fbpx
Wikipedia

Extreme weather

Extreme weather includes unexpected, unusual, severe, or unseasonal weather; weather at the extremes of the historical distribution—the range that has been seen in the past.[1][2] Extreme events are based on a location's recorded weather history. They are defined as lying in the most unusual ten percent (10th or 90th percentile of a probability density function).[2] The main types of extreme weather include heat waves, cold waves and heavy precipitation or storm events, such as tropical cyclones. The effects of extreme weather events are economic costs, loss of human lives, droughts, floods, landslides. Severe weather is a particular type of extreme weather which poses risks to life and property.

A tornado is an example for an extreme weather event. This tornado struck Anadarko, Oklahoma during a tornado outbreak in 1999.

Climate change is increasing the periodicity and intensity of some extreme weather events.[3] Confidence in the attribution of extreme weather and other events to anthropogenic climate change is highest in changes in frequency or magnitude of extreme heat and cold events with some confidence in increases in heavy precipitation and increases in the intensity of droughts.[4] Current evidence and climate models show that an increasing global temperature will intensify extreme weather events around the globe, thereby amplifying human loss, damages and economic costs, and ecosystem destruction.

Extreme weather has significant impacts on human society as well as natural ecosystems. For example, a global insurer Munich Re estimates that natural disasters cause more than $90 in billion global direct losses in 2015.[5] Some human activities can exacerbate the effects, for example poor urban planning, wetland destruction, and building homes along floodplains.

Definition edit

Extreme weather describes unusual weather events that are at the extremes of the historical distribution for a given area.[2]: 2908  The IPCC Sixth Assessment Report defines an extreme weather event as follows: "An event that is rare at a particular place and time of year. Definitions of 'rare' vary, but an extreme weather event would normally be as rare as or rarer than the 10th or 90th percentile of a probability density function estimated from observations."[2]: 2908 

In comparison, the term severe weather is any aspect of the weather that poses risks to life, property or requires the intervention of authorities.[citation needed] Severe weather is thus a particular type of extreme weather.

Types edit

Definitions of extreme weather vary in different parts of the community, changing the outcomes of research from those fields.[5]

Heat waves edit

 
2003 European heat wave

Heat waves are periods of abnormally high temperatures and heat index. Definitions of a heatwave vary because of the variation of temperatures in different geographic locations.[6] Excessive heat is often accompanied by high levels of humidity, but can also be catastrophically dry.[7]

Because heat waves are not visible as other forms of severe weather, like hurricanes, tornadoes, and thunderstorms, they are one of the less known forms of extreme weather.[8] Severely hot weather can damage populations and crops due to potential dehydration or hyperthermia, heat cramps, heat expansion, and heat stroke. Dried soils are more susceptible to erosion, decreasing lands available for agriculture. Outbreaks of wildfires can increase in frequency as dry vegetation has an increased likelihood of igniting. The evaporation of bodies of water can be devastating to marine populations, decreasing the size of the habitats available as well as the amount of nutrition present within the waters. Livestock and other animal populations may decline as well.

During excessive heat, plants shut their leaf pores (stomata), a protective mechanism to conserve water but also curtails plants' absorption capabilities. This leaves more pollution and ozone in the air, which leads to higher mortality in the population. It has been estimated that extra pollution during the hot summer of 2006 in the UK, cost 460 lives.[9] The European heat waves from summer 2003 are estimated to have caused 30,000 excess deaths, due to heat stress and air pollution.[10] Over 200 U.S cities have registered new record high temperatures.[11] The worst heat wave in the US occurred in 1936 and killed more than 5000 people directly. The worst heat wave in Australia occurred in 1938–39 and killed 438. The second worst was in 1896.

Power outages can also occur within areas experiencing heat waves due to the increased demand for electricity (i.e. air conditioning use).[12] The urban heat island effect can increase temperatures, particularly overnight.[13]

Cold waves edit

 
Cold wave in continental North America from Dec. 3–10, 2013. Red color means above mean temperature; blue represents below normal temperature.

A cold wave is a weather phenomenon that is distinguished by a cooling of the air. Specifically, as used by the U.S. National Weather Service, a cold wave is a rapid fall in temperature within a 24-hour period requiring substantially increased protection for agriculture, industry, commerce, and social activities. The precise criterion for a cold wave is determined by the rate at which the temperature falls, and the minimum to which it falls. This minimum temperature is dependent on the geographical region and time of year.[14] Cold waves generally are capable of occurring at any geological location and are formed by large cool air masses that accumulate over certain regions, caused by movements of air streams.[6]

A cold wave can cause death and injury to livestock and wildlife. Exposure to cold mandates greater caloric intake for all animals, including humans, and if a cold wave is accompanied by heavy and persistent snow, grazing animals may be unable to reach necessary food and water, and die of hypothermia or starvation. Cold waves often necessitate the purchase of fodder for livestock at a considerable cost to farmers.[6] Human populations can be inflicted with frostbite when exposed for extended periods of time to cold and may result in the loss of limbs or damage to internal organs.

Extreme winter cold often causes poorly insulated water pipes to freeze. Even some poorly protected indoor plumbing may rupture as frozen water expands within them, causing property damage. Fires, paradoxically, become more hazardous during extreme cold. Water mains may break and water supplies may become unreliable, making firefighting more difficult.[6]

Cold waves that bring unexpected freezes and frosts during the growing season in mid-latitude zones can kill plants during the early and most vulnerable stages of growth. This results in crop failure as plants are killed before they can be harvested economically. Such cold waves have caused famines. Cold waves can also cause soil particles to harden and freeze, making it harder for plants and vegetation to grow within these areas. One extreme was the so-called Year Without a Summer of 1816, one of several years during the 1810s in which numerous crops failed during freakish summer cold snaps after volcanic eruptions reduced incoming sunlight.

