kong totaled to approximately 17 million 38 In addition to the direct casualties from the storm China Airlines Flight 642 using an MD 11 aircraft crashed while attempting to land at Hong Kong International Airport killing three on board and injuring 219 At the time of the crash wind gusts in excess of 65 km h 40 mph were recorded at the airport 39 After moving into China Sam killed at least 17 36 and injured 100 people in Guangdong Direct economic losses in the province were about 18 million 38 Severe Tropical Storm Tanya edit Severe tropical storm JMA Category 1 typhoon SSHWS nbsp nbsp DurationAugust 19 August 24Peak intensity95 km h 60 mph 10 min 1000 hPa mbar On August 19 Tropical Depression 17 W formed at a usually high latitude of over 30 N from a westwards moving low pressure area The compact system intensified as it moved west under the influence of the subtropical ridge to the north with the JTWC upgrading it to Tropical Storm Tanya early the next day Tanya continued to slowly intensify reaching its peak as a 130 km h 81 mph typhoon on August 22 The next day Tanya began to recurve through a weakness in the ridge to its north and increasing wind shear weakened the storm The storm weakened further as it began to transition into an extratropical storm and the JTWC issued the final warning on the cyclone on August 24 40 The JMA also monitored Tanya and made it a severe tropical storm at its peak Post season analysis increased the initial intensity of the system making it a tropical storm before the JTWC began to issue full advisories on Tanya Typhoon Tanya had no effects on land 40 Severe Tropical Storm Dora edit Severe tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationAugust 20 Entered basin August 23Peak intensity95 km h 60 mph 10 min 990 hPa mbar Main article Hurricane Dora 1999 Hurricane Dora the strongest storm of the 1999 Pacific hurricane season crossed the International Date Line and entered the western Pacific on August 19 The final advisory from the Central Pacific Hurricane Center was written while Dora was still in the eastern Pacific as a minimal hurricane As the storm crossed the Date Line the JTWC assumed responsibility for the storm and downgraded it to a tropical storm on its first advisory Once in the West Pacific Tropical Storm Dora turned towards the northwest and weakened further as wind shear increased Dora weakened to a tropical depression on August 22 well to the north of Wake Island and drifted to the north before dissipating the next day 41 Dora became the first storm since 1994 s John to have existed in all three Pacific basins and no significant damage was caused by the system anywhere along its path 42 Tropical Depression 18W edit Tropical depression SSHWS nbsp nbsp DurationAugust 21 August 24Peak intensity55 km h 35 mph 1 min 1000 hPa mbar On August 21 a small tropical cyclone developed at the southern end of a westward moving shearline about 1 200 km 750 mi to the east of Tokyo The depression strengthened slightly to its peak with 55 km h 34 mph the next day before increasing vertical shear took its toll on the system The increasingly exposed low level circulation of the storm accelerated to the north towards the frontal system from which it had formed Finally Tropical Depression 18W became extratropical on August 24 to the east of Japan 43 Severe Tropical Storm Virgil edit Severe tropical storm JMA Category 1 typhoon SSHWS nbsp nbsp DurationAugust 23 August 29Peak intensity95 km h 60 mph 10 min 994 hPa mbar A tropical disturbance developed at the end of a shear line to the north of Iwo Jima on August 23 Vertical shear began to weaken and the JTWC began to issue advisories on Tropical Depression 19W the next day The storm turned to the southwest and rapidly intensified on August 25 strengthening from a tropical depression to its peak as a 130 km h 81 mph typhoon in 12 hours Virgil maintained typhoon strength for over a day before it entered a highly sheared environment in which it began to weaken again Under the influence of a passing frontal system the motion of the dissipating cyclone turned clockwise to the northeast The storm dissipated on August 29 over water having never approached land 44 The JMA monitored Typhoon Virgil and made it a minimal severe tropical storm at its peak 45 Tropical Storm Wendy Mameng edit Tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationSeptember 1 September 4Peak intensity65 km h 40 mph 10 min 996 hPa mbar Main article Tropical Storm Wendy 1999 Late in August a broad area of convection developed over a low pressure area in the Philippine Sea to the east of Luzon The JTWC issued a TCFA for the developing system on August 31 and the disturbance developed into Tropical Depression 20W on September 1 as it moved to the west The depression did not intensify as it moved to the northwest brushing the northeast tip of Luzon on September 2 After entering the South China Sea the system turned more to the west and reached its peak as a 75 km h 47 mph tropical storm It maintained this intensity until it made landfall in China 220 km 140 mi east northeast of Hong Kong on September 3 The storm moved inland and dissipated soon after 46 Both the JMA and PAGASA monitored