In some cases more frequent extremely cold winter weather – i.e. across parts of Asia and North America including the February 2021 North American cold wavecan be a result of climate change such as due to changes in the Arctic.[15][16] However, conclusions that link climate change to cold waves are considered to still be controversial.[17][unreliable source?][additional citation(s) needed] The JRC PESETA IV project concluded in 2020 that overall climate change will result in a decline in the intensity and frequency of extreme cold spells, with milder winters reducing fatalities from extreme cold,[18][additional citation(s) needed] even if individual cold extreme weather may sometimes be caused by changes due to climate change and possibly even become more frequent in some regions. According to a 2023 study, "weak extreme cold events (ECEs) significantly decrease in frequency, projection area and total area over the north hemisphere with global warming. However, the frequency, projection area and total area of strong ECEs show no significant trend, whereas they are increasing in Siberia and Canada."[19]

Heavy rain and storms edit

Tropical cyclones edit

NASA film In Katrina's Wake, covering the impacts from Hurricane Katrina.

A tropical cyclone is a rapidly rotating storm system characterized by a low-pressure center, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is referred to by different names, including hurricane (/ˈhʌrɪkən, -kn/), typhoon (/tˈfn/), tropical storm, cyclonic storm, tropical depression, or simply cyclone. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean, and a typhoon occurs in the northwestern Pacific Ocean. In the Indian Ocean and South Pacific, comparable storms are referred to as "tropical cyclones". In modern times, on average around 80 to 90 named tropical cyclones form each year around the world, over half of which develop hurricane-force winds of 65 kn (120 km/h; 75 mph) or more.[20] Tropical cyclones carry heat and energy away from the tropics and transport it towards temperate latitudes, which plays an important role in regulating global climate.

Tropical cyclones typically form over large bodies of relatively warm water. They derive their energy through the evaporation of water from the ocean surface, which ultimately condenses into clouds and rain when moist air rises and cools to saturation. This energy source differs from that of mid-latitude cyclonic storms, such as nor'easters and European windstorms, which are powered primarily by horizontal temperature contrasts. Tropical cyclones are typically between 100 and 2,000 km (62 and 1,243 mi) in diameter.

Causes and attribution edit

Generally speaking, one event in extreme weather cannot be attributed to any one cause; however, certain system wide changes to global weather systems can lead to increased frequency or intensity of extreme weather events.[5]

Natural variability edit

Aspects of our climate system have a certain level of natural variability, and extreme weather events can occur for several reasons beyond human impact, including changes in pressure or the movement of air. Areas along the coast or located in tropical regions are more likely to experience storms with heavy precipitation than temperate regions, although such events can occur. Not every unusual weather event can be blamed on climate change. The atmosphere is a complex and dynamic system, influenced by several factors such as the natural tilt and orbit of the Earth, the absorption or reflection of solar radiation, the movement of air masses, and the hydrologic cycle. Due to this, weather patterns can experience some variation, and so extreme weather can be attributed, at least in part, to the natural variability that exists on Earth. Climatic variations such as the El Niño-Southern Oscillation or the North Atlantic Oscillation impact weather patterns in specific regions of the world, influencing temperature and precipitation.[21] The record-breaking extreme weather events that have been catalogued throughout the past two hundred years most likely arise when climate patterns like ENSO or NAO work "in the same direction as human‐induced warming."[21]

Climate change edit

 
The IPCC Sixth Assessment Report (2021) projects progressively large increases in both the frequency (horizontal bars) and intensity (vertical bars) of extreme weather events, for increasing degrees of global warming—including more than a 5 °C increase in extreme heat events for a 4 °C global average temperature increase.[22]

Some studies assert a connection between rapidly warming arctic temperatures and thus a vanishing cryosphere to extreme weather in mid-latitudes.[23][24][25][26] In a study published in Nature in 2019, scientists used several simulations to determine that the melting of ice sheets in Greenland and Antarctica could affect overall sea level and sea temperature.[27] Other models have shown that modern temperature rise and the subsequent addition of meltwater to the ocean could lead to a disruption of the thermohaline circulation, which is responsible for the movement of seawater and distribution of heat around the globe.[28] A collapse of this circulation in the northern hemisphere could lead to an increase in extreme temperatures in Europe, as well as more frequent storms by throwing off natural climate variability and conditions.[28] Thus, as increasing temperatures cause glaciers to melt, mid-latitudes could experience shifts in weather patterns or temperatures.[28]

There were around 6,681 climate-related events reported during 2000-2019, compared to 3,656 climate-related events reported during 1980–1999.[29] In this report, a 'climate-related event' refers to floods, storms, droughts, landslides, extreme temperatures (like heat waves or freezes), and wildfires; it excludes geophysical events such as volcanic eruptions, earthquakes, or mass movements.[29] While there is evidence that a changing global climate, such as an increase in temperature, has impacted the frequency of extreme weather events, the most significant effects are likely to arise in the future. This is where climate models are useful, for they can provide simulations of how the atmosphere may behave over time and what steps need to be taken in the present day to mitigate any negative changes.[30]

The increasing probability of record week-long heat extremes occurrence depends on warming rate, rather than global warming level.[31][32]

Some researchers attribute increases in extreme weather occurrences to more reliable reporting systems.[29] A difference in what qualifies as 'extreme weather' in varying climate systems could also be argued. Over or under reporting of casualties or losses can lead to inaccuracy in the impact of extreme weather. However, the UN reports show that, although some countries have experienced greater effects, there have been increases in extreme weather events on all continents.[29] Current evidence and climate models show that an increasing global temperature will intensify extreme weather events around the globe, thereby amplifying human loss, damages and economic costs, and ecosystem destruction.[citation needed]

Tropical cyclones and climate change edit

In 2020, the National Oceanic and Atmospheric Administration (NOAA) of the U.S. government predicted that, over the 21st Century, the frequency of tropical storms and Atlantic hurricanes would decline by 25 percent while their maximum intensity would rise by 5 percent.[33]

 
North Atlantic tropical cyclone activity according to the Power Dissipation Index, 1949–2015. Sea surface temperature has been plotted alongside the PDI to show how they compare. The lines have been smoothed using a five-year weighted average, plotted at the middle year.