Tropical Storm Wendy with PAGASA naming this storm Mameng PAGASA considered Wendy to have stronger winds than the JTWC despite the fact that PAGASA uses a 10 minute averaging period to measure sustained winds which generally results in a lower speed 37 Tropical Storm Wendy fueled severe rain over much of southern China in the week after it made landfall with amounts as high as 500 mm 20 in recorded in northern Jiangxi and southern Zhejiang At least 118 people were killed 47 and over 2 600 people were injured the province of Wenzhou was significantly impacted by Wendy s effects Over 500 000 people had to be evacuated over 2 2 million people had been affected by the storm and a local government spokesman called it the most serious storm in a century The direct economic damage in the region exceeded 275 million 1999 USD 47 Whilst mainland China was severely affected by Wendy the storm only had a minimal impact in Hong Kong 46 Severe Tropical Storm York Neneng edit Severe tropical storm JMA Category 1 typhoon SSHWS nbsp nbsp DurationSeptember 10 September 17Peak intensity100 km h 65 mph 10 min 980 hPa mbar Main article Tropical Storm York A tropical disturbance developed on September 10 in the western Philippine Sea but initially failed to develop as it interacted with Luzon The disturbance passed over Luzon and entered the South China Sea where it became more organized and developed into Tropical Depression 21W late on September 11 The system gradually strengthened as it moved northwest towards the Chinese coastline reaching its peak as a 130 km h 81 mph typhoon as it turned towards Hong Kong on September 16 York made landfall to the west of Hong Kong soon after and dissipated into a low pressure area over China the next day 48 Both the JMA and PAGASA monitored York as a tropical storm with PAGASA naming the system Neneng 49 As the developing depression was crossing the Philippines it brought heavy showers of up to 400 mm 16 in which caused some flooding in the Cagayan Valley 50 Eighteen people were killed in landslides in northern Luzon As Typhoon York approached and landed on Hong Kong s Lantau Island the Hong Kong Observatory HKO raised the No 10 warning for the first time since 1983 and maintained it for 11 hours the longest hoisting period on record The peak sustained winds of 150 km h 93 mph were recorded on Waglan Island and the peak gusts of 234 km h 145 mph were the highest on record there A total of 300 mm 12 in of rain fell on the territory as York passed directly over it and the resulting floods had a severe effect on agriculture throughout Hong Kong Two people died in the storm and over 500 were injured 11 seriously Some 18 000 homes lost power in the wake of the storm and 4 000 trees were uprooted Damage from York in Hong Kong exceeded 10 million USD and economic losses from the storm reached several billion Hong Kong dollars HKD Transport in the territory was severely disrupted with 470 flights cancelled and 80 000 passengers affected 51 Two ships ran aground and a cargo ship sank but all the crew were successfully rescued One person was injured in Macau and 120 incidents related to the storm were reported there After passing over Hong Kong York killed 15 and injured 700 in Guangdong with economic losses there exceeding 24 million USD 51 Ten thousand people were left stranded by flooding in China after the storm and more than 10 000 trees were uprooted in Shenzhen 52 Tropical Storm Zia edit Tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationSeptember 11 September 15Peak intensity85 km h 50 mph 10 min 985 hPa mbar The JTWC began to track a disturbance in a monsoon trough to the west of the Marianas Islands on September 11 The disturbance moved to the north without any significant development until September 13 when the outflow of the system markedly improved and it soon developed into a tropical depression to the east of Okinawa The depression strengthened further becoming Tropical Storm Zia later that day as it approached Kyushu Zia peaked with 85 km h 53 mph winds as it made landfall on the island on September 14 The storm turned to the northeast and tracked over Japan and dissipated over central Honshu the next day 53 Tropical Storm Zia brought heavy rain to western Japan which exceeded 500 mm 20 in in places The resulting flooding and landslides prompted evacuations of over 14 000 people and stranded over 1 300 tourists in a Japanese mountain resort Nine people died in Japan as a result of Tropical Storm Zia 49 Severe Tropical Storm Ann edit Severe tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationSeptember 14 September 19Peak intensity95 km h 60 mph 10 min 985 hPa mbar Tropical Depression 23W formed about 165 km 103 mi to the east of Okinawa on September 15 from a disturbance moving to the northwest under the influence of a subtropical high located on the eastern side of a monsoon trough 49 As the system developed it turned first to the northwest and then to the west becoming Tropical Storm Ann a day after forming As Ann approached the Chinese coast to the north of Shanghai on September 18 it reached its peak with 85 km h 53 mph winds and began to recurve to the northwest The storm started to weaken as it