Climate change can affect tropical cyclones in a variety of ways: an intensification of rainfall and wind speed, a decrease in overall frequency, an increase in the frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human-induced climate change.[34] Tropical cyclones use warm, moist air as their source of energy or "fuel". As climate change is warming ocean temperatures, there is potentially more of this fuel available.[35]

Between 1979 and 2017, there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the Saffir–Simpson scale. The trend was most clear in the North Atlantic and in the Southern Indian Ocean. In the North Pacific, tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period.[36] With 2 °C (3.6 °F) warming, a greater percentage (+13%) of tropical cyclones are expected to reach Category 4 and 5 strength.[34] A 2019 study indicates that climate change has been driving the observed trend of rapid intensification of tropical cyclones in the Atlantic basin. Rapidly intensifying cyclones are hard to forecast and therefore pose additional risk to coastal communities.[37]

Human activities that exacerbate the effects edit

There are plenty of anthropogenic activities that can exacerbate the effects of extreme weather events. Urban planning often amplifies urban flooding impacts, especially in areas that are at increased risk of storms due to their location and climate variability. First, increasing the amount of impervious surfaces, such as sidewalks, roads, and roofs, means that less of the water from incoming storms is absorbed by the land.[38] The destruction of wetlands, which act as a natural reservoir by absorbing water, can intensify the impact of floods and extreme precipitation.[39] This can happen both inland and at the coast. However, wetland destruction along the coast can mean decreasing an area's natural 'cushion,' thus allowing storm surges and flood waters to reach farther inland during hurricanes or cyclones.[40] Building homes below sea level or along a floodplain puts residents at increased risk of destruction or injury in an extreme precipitation event.

More urban areas can also contribute to the rise of extreme or unusual weather events. Tall structures can alter the way that wind moves throughout an urban area, pushing warmer air upwards and inducing convection, creating thunderstorms.[38] With these thunderstorms comes increased precipitation, which, because of the large amounts of impervious surfaces in cities, can have devastating impacts.[38] Impervious surfaces also absorb energy from the sun and warm the atmosphere, causing drastic increases in temperatures in urban areas. This, along with pollution and heat released from cars and other anthropogenic sources, contributes to urban heat islands.[41]

Attribution research edit

Early research in extreme weather focused on statements about predicting certain events. Contemporary research focuses more on the attribution of causes to trends in events.[5] In particular the field is focusing on climate change alongside other causal factors for these events.[5]

A 2016 report from the National Academies of Sciences, Engineering, and Medicine, recommended investing in improved shared practices across the field working on attribution research, improving the connection between research outcomes and weather forecasting.[4]

As more research is done in this area, scientists have begun to investigate the connection between climate change and extreme weather events and what future impacts may arise. Much of this work is done through climate modeling. Climate models provide important predictions about the future characteristics of the atmosphere, oceans, and Earth using data collected in the modern day.[30] However, while climate models are vital for studying more complex processes such as climate change or ocean acidification, they are still only approximations.[30] Moreover, weather events are complex and cannot be tied to a singular cause—there are often many atmospheric variables such as temperature, pressure, or moisture to note on top of any influences from climate change or natural variability.[30]

An important record of extreme weather events is gathered statistics from around the world, which can help scientists and policymakers to have a better understanding of any changes in weather and climate conditions. These statistics can influence climate modeling as well. Statistics have shown an increase in extreme weather events throughout the 1900s and into the 2000s.[citation needed]

Effects edit

 
In recent decades, new high temperature records have substantially outpaced new low temperature records on a growing portion of Earth's surface.[42]
 
The IPCC Sixth Assessment Report (2021) projects progressively large increases in both the frequency and intensity of extreme weather events, for increasing degrees of global warming.[43]

The effects of extreme weather includes, but are not limited to:[44][45]

  • Too much rain (heavy downpours), causing floods and landslides
  • Too much heat and no rain (heatwave) causing droughts and wildfires
  • Strong winds, such as hurricanes and tornadoes, causing damage to man made structures and animal habitats
  • Large snowfalls, causing avalanches and blizzards

Economic cost edit

According to IPCC (2011) estimates of annual losses have ranged since 1980 from a few billion to above US$200 billion (in 2010 dollars), with the highest value for 2005 (the year of Hurricane Katrina).[46] The global weather-related disaster losses, such as loss of human lives, cultural heritage, and ecosystem services, are difficult to value and monetize, and thus they are poorly reflected in estimates of losses.[47][48] Yet, recent abnormally intense storms, hurricanes, floods, heatwaves, droughts and associated large-scale wildfires have led to unprecedented negative ecological consequences for tropical forests and coral reefs around the world.[49]

Loss of human lives edit

The death toll from natural disasters has declined over 90 percent since the 1920s, according to the International Disaster Database, even as the total human population on Earth quadrupled, and temperatures rose 1.3 °C. In the 1920s, 5.4 million people died from natural disasters while in the 2010s, just 400,000 did.[50]

The most dramatic and rapid declines in deaths from extreme weather events have taken place in south Asia. Where a tropical cyclone in 1991 in Bangladesh killed 135,000 people, and a 1970 cyclone killed 300,000, the similarly-sized Cyclone Ampham, which struck India and Bangladesh in 2020, killed just 120 people in total.[51][52][53]

On July 23, 2020, Munich Re announced that the 2,900 total global deaths from natural disasters for the first half of 2020 were a record-low, and "much lower than the average figures for both the last 30 years and the last 10 years."[54]

A 2021 study found that 9.4% of global deaths between 2000 and 2019 – ~5 million annually – can be attributed to extreme temperature with cold-related ones making up the larger share and decreasing and heat-related ones making up ~0.91 % and increasing.[55][56]

Droughts and floods edit

 
A dry lakebed in California, which is in 2022 experiencing its most serious drought in 1,200 years, worsened by climate change.[57]