entered a higher shear environment Ann captured by a mid level trough moving through the region and turned to the east rapidly weakening as it crossed the Yellow Sea The system dissipated just off the South Korean coast near Mokpo early on September 20 54 Tropical Storm Ann brought moderate rain of up to 100 mm 3 9 in to Anhui Jiangsu and Shandong on September 18 55 Rains of up to 200 mm 7 9 in from Ann and Typhoon Bart saturated South Korea and southwestern Japan causing flooding and damage to rice paddies 56 Typhoon Bart Oniang edit Main article Typhoon Bart 1999 Very strong typhoon JMA Category 5 super typhoon SSHWS nbsp nbsp DurationSeptember 17 September 25Peak intensity165 km h 105 mph 10 min 930 hPa mbar Tropical Depression 24W developed on September 17 to the east of Taiwan The storm drifted to the northwest becoming Tropical Storm Bart on September 19 and reaching typhoon strength the next day Bart intensified further as it turned to the northeast under the influence of an upper level anticyclone 49 Typhoon Bart reached its peak on September 22 with 260 km h 160 mph winds when it passed 75 km 47 mi to the west of Okinawa becoming the only super typhoon during the 1999 Pacific typhoon season Afterwards Bart began to weaken slowly as it continued north towards Kyushu Japan which it struck on September 23 with 185 km h 115 mph winds After crossing Kyushu and western Honshu the storm accelerated to the northeast in the Sea of Japan becoming extratropical shortly before it reached northern Hokkaidō 57 As Typhoon Bart formed in PAGASA s area of responsibility it was named Oniang by PAGASA before moving to the north 49 Typhoon Bart claimed at least two lives on Okinawa and brought over 710 mm 28 in of rain to the island 57 Kadena Air Base was badly damaged by the typhoon with over 5 million of damage on the base 58 Heavy flooding and landslides led to total of a 30 deaths and over 1 000 injuries in Japan Over 800 000 homes lost power and 80 000 damaged in the aftermath of the storm The worst damage was in Kumamoto Prefecture on Kyushu where 16 people died and over 45 000 homes were damaged Bart affected the whole of Japan with some minor damages occurring in Hokkaidō shortly after the storm became extratropical 59 A large crane in Hiroshima collapsed killing three and injuring four people in the Mitsubishi plant there and the Itsukushima Shrine was also damaged 60 Damage from the storm amounted to 16 31 billion US 155 million insurance payouts reached 31 47 billion US 299 million 61 An additional 5 million 1999 USD in damage occurred to the Japanese economy 62 Tropical Storm Cam edit Tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationSeptember 22 September 26Peak intensity85 km h 50 mph 10 min 992 hPa mbar A disturbed area of weather to the south of Hong Kong in the South China Sea became more organized early on September 23 and the JTWC issued a TCFA for the system It developed into the 25th depression of the season per the JTWC a few hours later and began to track to the northeast under the influence of a mid level ridge to the east The depression gradually intensified becoming Tropical Storm Cam on September 24 Later that day the storm reached its peak winds of 75 km h 47 mph Around this time Cam s motion gradually turned towards the north As it neared the Chinese coast a strong ridge to the north turned Cam abruptly to the west towards Hong Kong and it began to weaken The JTWC issued its last warning while the storm was still at sea shortly before it made landfall over Hong Kong with 35 km h 22 mph winds The storm dissipated over China on September 26 63 As Tropical Storm Cam approached Hong Kong the HKO hoisted the No 8 Signal for the fifth time in the year the last time this had occurred was in 1964 The highest gust recorded on land was 121 km h 75 mph on Tai Mo Shan and 41 mm 1 6 in of rain fell on Hong Kong Cam was responsible for 23 injuries in Hong Kong and one death in a ship off Stonecutters Island There was limited flooding in the region and about 150 people were evacuated to emergency shelters There was some disruption to air travel into the territory with 100 flights cancelled or delayed 64 Typhoon Dan Pepang edit Main article Typhoon Dan 1999 Typhoon JMA Category 3 typhoon SSHWS nbsp nbsp DurationOctober 2 October 10Peak intensity150 km h 90 mph 10 min 955 hPa mbar Tropical Depression 26W developed over the Philippine Sea on October 1 about 750 km 470 mi to the east of Luzon The system intensified as it moved west northwest becoming Tropical Storm Dan on October 3 before reaching typhoon strength the next day Typhoon Dan reached its peak with 205 km h 127 mph early on October 5 and hit northern Luzon at that strength The typhoon weakened as it entered the South China Sea but re intensified as it turned towards the north Typhoon Dan made its second landfall near Xiamen China on October 9 and weakened overland Dan turned to the northeast and weakened to a tropical depression before it moved over the Yellow Sea late on October 10 The depression was absorbed by a frontal system over the Yellow Sea early the next day 65 Both the JMA and PAGASA treated this storm as a typhoon with PAGASA naming it Pepang 66 Typhoon Dan brought torrential rain of up to 500 mm 20 in to both northern Luzon and southern Taiwan 67 Flooding in the Philippines affected 2 600 homes and killed at least five people There was more than 2 million of damage to agriculture in the Philippines 68 Southern Taiwan was still recovering from the Chi Chi earthquake of the previous month and Dan delayed the recovery efforts The typhoon burst a dike in Kaohsiung and another in Tainan that had been damaged by the earthquake Dan knocked down a large number of trees on Kinmen which led to the disruption of 70 of the island s power supply Several fishing boats were sunk and house damaged on Penghu 69 Thirty four died and 1 400 people were injured as a result of the storm in Fujian 1 500 houses were destroyed and 240 million of damage occurred in the province 68 Dan was the worst typhoon to hit Xiamen in 46 years killing five and injuring over 100 in the city 65 Tropical Storm Eve Rening edit See also 1999 Vietnamese floods Tropical storm JMA Tropical storm SSHWS nbsp nbsp DurationOctober 15 October 20Peak intensity85 km h 50 mph 10 min 990 hPa mbar A broad area of convection to the northeast of Mindanao over the Philippine Sea began to develop on October 15 as it moved to the west becoming Tropical Depression 27W The depression made landfall on Samar Island the same day and moved to the northwest across the central Philippines throughout October 6 The depression turned to the west after it emerged into the South China Sea and turned to the southwest on October 18 in response to increasing mid level ridging over southeastern China As it neared the Vietnamese coast the depression strengthened slightly and became Tropical Storm Eve Eve made landfall 110 km 68 mi southeast of Da Nang as a minimal tropical storm on October 19 and quickly dissipated overland 70 Both the JMA and PAGASA considered Eve a tropical storm with PAGASA naming it Rening 66 Tropical Storm Eve brought torrential rain to much of central Vietnam with about 290 mm 11 in falling on Huế City and as much as 470 mm 19 in of rain falling in parts of Ha Tĩnh Province 71 Eve was the first in a series of storms to bring torrential rain to the region and the resulting floods killed over 590 people and they also caused nearly 235 million of damage directly 70 Tropical Depression 28W edit Tropical depression JMA Tropical depression SSHWS nbsp nbsp DurationNovember 5 November 6Peak intensity55 km h 35 mph 10 min 1000 hPa mbar A tropical disturbance began to develop 45 km 28 mi to the southeast of Agrihan an island of the Northern Mariana Islands early on November 5 from the tail end of shear line connected to a front that ran to Japan It strengthened into Tropical Depression 28W early the next day and moved to the northeast along the shear line reaching its peak with 55 km h 34 mph winds The depression did not develop further but its motion accelerated and it became an extratropical low 18 hours after forming 72 Tropical Depression Frankie Sendang edit Tropical depression JMA Tropical storm SSHWS nbsp nbsp DurationNovember 6 November 10Peak intensity55 km h 35 mph 10 min 994 hPa mbar A disturbance to the northeast of Koror in the Philippine Sea developed as it moved to the west on November 6 becoming Tropical Depression 29W The depression moved rapidly to the west under the influence of the subtropical ridge to the north crossing Samar early on November 8 The system strengthened over the central Philippines becoming Tropical Storm Frankie The influence of a developing ridge to the southeast led to Frankie becoming quasi stationary over the Sibuyan Sea The storm soon weakened due to increasing wind shear and interaction with land and it dissipated on November 11 73 PAGASA tracked Frankie as a tropical storm naming it Sendang The JMA considered this storm to have been a tropical depression 74 Tropical Storm Frankie brought heavy rain of up to 300 mm 12 in to the central Philippines that disrupted the rice harvest 75 Flooding from the storm forced the evacuation of 300 families in Calbayog 76 Severe Tropical Storm Gloria Trining edit Severe tropical storm JMA Category 1 typhoon SSHWS nbsp nbsp DurationNovember 13 November 16Peak intensity95 km h 60 mph 10 min 980 hPa mbar In mid November a persistent area of circulation developed at the end of a shear line to the east of Samar It began to become more organized as it moved to the north on November 12 and became a tropical depression the next day The cyclone continued to slowly intensify becoming Tropical Storm Gloria as it turned the northeast when it was well to the east of Luzon Gloria began to accelerate to the northeast under the influence of an upper level flow and maintained its strength The storm passed east of Okinawa on November 15 when the shear markedly reduced and allowed a rapid intensification to typhoon strength Gloria briefly peaked as a 120 km h 75 mph typhoon later that day before weakening as it started to become extratropical Typhoon Gloria became fully extratropical on November 16 having weakened back into a tropical storm 77 Both the JMA and PAGASA monitored Gloria with PAGASA naming the storm Trining The JMA assessed Gloria as being a severe tropical storm at its peak strength