Climate change has led to an increase in the frequency and/or intensity of certain types of extreme weather.[58] Storms such as hurricanes or tropical cyclones may experience greater rainfall, causing major flooding events or landslides by saturating soil. This is because warmer air is able to 'hold' more moisture due to the water molecules having increased kinetic energy, and precipitation occurs at a greater rate because more molecules have the critical speed needed to fall as rain drops.[59] A shift in rainfall patterns can lead to greater amounts of precipitation in one area while another experiences much hotter, drier conditions, which can lead to drought.[60] This is because an increase in temperatures also lead to an increase in evaporation at the surface of the earth, so more precipitation does not necessarily mean universally wetter conditions or a worldwide increase in drinking water.[59]

See also edit

References edit

  1. ^ . Intergovernmental Panel on Climate Change. Archived from the original on 2005-11-01. Retrieved 13 April 2007.
  2. ^ a b c d IPCC, 2022: Annex II: Glossary [Möller, V., R. van Diemen, J.B.R. Matthews, C. Méndez, S. Semenov, J.S. Fuglestvedt, A. Reisinger (eds.)]. In: Climate Change 2022: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [H.-O. Pörtner, D.C. Roberts, M. Tignor, E.S. Poloczanska, K. Mintenbeck, A. Alegría, M. Craig, S. Langsdorf, S. Löschke, V. Möller, A. Okem, B. Rama (eds.)]. Cambridge University Press, Cambridge, UK and New York, NY, US, pp. 2897–2930, doi:10.1017/9781009325844.029.
  3. ^ Seneviratne, Sonia I.; Zhang, Xuebin; Adnan, M.; Badi, W.; et al. (2021). "Chapter 11: Weather and climate extreme events in a changing climate" (PDF). Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate. Cambridge University Press. p. 1517.
  4. ^ a b Attribution of Extreme Weather Events in the Context of Climate Change (Report). Washington, DC: The National Academies Press. 2016. pp. 127–136. doi:10.17226/21852. ISBN 978-0-309-38094-2. from the original on 2022-02-15. Retrieved 2020-02-22.
  5. ^ a b c d e Attribution of Extreme Weather Events in the Context of Climate Change (Report). Washington, DC: The National Academies Press. 2016. pp. 21–24. doi:10.17226/21852. ISBN 978-0-309-38094-2.
  6. ^ a b c d Mogil, H Michael (2007). Extreme Weather. New York: Black Dog & Leventhal Publishers. pp. 210–211. ISBN 978-1-57912-743-5.
  7. ^ NOAA NWS. . Archived from the original on 2014-07-05. Retrieved 2014-06-16.
  8. ^ Casey Thornbrugh; Asher Ghertner; Shannon McNeeley; Olga Wilhelmi; Robert Harriss (2007). . National Center for Atmospheric Research. Archived from the original on 2018-08-01. Retrieved 2009-08-18.
  9. ^ "It's not just the heat – it's the ozone: Study highlights hidden dangers". University of York. 2013. from the original on 2018-07-29. Retrieved 2014-06-16.
  10. ^ Brücker, G. (2005). "Vulnerable populations: Lessons learnt from the summer 2003 heatwaves in europe". Eurosurveillance. 10 (7): 1–2. doi:10.2807/esm.10.07.00551-en.
  11. ^ Epstein, Paul R (2005). "Climate Change and Human Health". The New England Journal of Medicine. 353 (14): 1433–1436. doi:10.1056/nejmp058079. PMC 2636266. PMID 16207843.
  12. ^ Doan, Lynn; Covarrubias, Amanda (2006-07-27). "Heat Eases, but Thousands of Southern Californians Still Lack Power". Los Angeles Times. from the original on 2023-04-16. Retrieved June 16, 2014.
  13. ^ T. R. Oke (1982). "The energetic basis of the urban heat island". Quarterly Journal of the Royal Meteorological Society. 108 (455): 1–24. Bibcode:1982QJRMS.108....1O. doi:10.1002/qj.49710845502. S2CID 120122894.
  14. ^ Glossary of Meteorology (2009). . American Meteorological Society. Archived from the original on 2011-05-14. Retrieved 2009-08-18.
  15. ^ "Climate change: Arctic warming linked to colder winters". BBC News. 2 September 2021. from the original on 20 October 2021. Retrieved 20 October 2021.
  16. ^ Cohen, Judah; Agel, Laurie; Barlow, Mathew; Garfinkel, Chaim I.; White, Ian (3 September 2021). "Linking Arctic variability and change with extreme winter weather in the United States". Science. 373 (6559): 1116–1121. Bibcode:2021Sci...373.1116C. doi:10.1126/science.abi9167. PMID 34516838. S2CID 237402139.
  17. ^ Irfan, Umair (18 February 2021). "Scientists are divided over whether climate change is fueling extreme cold events". Vox. from the original on 23 October 2021. Retrieved 24 October 2021.
  18. ^ "Climate change impacts of heat and cold extremes on humans" (PDF). (PDF) from the original on 21 August 2021. Retrieved 25 October 2021.
  19. ^ He, Yongli; Wang, Xiaoxia; Zhang, Boyuan; Wang, Zhanbo; Wang, Shanshan (2023-05-13). "Contrast responses of strong and weak winter extreme cold events in the Northern Hemisphere to global warming". Climate Dynamics. 61 (9–10): 4533–4550. Bibcode:2023ClDy...61.4533H. doi:10.1007/s00382-023-06822-7. ISSN 1432-0894. S2CID 258681375.
  20. ^ Global Guide to Tropical Cyclone Forecasting: 2017 (PDF) (Report). World Meteorological Organization. April 17, 2018. (PDF) from the original on July 14, 2019. Retrieved September 6, 2020.
  21. ^ a b Trenberth, Kevin E. (November 2011). "Attribution of climate variations and trends to human influences and natural variability: Attribution of the human influence". Wiley Interdisciplinary Reviews: Climate Change. 2 (6): 925–930. doi:10.1002/wcc.142. S2CID 140147654.
  22. ^ "Climate Change 2021 / The Physical Science Basis / Working Group I contribution to the WGI Sixth Assessment Report of the Intergovernmental Panel on Climate Change / Summary for Policymakers" (PDF). Intergovernmental Panel on Climate Change. 9 August 2021. Fig. SPM.6 (p. 18), 23. (PDF) from the original on 4 November 2021.
  23. ^ Francis, Jennifer A.; Vavrus, Stephen J. (2012). "Evidence linking Arctic amplification to extreme weather in mid-latitudes". Geophysical Research Letters. 39 (6): L06801. Bibcode:2012GeoRL..39.6801F. doi:10.1029/2012GL051000.
  24. ^ Vladimir Petoukhov; Vladimir A. Semenov (November 2010). "A link between reduced Barents-Kara sea ice and cold winter extremes over northern continents" (PDF). Journal of Geophysical Research: Atmospheres. 115 (21): D21111. Bibcode:2010JGRD..11521111P. doi:10.1029/2009JD013568. (PDF) from the original on 2017-08-09. Retrieved 2019-09-24.
  25. ^ J A Screen (November 2013). "Influence of Arctic sea ice on European summer precipitation". Environmental Research Letters. 8 (4): 044015. Bibcode:2013ERL.....8d4015S. doi:10.1088/1748-9326/8/4/044015. hdl:10871/14835.
  26. ^ Qiuhong Tang; Xuejun Zhang; Jennifer A. Francis (December 2013). "Extreme summer weather in northern mid-latitudes linked to a vanishing cryosphere". Nature Climate Change. 4 (1): 45–50. Bibcode:2014NatCC...4...45T. doi:10.1038/nclimate2065.
  27. ^ Golledge, Nicholas R.; Keller, Elizabeth D.; Gomez, Natalya; Naughten, Kaitlin A.; Bernales, Jorge; Trusel, Luke D.; Edwards, Tamsin L. (February 2019). "Global environmental consequences of twenty-first-century ice-sheet melt". Nature. 566 (7742): 65–72. Bibcode:2019Natur.566...65G. doi:10.1038/s41586-019-0889-9. ISSN 0028-0836. PMID 30728520. S2CID 59606358. from the original on 2021-06-19. Retrieved 2021-05-05.
  28. ^ a b c Caesar, L.; McCarthy, G. D.; Thornalley, D. J. R.; Cahill, N.; Rahmstorf, S. (March 2021). "Current Atlantic Meridional Overturning Circulation weakest in last millennium". Nature Geoscience. 14 (3): 118–120. Bibcode:2021NatGe..14..118C. doi:10.1038/s41561-021-00699-z. ISSN 1752-0894. S2CID 232052381. from the original on 2021-06-17. Retrieved 2021-05-05.
  29. ^ a b c d Human Cost of Disasters. United Nations. 2020. doi:10.18356/79b92774-en. ISBN 978-92-1-005447-8. S2CID 243258946.
  30. ^ a b c d Oreskes, Naomi (2018-02-19), "Why Believe a Computer? Models, Measures, and Meaning in the Natural World", The Earth Around Us, Routledge, pp. 70–82, doi:10.4324/9780429496653-8, ISBN 978-0-429-49665-3
  31. ^ "Extreme heat waves in a warming world don't just break records – they shatter them". PBS NewsHour. 28 July 2021. from the original on 12 August 2021. Retrieved 13 August 2021.
  32. ^ Fischer, E. M.; Sippel, S.; Knutti, R. (August 2021). "Increasing probability of record-shattering climate extremes". Nature Climate Change. 11 (8): 689–695. Bibcode:2021NatCC..11..689F. doi:10.1038/s41558-021-01092-9. ISSN 1758-6798. S2CID 236438374.
  33. ^ Knutson, Tom. "Global Warming and Hurricanes". www.gfdl.noaa.gov. from the original on 2020-04-16. Retrieved 2020-08-29.
  34. ^ a b Knutson, Thomas; Camargo, Suzana J.; Chan, Johnny C. L.; Emanuel, Kerry; Ho, Chang-Hoi; Kossin, James; Mohapatra, Mrutyunjay; Satoh, Masaki; Sugi, Masato; Walsh, Kevin; Wu, Liguang (August 6, 2019). "Tropical Cyclones and Climate Change Assessment: Part II. Projected Response to Anthropogenic Warming". Bulletin of the American Meteorological Society. 101 (3): BAMS–D–18–0194.1. Bibcode:2020BAMS..101E.303K. doi:10.1175/BAMS-D-18-0194.1.
  35. ^ "Major tropical cyclones have become '15% more likely' over past 40 years". Carbon Brief. May 18, 2020. from the original on August 8, 2020. Retrieved August 31, 2020.
  36. ^ Kossin, James P.; Knapp, Kenneth R.; Olander, Timothy L.; Velden, Christopher S. (May 18, 2020). "Global increase in major tropical cyclone exceedance probability over the past four decades". Proceedings of the National Academy of Sciences. 117 (22): 11975–11980. Bibcode:2020PNAS..11711975K. doi:10.1073/pnas.1920849117. PMC 7275711. PMID 32424081.