on November 15 74 Typhoon Gloria did not approach land closely Gloria is the last name to use English names in the basin Tropical Depression 31W edit Tropical depression SSHWS nbsp nbsp DurationDecember 1 December 4 Exited basin Peak intensity55 km h 35 mph 1 min 1000 hPa mbar An area of low pressure just off Palawan became more organized as it moved to the northwest away from the island becoming Tropical Depression 31W early on December 1 A subtropical ridge to the north of the system caused it to move southwest through the South China Sea and off the Vietnamese coast Winds from the depression peaked at 55 km h 34 mph Early on December 3 when the storm was to the south of Vietnam it turned to the northwest and headed towards the Malay Peninsula The depression made landfall in Thailand to the northeast of Phuket on December 4 and the JTWC ceased advisories as the storm weakened overland The remnants entered the Andaman Sea but redevelopment did not occur 78 Tropical Depression 32W edit Tropical depression SSHWS nbsp nbsp DurationDecember 9 December 11Peak intensity55 km h 35 mph 1 min 1000 hPa mbar Tropical Depression 32W developed on December 9 in the South China Sea between Palawan and Borneo and slowly moved to the west After the depression reached its peak with 55 km h 34 mph winds it began to accelerate to the west By December 11 when the storm was to the south of Vietnam it became more sheared and the low level circulation became exposed The system dissipated soon afterwards having never approached land 79 Tropical Depression 33W edit Tropical depression HKO Tropical depression SSHWS nbsp nbsp DurationDecember 14 December 16Peak intensity55 km h 35 mph 10 min 1000 hPa mbar On December 14 Tropical Depression 33W formed within a persistent trough about 425 km 264 mi to the east of Cam Ranh Bay Vietnam A high level of wind shear restricted the storm s strength to 55 km h 34 mph which it maintained as it moved west towards Vietnam The storm turned to the north shortly before it made landfall on December 16 and dissipated soon after over Vietnam under the influence of increased wind shear and interaction with land It is unknown if the storm had any effects on land 80 Other systems editOn October 21 an area of convection formed in the Sulu Sea and emerged over the South China Sea on the next day Thunderstorm activity started to increase and the Joint Typhoon Warning Center issued a Tropical Cyclone Formation Alert TCFA on the system However the low failed to develop further and this caused the cancellation of the TCFA On October 24 the low crossed the Malay Peninsula and emerged into the North Indian Ocean On the next day while over the Andaman Sea the low became a tropical depression which became the deadly 1999 Odisha cyclone Storm names editSee also Lists of tropical cyclone names and Tropical cyclone naming During the season 21 named tropical cyclones developed in the Western Pacific and were named by the Joint Typhoon Warning Center when it was determined that they had become tropical storms These names were contributed to a revised list from 1996 However the agency stopped naming cyclones after this season as the Japan Meteorological Agency started naming systems Consequently this was the last year the following lists were used Hilda Iris Jacob Kate Leo Maggie Neil Olga Paul Rachel Sam TanyaVirgil Wendy York Zia Ann Bart Cam Dan Eve Frankie GloriaPhilippines edit Auring Bebeng Karing Diding EtangGening Helming Ising Luding MamengNeneng Oniang Pepang Rening SendangTrining Ulding unused Warling unused Yayang unused Auxiliary listAding unused Barang unused Krising unused Dadang unused Erling unused Goying unused The Philippine Atmospheric Geophysical and Astronomical Services Administration uses its own naming scheme for tropical cyclones in their area of responsibility PAGASA assigns names to tropical depressions that form within their area of responsibility and any tropical cyclone that might move into their area of responsibility Should the list of names for a given year prove to be insufficient names are taken from an auxiliary list the first 10 of which are published each year before the season starts This is the same list used for the 1995 season PAGASA uses its own naming scheme that starts in the Filipino alphabet with names of Filipino female names ending with ng A B K D etc Because PAGASA started a new naming scheme in 2001 therefore this naming list would not be used in the 2003 season Names that were not assigned going to use are marked in gray Season effects editThis table summarizes all the systems that developed within or moved into the North Pacific Ocean to the west of the International Date Line during 1999 The tables also provide an overview of a systems intensity duration land areas affected and any deaths or damages associated with the system Name Dates Peak intensity Areas affected Damage USD Deaths RefsCategory Wind speed PressureHilda Auring January 3 8 Tropical depression 55 km h 34 mph 1000 hPa 29 53 inHg Malaysia 1 3 million 5TD February 9 10 Tropical depression Not specified 1004 hPa 29 65 inHg None None NoneIris Bebeng February 14 19 Tropical depression 55 km h 34 mph 1000 hPa 29 53 inHg None None NoneJacob