  37. ^ Collins, M.; Sutherland, M.; Bouwer, L.; Cheong, S.-M.; et al. (2019). "Chapter 6: Extremes, Abrupt Changes and Managing Risks" (PDF). IPCC Special Report on the Ocean and Cryosphere in a Changing Climate. p. 602. (PDF) from the original on December 20, 2019. Retrieved October 6, 2020.
  38. ^ a b c Douglas, Ian; Goode, David; Houck, Michael C.; Maddox, David, eds. (2010). The Routledge Handbook of Urban Ecology. doi:10.4324/9780203839263. hdl:11603/25230. ISBN 978-1-136-88341-5.
  39. ^ Rome, Adam (2001). The Bulldozer in the Countryside. Cambridge University Press. doi:10.1017/cbo9780511816703. ISBN 978-0-521-80490-5.
  40. ^ . Louisiana Resiliency Assistance Program. Archived from the original on 2021-05-07. Retrieved 2021-05-05.
  41. ^ Kleerekoper, Laura; van Esch, Marjolein; Salcedo, Tadeo Baldiri (July 2012). "How to make a city climate-proof, addressing the urban heat island effect". Resources, Conservation and Recycling. 64: 30–38. doi:10.1016/j.resconrec.2011.06.004. from the original on 2022-01-20. Retrieved 2021-05-05.
  42. ^ "Mean Monthly Temperature Records Across the Globe / Timeseries of Global Land and Ocean Areas at Record Levels for July from 1951-2023". NCEI.NOAA.gov. National Centers for Environmental Information (NCEI) of the National Oceanic and Atmospheric Administration (NOAA). August 2023. from the original on 14 August 2023. (change "202307" in URL to see years other than 2023, and months other than 07=July)
  43. ^ "Climate Change 2021: The Physical Science Basis: Summary for Policymakers" (PDF). Intergovernmental Panel on Climate Change. 9 August 2021. p. SPM-23. (PDF) from the original on 4 November 2021.
  44. ^ "Fun Facts for Kids on Animals, Earth, History and more!". DK Find Out!. from the original on 2021-07-22. Retrieved 2020-05-26.
  45. ^ "Extreme Weather and Climate Change". Center for Climate and Energy Solutions. 2019-08-14. from the original on 2021-06-16. Retrieved 2020-05-26.
  46. ^ "Billion-Dollar Weather and Climate Disasters: Summary Stats". National Centers for Environmental Information (NCEI). from the original on 2018-07-13. Retrieved 2015-03-23.
  47. ^ Smith A.B.; R. Katz (2013). (PDF). Natural Hazards. 67 (2): 387–410. Bibcode:2013NatHa..67..387S. doi:10.1007/s11069-013-0566-5. S2CID 30742858. Archived from the original (PDF) on 2016-03-04. Retrieved 2015-03-23.
  48. ^ (PDF). Archived from the original on November 24, 2011.
  49. ^ França, Filipe (2020). "Climatic and local stressor interactions threaten tropical forests and coral reefs". Philosophical Transactions of the Royal Society B. 375 (1794). doi:10.1098/rstb.2019.0116. PMC 7017775. PMID 31983328.
  50. ^ "The international disasters database". EM-DAT. from the original on 2021-06-18. Retrieved 2020-08-29.
  51. ^ "Bangladesh cyclone of 1991". History.com. 29 April 2019. from the original on 2021-05-07. Retrieved 2020-08-29.
  52. ^ "The Deadliest Tropical Cyclone on Record Killed 300,000 People". The Weather Channel. from the original on 2021-06-24. Retrieved 2020-08-29.
  53. ^ "Amphan's Toll: More Than 100 Killed, billions in Damage, Hundreds of Thousands Homeless". www.wunderground.com. from the original on 2020-10-14. Retrieved 2020-08-29.
  54. ^ "Very high losses from thunderstorms – The natural disaster figures for the first half of 2020". www.munichre.com. from the original on 2021-06-24. Retrieved 2020-08-29.
  55. ^ "Extreme temperatures kill 5 million people a year with heat-related deaths rising, study finds". The Guardian. 7 July 2021. from the original on 14 August 2021. Retrieved 14 August 2021.
  56. ^ Zhao, Qi; et al. (1 July 2021). "Global, regional, and national burden of mortality associated with non-optimal ambient temperatures from 2000 to 2019: a three-stage modelling study". The Lancet Planetary Health. 5 (7): e415–e425. doi:10.1016/S2542-5196(21)00081-4. hdl:2158/1285803. ISSN 2542-5196. PMID 34245712. S2CID 235791583.
  57. ^ Irina Ivanova (June 2, 2022). "California is rationing water amid its worst drought in 1,200 years". CBS News. from the original on January 13, 2023. Retrieved June 2, 2022.
  58. ^ Seneviratne, Sonia I.; Zhang, Xuebin; Adnan, M.; Badi, W.; et al. (2021). "Chapter 11: Weather and climate extreme events in a changing climate" (PDF). IPCC AR6 WG1 2021. p. 1517. (PDF) from the original on 2022-05-29. Retrieved 2022-05-13. in IPCC (2021). Masson-Delmotte, V.; Zhai, P.; Pirani, A.; Connors, S. L.; et al. (eds.). Climate Change 2021: The Physical Science Basis (PDF). Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press (In Press). (PDF) from the original on 2021-08-13. Retrieved 2022-05-13.
  59. ^ a b US EPA, OAR (2016-06-27). "Climate Change Indicators: U.S. and Global Precipitation". US EPA. from the original on 2021-06-16. Retrieved 2021-05-05.
  60. ^ US EPA, OAR (2016-06-27). "Climate Change Indicators: Drought". US EPA. from the original on 2021-06-16. Retrieved 2021-05-05.