Karing April 7 10 Tropical depression 55 km h 34 mph 1006 hPa 29 71 inHg Philippines None NoneKate Diding April 21 28 Severe tropical storm 100 km h 62 mph 980 hPa 28 94 inHg Philippines None NoneLeo April 27 May 2 Strong typhoon 120 km h 75 mph 970 hPa 28 64 inHg South China None NoneMaggie Etang June 1 9 Strong typhoon 120 km h 75 mph 970 hPa 28 64 inHg Philippines Taiwan South China 168 million 9TD June 1 2 Tropical depression Not specified 1004 hPa 29 65 inHg None None NoneGening June 3 6 Tropical depression 55 km h 34 mph 996 hPa 29 41 inHg None None NoneTD July 9 15 Tropical depression 55 km h 34 mph 996 hPa 29 41 inHg Japan None None07W July 14 18 Tropical storm 65 km h 40 mph 996 hPa 29 41 inHg None None None08W July 19 23 Tropical depression Not specified 1004 hPa 29 65 inHg None None NoneNeil Heling July 22 28 Severe tropical storm 95 km h 59 mph 980 hPa 28 94 inHg Japan Korea None 1510W July 23 28 Tropical storm 75 km h 47 mph 985 hPa 29 09 inHg China None NoneOlga Ising July 29 August 3 Strong typhoon 120 km h 75 mph 970 hPa 28 64 inHg Caroline Islands Ryukyu Islands Korea 657 million 106Paul August 3 9 Tropical storm 85 km h 53 mph 980 hPa 28 94 inHg Mariana Islands Japan South Korea China None NoneRachel August 5 11 Tropical storm 65 km h 40 mph 992 hPa 29 29 inHg Taiwan Ryukyu Islands China None None14W August 7 11 Tropical depression Not specified 1004 hPa 29 65 inHg Japan None NoneTD August 9 11 Tropical depression Not specified 1000 hPa 29 53 inHg None None NoneTD August 11 Tropical depression Not specified 1000 hPa 29 53 inHg None None NoneTD August 11 16 Tropical depression Not specified 1000 hPa 29 53 inHg Japan None None15W August 14 20 Tropical depression Not specified 1000 hPa 29 53 inHg Japan None NoneTD August 16 17 Tropical depression Not specified 1010 hPa 29 83 inHg None None NoneSam Luding August 18 24 Severe tropical storm 100 km h 62 mph 980 hPa 28 94 inHg Philippines South China 35 million 20Tanya August 19 24 Severe tropical storm 95 km h 59 mph 1000 hPa 29 53 inHg Wake Island None NoneDora August 20 26 Severe tropical storm 95 km h 59 mph 990 hPa 29 23 inHg Wake Island None None18W August 21 24 Tropical depression Not specified 1010 hPa 29 83 inHg None None NoneVirgil August 23 29 Severe tropical storm 95 km h 59 mph 1000 hPa 29 53 inHg None None NoneTD August 30 Tropical depression Not specified 1008 hPa 29 77 inHg None None NoneWendy Mameng September 1 7 Tropical storm 65 km h 40 mph 990 hPa 29 23 inHg Philippines China 309 million 133York Neneng September 9 17 Severe tropical storm 100 km h 62 mph 980 hPa 28 94 inHg Philippines South China 34 million 35Zia September 11 15 Tropical storm 65 km h 40 mph 990 hPa 29 23 inHg Philippines China None NoneAnn September 14 19 Severe tropical storm 95 km h 59 mph 985 hPa 29 09 inHg East China None NoneBart Oniang September 17 25 Very strong typhoon 165 km h 103 mph 930 hPa 27 46 inHg Japan 155 million 36TD September 21 Tropical depression Not specified 1008 hPa 29 77 inHg None None NoneCam September 22 26 Tropical storm 85 km h 53 mph 992 hPa 29 29 inHg South China None 1Dan Pepang October 2 10 Strong typhoon 150 km h 93 mph 955 hPa 28 20 inHg Philippines Taiwan China South Korea 242 million 44Eve Rening October 15 20 Tropical storm 85 km h 53 mph 990 hPa 29 23 inHg Philippines Vietnam 235 million 590TD October 23 24 Tropical depression Not specified 1004 hPa 29 65 inHg Vietnam Thailand None NoneTD November 5 Tropical depression Not specified 1002 hPa 29 59 inHg Vietnam None None28W November 5 8 Tropical depression 55 km h 34 mph 1000 hPa 29 53 inHg Mariana Islands None NoneFrankie Sendang November 6 11 Tropical depression 55 km h 34 mph 994 hPa 29 35 inHg Philippines None NoneGloria Trining November 13 16 Severe tropical storm 95 km h 59 mph 980 hPa 28 94 inHg None None None31W December 1 4 Tropical depression 55 km h 34 mph 1004 hPa 29 65 inHg Thailand None None32W December 8 10 Tropical depression 55 km h 34 mph 1002 hPa 29 59 inHg None None None33W December 14 16 Tropical depression 55 km h 34 mph 1000 hPa 29 53 inHg Vietnam None NoneSeason aggregates46 systems January 3 December 16 1999 165 km h 103 mph 930 hPa 27 46 inHg 1 84 billion 976See also edit nbsp Tropical cyclones portal1999 Pacific hurricane season 1999 Atlantic hurricane season 1999 2000 Australian region cyclone season 1999 2000 South Pacific cyclone season 1999 2000 South West Indian Ocean cyclone seasonReferences edit Joint Typhoon Warning Center Bwp011999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 Padgett Gary Monthly Global Tropical Cyclone Summary January 1999 Archived from the original on 2007 02 09 Retrieved 2007 02 17 Pederoso Wayne Effects of Tropical Storm Hilda on Sea Turtles in Sipadan Sabah Malaysia Universiti Malaysia Sabah Research Project Archived from the original on 2013 09 28 Retrieved 2013 08 19 Borneo Bulletin 1999 01 11 Hilda causes RM15 mil in road damages in Sabah a b Padgett Gary Monthly Global Tropical Cyclone Summary February 1999 Archived from the original on 2007 02 09 Retrieved 2007 02 17 Joint Typhoon Warning Center Bwp021999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 Joint Typhoon Warning Center Bwp031999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 