External links edit

extreme, weather, includes, unexpected, unusual, severe, unseasonal, weather, weather, extremes, historical, distribution, range, that, been, seen, past, extreme, events, based, location, recorded, weather, history, they, defined, lying, most, unusual, percent. Extreme weather includes unexpected unusual severe or unseasonal weather weather at the extremes of the historical distribution the range that has been seen in the past 1 2 Extreme events are based on a location s recorded weather history They are defined as lying in the most unusual ten percent 10th or 90th percentile of a probability density function 2 The main types of extreme weather include heat waves cold waves and heavy precipitation or storm events such as tropical cyclones The effects of extreme weather events are economic costs loss of human lives droughts floods landslides Severe weather is a particular type of extreme weather which poses risks to life and property A tornado is an example for an extreme weather event This tornado struck Anadarko Oklahoma during a tornado outbreak in 1999 Climate change is increasing the periodicity and intensity of some extreme weather events 3 Confidence in the attribution of extreme weather and other events to anthropogenic climate change is highest in changes in frequency or magnitude of extreme heat and cold events with some confidence in increases in heavy precipitation and increases in the intensity of droughts 4 Current evidence and climate models show that an increasing global temperature will intensify extreme weather events around the globe thereby amplifying human loss damages and economic costs and ecosystem destruction Extreme weather has significant impacts on human society as well as natural ecosystems For example a global insurer Munich Re estimates that natural disasters cause more than 90 in billion global direct losses in 2015 5 Some human activities can exacerbate the effects for example poor urban planning wetland destruction and building homes along floodplains Contents 1 Definition 2 Types 2 1 Heat waves 2 2 Cold waves 2 3 Heavy rain and storms 2 3 1 Tropical cyclones 3 Causes and attribution 3 1 Natural variability 3 2 Climate change 3 2 1 Tropical cyclones and climate change 3 3 Human activities that exacerbate the effects 3 4 Attribution research 4 Effects 4 1 Economic cost 4 2 Loss of human lives 4 3 Droughts and floods 5 See also 6 References 7 External linksDefinition editExtreme weather describes unusual weather events that are at the extremes of the historical distribution for a given area 2 2908 The IPCC Sixth Assessment Report defines an extreme weather event as follows An event that is rare at a particular place and time of year Definitions of rare vary but an extreme weather event would normally be as rare as or rarer than the 10th or 90th percentile of a probability density function estimated from observations 2 2908 In comparison the term severe weather is any aspect of the weather that poses risks to life property or requires the intervention of authorities citation needed Severe weather is thus a particular type of extreme weather Types editDefinitions of extreme weather vary in different parts of the community changing the outcomes of research from those fields 5 Heat waves edit nbsp 2003 European heat waveMain article Heat wave Further information Effects of climate change Heat waves and temperature extremes Further information List of heat waves Heat waves are periods of abnormally high temperatures and heat index Definitions of a heatwave vary because of the variation of temperatures in different geographic locations 6 Excessive heat is often accompanied by high levels of humidity but can also be catastrophically dry 7 Because heat waves are not visible as other forms of severe weather like hurricanes tornadoes and thunderstorms they are one of the less known forms of extreme weather 8 Severely hot weather can damage populations and crops due to potential dehydration or hyperthermia heat cramps heat expansion and heat stroke Dried soils are more susceptible to erosion decreasing lands available for agriculture Outbreaks of wildfires can increase in frequency as dry vegetation has an increased likelihood of igniting The evaporation of bodies of water can be devastating to marine populations decreasing the size of the habitats available as well as the amount of nutrition present within the waters Livestock and other animal populations may decline as well During excessive heat plants shut their leaf pores stomata a protective mechanism to conserve water but also curtails plants absorption capabilities This leaves more pollution and ozone in the air which leads to higher mortality in the population It has been estimated that extra pollution during the hot summer of 2006 in the UK cost 460 lives 9 The European heat waves from summer 2003 are estimated to have caused 30 000 excess deaths due to heat stress and air pollution 10 Over 200 U S cities have registered new record high temperatures 11 The worst heat wave in the US occurred in 1936 and killed more than 5000 people directly The worst heat wave in Australia occurred in 1938 39 and killed 438 The second worst was in 1896 Power outages can also occur within areas experiencing heat waves due to the increased demand for electricity i e air conditioning use 12 The urban heat island effect can increase temperatures particularly overnight 13 Cold waves edit nbsp Cold wave in continental North America from Dec 3 10 2013 Red color means above mean temperature blue represents below normal temperature Main article Cold wave A cold wave is a weather phenomenon that is distinguished by a cooling of the air Specifically as used by the U S National Weather Service a cold wave is a rapid fall in temperature within a 24 hour period requiring substantially increased protection for agriculture industry commerce and social activities The precise criterion for a cold wave is determined by the rate at which the temperature falls and the minimum to which it falls This minimum temperature is dependent on the geographical region and time of year 14 Cold waves generally are capable of occurring at any geological location and are formed by large cool air masses that accumulate over certain regions caused by movements of air streams 6 A cold wave can cause death and injury to livestock and wildlife Exposure to cold mandates greater caloric intake for all animals including humans and if a cold wave is accompanied by heavy and persistent snow grazing animals may be unable to reach necessary food and water and die of hypothermia or starvation Cold waves often necessitate the purchase of fodder for livestock at a considerable cost to farmers 6 Human populations can be inflicted with frostbite when exposed for extended periods of time to cold and may result in the loss of limbs or damage to internal organs Extreme winter cold often causes poorly insulated water pipes to freeze Even some poorly protected indoor plumbing may rupture as frozen water expands within them causing property damage Fires paradoxically become more hazardous during extreme cold Water mains may break and water supplies may become unreliable making firefighting more difficult 6 Cold waves that bring unexpected freezes and frosts during the growing season in mid latitude zones can kill plants during the early and most vulnerable stages of growth This results in crop failure as plants are killed before they can be harvested economically Such cold waves have caused famines Cold waves can also cause soil particles to harden and freeze making it harder for plants and vegetation to grow within these areas One extreme was the so called Year Without a Summer of 1816 one of several years during the 1810s in which numerous crops failed during freakish summer cold snaps after volcanic eruptions reduced incoming sunlight In some cases more frequent extremely cold winter weather i e across parts of Asia and North America including the February 2021 North American cold wave can be a result of climate change such as due to changes in the Arctic 15 16 However conclusions that link climate change to cold waves are considered to still be controversial 17 unreliable source additional citation s needed The JRC PESETA IV project concluded in 2020 that overall climate change will result in a decline in the intensity and frequency of extreme cold spells with milder winters reducing fatalities from extreme cold 18 additional citation s needed even if individual cold extreme weather may sometimes be caused by changes due to climate change and possibly even become more frequent in some regions According to a 2023 study weak extreme cold events ECEs significantly decrease in frequency projection area and total