a b Padgett Gary Monthly Global Tropical Cyclone Summary April 1999 Archived from the original on 2007 02 09 Retrieved 2007 02 17 Climate Prediction Center 1999 04 10 Weekly Global Climate Highlights Archived from the original on 2006 10 11 Retrieved 2007 02 18 Joint Typhoon Warning Center Bwp041999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 Climate Prediction Center 1999 04 24 Weekly Global Climate Highlights Archived from the original on 2006 10 11 Retrieved 2007 02 18 Joint Typhoon Warning Center Typhoon Kate 04W PDF 1999 Annual Tropical Cyclone Report p 25 Archived from the original PDF on 2016 12 24 Retrieved 2013 10 06 Joint Typhoon Warning Center Bwp051999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 Climate Prediction Center 1999 05 01 Weekly Global Climate Highlights Archived from the original on 2006 10 11 Retrieved 2007 02 18 Hong Kong Observatory April 2000 Typhoon Leo 9902 PDF Tropical cyclones in 1999 pp 36 40 Archived from the original PDF on 2011 05 24 Retrieved 2007 02 18 Joint Typhoon Warning Center Bwp061999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 Padgett Gary Monthly Global Tropical Cyclone Summary June 1999 Archived from the original on 2007 02 09 Retrieved 2007 02 17 a b Hong Kong Observatory Typhoon Maggie 9903 2 8 June 1999 PDF 1999 Hong Kong Observatory Report Archived from the original PDF on 26 September 2013 Retrieved 2013 08 19 USDA NOAA 1999 06 15 Weekly Weather and Crop Bulletin PDF p 26 Archived from the original pdf on 2006 09 20 Retrieved 2007 02 17 Joint Typhoon Warning Center Bwp071999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Depression 08W PDF 1999 Annual Tropical Cyclone Report p 45 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Bwp091999 txt 1999 Joint Typhoon Warning Center Best Track Retrieved 2013 08 19 a b c d Padgett Gary Monthly Global Tropical Cyclone Summary July 1999 Archived from the original on 23 March 2007 Retrieved 2007 02 17 Joint Typhoon Warning Center Tropical Storm Neil 09W PDF 1999 Annual Tropical Cyclone Report p 48 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Newman Steve 1999 08 06 Earthweek A Diary of the Planet CNN Retrieved 2007 02 18 Joint Typhoon Warning Center Tropical Depression 10W PDF 1999 Annual Tropical Cyclone Report p 53 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Hong Kong Observatory April 2000 Tropical Storm 9906 PDF Tropical cyclones in 1999 pp 50 54 Archived from the original PDF on 2011 05 24 Retrieved 2007 02 18 a b c Joint Typhoon Warning Center Typhoon Olga 11W PDF 1999 Annual Tropical Cyclone Report p 56 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 a b Dartmouth Flood Observatory 1999 Flood Archive Archived from the original on 2008 02 26 Retrieved 2007 02 18 USDA NOAA 1999 08 10 Weekly Weather and Crop Bulletin PDF p 29 Archived from the original pdf on 2006 09 16 Retrieved 2007 02 17 Staff Writer 1999 08 06 High alert as typhoon threatens BBC Retrieved 2007 02 18 a b Joint Typhoon Warning Center Tropical Storm Paul 12W PDF 1999 Annual Tropical Cyclone Report p 63 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Storm Rachel 13W PDF 1999 Annual Tropical Cyclone Report p 68 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Depression 14W PDF 1999 Annual Tropical Cyclone Report p 70 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Depression 15W PDF 1999 Annual Tropical Cyclone Report p 73 Archived from the original PDF on 2016 12 24 Retrieved 2007 02 17 a b c Joint Typhoon Warning Center Typhoon Sam 16W PDF 1999 Annual Tropical Cyclone Report p 76 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 a b c Padgett Gary Monthly Global Tropical Cyclone Summary August 1999 Archived from the original on 23 March 2007 Retrieved 2007 02 17 a b Hong Kong Observatory April 2000 Typhoon Sam 9910 PDF Tropical cyclones in 1999 pp 56 66 Archived from the original PDF on 2011 05 24 Retrieved 2007 02 17 Civil Aviation Department Hong Kong December 2004 Aircraft Accident Report 1 2004 PDF Retrieved 2007 02 17 a b Joint Typhoon Warning Center Typhoon Tanya 17W PDF 1999 Annual Tropical Cyclone Report p 81 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Hurricane Dora 07E PDF 1999 Annual Tropical Cyclone Report p 139 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Lawrence Miles Kimberlain Todd Preliminary Report Hurricane Dora National Hurricane Center Retrieved 2007 02 17 Joint Typhoon Warning Center Tropical Depression 18W PDF 1999 Annual Tropical Cyclone Report p 84 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Typhoon Virgil 19W PDF 1999 Annual Tropical Cyclone Report p 86 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Japan Meteorological Agency Bst9099 txt 1990 1999 RSMC Tokyo Best Track Data Text Archived from the original on 2013 01 22 Retrieved 2013 09 26 a b Joint Typhoon Warning Center Tropical Storm Wendy 20W PDF 1999 Annual Tropical Cyclone Report p 89 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 a b Staff Writer 1999 09 07 Wendy Death Toll Hits 133 China Daily Retrieved 2007 02 18 Joint Typhoon Warning Center Typhoon York 21W PDF 1999 Annual Tropical Cyclone Report p 92 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 a b c d e Padgett Gary Monthly Global Tropical Cyclone Summary September 1999 Archived from the original on 23 March 2007 Retrieved 2007 02 17 USDA NOAA 1999 09 14 Weekly Weather and Crop Bulletin PDF p 26 Archived from the original pdf on 2006 09 19 Retrieved 2007 02 17 a b Hong Kong Observatory April 2000 Typhoon York 9915 PDF Tropical cyclones in 1999 pp 73 83 Archived from the original PDF on 2011 05 24 Retrieved 2007 02 18 Staff Writer 1999 09 17 China typhoon strands thousands BBC Retrieved 2007 02 17 Joint Typhoon Warning Center Tropical Storm Zia 22W PDF 1999 Annual Tropical Cyclone Report p 95 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Storm Ann 23W PDF 1999 Annual Tropical Cyclone Report p 98 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Climate Prediction Center 1999 09 18 Weekly Global Climate Highlights Archived from the original on 2006 10 11 Retrieved 2007 02 18 USDA NOAA 1999 09 28 Weekly Weather and Crop Bulletin PDF p 21 Archived from the original pdf on 2006 09 21 Retrieved 2007 02 17 a b Joint Typhoon Warning Center Super Typhoon Bart 24W PDF 1999 Annual Tropical Cyclone Report p 102 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Major D Lehosit 1999 Super Typhoon Bart Blasts Kadena PDF The U S Air Force Civil Engineer p 8 Archived from the original PDF on 2007 02 02 Retrieved 2007 02 19 Fire and Disaster Management Agency 1999 10 19 ȏ h 平成11年 9月21日からの大雨による被害状況について 第30報 台風第18号の被害を含む in Japanese Archived from the original on 17 February 2007 Retrieved 2007 02 19 Staff Writer 1999 09 24 26 killed in typhoon off west coast of Japan Radio Telefis Eireann Retrieved 2007 02 17 Digital Typhoon Typhoon 199918 BART Disaster Information agora ex nii ac jp Retrieved 2021 02 07 Munich Re 2002 Insured losses of 1 billion and above PDF Annual Review Natural Catastrophes 2001 p 19 Archived from the original PDF on 2007 09 28 Retrieved 2007 02 19 Joint Typhoon Warning Center Tropical Storm Cam 25W PDF 1999 Annual Tropical Cyclone Report p 108 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Hong Kong Observatory April 2000 Severe Tropical Storm Cam 9919 PDF Tropical cyclones in 1999 pp 85 90 Archived from the original PDF on 2011 05 24 Retrieved 2007 02 17 a b Joint Typhoon Warning Center Typhoon Dan 26W PDF 1999 Annual Tropical Cyclone Report p 111 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 a b Padgett Gary Monthly Global Tropical Cyclone Summary October 1999 Archived from the original on 23 March 2007 Retrieved 2007 02 17 Climate Prediction Center 1999 10 09 Weekly Global Climate Highlights Archived from the original on 2006 10 11 Retrieved 2007 02 18 a b Hong Kong Observatory April 2000 Typhoon Dan 9920 PDF Tropical cyclones in 1999 pp 92 95 Archived from the original PDF on 2011 05 24 Retrieved 2007 02 18 Staff Writer 1999 10 10 Typhoon Dan downs power lines uproots trees in the south Taipei Times Retrieved 2007 02 18 a b Joint Typhoon Warning Center Tropical Storm Eve 27W PDF 1999 Annual Tropical Cyclone Report p 119 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Asian Disaster Preparedness Center 2003 11 30 Local Institutions Response to 1999 Flood Event in Central Vietnam The role of local institutions in reducing vulnerability to recurrent natural disasters and in sustainable livelihoods development Vietnam case study FAO Retrieved 2007 02 17 Joint Typhoon Warning Center Tropical Depression 28W PDF 1999 Annual Tropical Cyclone Report p 122 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Storm Frankie 29W PDF 1999 Annual Tropical Cyclone Report p 124 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 a b Padgett Gary Monthly Global Tropical Cyclone Summary November 1999 Archived from the original on 23 March 2007 Retrieved 2007 02 17 USDA NOAA 1999 11 16 Weekly Weather and Crop Bulletin PDF p 20 Archived from the original pdf on 2006 09 22 Retrieved 2007 02 17 Newman Steve 1999 11 12 Earthweek A Diary of the Planet CNN Retrieved 2007 02 18 Joint Typhoon Warning Center Typhoon Gloria 30W PDF 1999 Annual Tropical Cyclone Report p 127 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Depression 31W PDF 1999 Annual Tropical Cyclone Report p 131 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Depression 32W PDF 1999 Annual Tropical Cyclone Report p 135 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 Joint Typhoon Warning Center Tropical Depression TD 33W PDF 1999 Annual Tropical Cyclone Report p 137 Archived from the original PDF on 2016 12 24 Retrieved 2013 08 19 External links edit nbsp Wikimedia Commons has media related to 1999 Pacific typhoon season Japan Meteorological Agency Joint Typhoon Warning Center Archived 2010 03 01 at the Wayback Machine China Meteorological Agency National Weather Service Guam Hong Kong Observatory Macau Meteorological Geophysical Services Korea Meteorological Agency Philippine Atmospheric Geophysical and Astronomical Services Administration Taiwan Central Weather Bureau Satellite movie of 1999 Pacific typhoon season Retrieved from https en wikipedia org w index php title 1999 Pacific typhoon season amp oldid 1183415827 Severe Tropical Storm Virgil, wikipedia, wiki, book, books, library,

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