area over the north hemisphere with global warming However the frequency projection area and total area of strong ECEs show no significant trend whereas they are increasing in Siberia and Canada 19 Heavy rain and storms edit See also Effects of climate change on the water cycle Tropical cyclones edit Main article Tropical cyclones source source source source track NASA film In Katrina s Wake covering the impacts from Hurricane Katrina This section is an excerpt from Tropical cyclone edit A tropical cyclone is a rapidly rotating storm system characterized by a low pressure center a closed low level atmospheric circulation strong winds and a spiral arrangement of thunderstorms that produce heavy rain and squalls Depending on its location and strength a tropical cyclone is referred to by different names including hurricane ˈ h ʌr ɪ k en k eɪ n typhoon t aɪ ˈ f uː n tropical storm cyclonic storm tropical depression or simply cyclone A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean and a typhoon occurs in the northwestern Pacific Ocean In the Indian Ocean and South Pacific comparable storms are referred to as tropical cyclones In modern times on average around 80 to 90 named tropical cyclones form each year around the world over half of which develop hurricane force winds of 65 kn 120 km h 75 mph or more 20 Tropical cyclones carry heat and energy away from the tropics and transport it towards temperate latitudes which plays an important role in regulating global climate Tropical cyclones typically form over large bodies of relatively warm water They derive their energy through the evaporation of water from the ocean surface which ultimately condenses into clouds and rain when moist air rises and cools to saturation This energy source differs from that of mid latitude cyclonic storms such as nor easters and European windstorms which are powered primarily by horizontal temperature contrasts Tropical cyclones are typically between 100 and 2 000 km 62 and 1 243 mi in diameter Causes and attribution editFurther information Extreme event attributionGenerally speaking one event in extreme weather cannot be attributed to any one cause however certain system wide changes to global weather systems can lead to increased frequency or intensity of extreme weather events 5 Natural variability edit Aspects of our climate system have a certain level of natural variability and extreme weather events can occur for several reasons beyond human impact including changes in pressure or the movement of air Areas along the coast or located in tropical regions are more likely to experience storms with heavy precipitation than temperate regions although such events can occur Not every unusual weather event can be blamed on climate change The atmosphere is a complex and dynamic system influenced by several factors such as the natural tilt and orbit of the Earth the absorption or reflection of solar radiation the movement of air masses and the hydrologic cycle Due to this weather patterns can experience some variation and so extreme weather can be attributed at least in part to the natural variability that exists on Earth Climatic variations such as the El Nino Southern Oscillation or the North Atlantic Oscillation impact weather patterns in specific regions of the world influencing temperature and precipitation 21 The record breaking extreme weather events that have been catalogued throughout the past two hundred years most likely arise when climate patterns like ENSO or NAO work in the same direction as human induced warming 21 Climate change edit See also Effects of climate change Weather nbsp The IPCC Sixth Assessment Report 2021 projects progressively large increases in both the frequency horizontal bars and intensity vertical bars of extreme weather events for increasing degrees of global warming including more than a 5 C increase in extreme heat events for a 4 C global average temperature increase 22 Some studies assert a connection between rapidly warming arctic temperatures and thus a vanishing cryosphere to extreme weather in mid latitudes 23 24 25 26 In a study published in Nature in 2019 scientists used several simulations to determine that the melting of ice sheets in Greenland and Antarctica could affect overall sea level and sea temperature 27 Other models have shown that modern temperature rise and the subsequent addition of meltwater to the ocean could lead to a disruption of the thermohaline circulation which is responsible for the movement of seawater and distribution of heat around the globe 28 A collapse of this circulation in the northern hemisphere could lead to an increase in extreme temperatures in Europe as well as more frequent storms by throwing off natural climate variability and conditions 28 Thus as increasing temperatures cause glaciers to melt mid latitudes could experience shifts in weather patterns or temperatures 28 There were around 6 681 climate related events reported during 2000 2019 compared to 3 656 climate related events reported during 1980 1999 29 In this report a climate related event refers to floods storms droughts landslides extreme temperatures like heat waves or freezes and wildfires it excludes geophysical events such as volcanic eruptions earthquakes or mass movements 29 While there is evidence that a changing global climate such as an increase in temperature has impacted the frequency of extreme weather events the most significant effects are likely to arise in the future This is where climate models are useful for they can provide simulations of how the atmosphere may behave over time and what steps need to be taken in the present day to mitigate any negative changes 30 The increasing probability of record week long heat extremes occurrence depends on warming rate rather than global warming level 31 32 Some researchers attribute increases in extreme weather occurrences to more reliable reporting systems 29 A difference in what qualifies as extreme weather in varying climate systems could also be argued Over or under reporting of casualties or losses can lead to inaccuracy in the impact of extreme weather However the UN reports show that although some countries have experienced greater effects there have been increases in extreme weather events on all continents 29 Current evidence and climate models show that an increasing global temperature will intensify extreme weather events around the globe thereby amplifying human loss damages and economic costs and ecosystem destruction citation needed Tropical cyclones and climate change edit In 2020 the National Oceanic and Atmospheric Administration NOAA of the U S government predicted that over the 21st Century the frequency of tropical storms and Atlantic hurricanes would decline by 25 percent while their maximum intensity would rise by 5 percent 33 This section is an excerpt from Tropical cyclones and climate change edit nbsp North Atlantic tropical cyclone activity according to the Power Dissipation Index 1949 2015 Sea surface temperature has been plotted alongside the PDI to show how they compare The lines have been smoothed using a five year weighted average plotted at the middle year Climate change can affect tropical cyclones in a variety of ways an intensification of rainfall and wind speed a decrease in overall frequency an increase in the frequency of very intense storms and a poleward extension of where the cyclones reach maximum intensity are among the possible consequences of human induced climate change 34 Tropical cyclones use warm moist air as their source of energy or fuel As climate change is warming ocean temperatures there is potentially more of this fuel available 35 Between 1979 and 2017 there was a global increase in the proportion of tropical cyclones of Category 3 and higher on the Saffir Simpson scale The trend was most clear in the North Atlantic and in the Southern Indian Ocean In the North Pacific tropical cyclones have been moving poleward into colder waters and there was no increase in intensity over this period 36 With 2 C 3 6 F warming a greater percentage 13 of tropical cyclones are expected to reach Category 4 and 5 strength 34 A 2019 study indicates that climate change has been driving the observed trend of rapid intensification of tropical cyclones in the Atlantic basin Rapidly intensifying cyclones are hard to forecast and therefore pose additional risk to coastal communities 37 Human activities that exacerbate the effects edit There are plenty of anthropogenic activities that can exacerbate the effects of extreme weather events Urban planning often amplifies urban flooding impacts especially in areas that are at increased risk of storms due to their location and climate variability First increasing the amount of impervious surfaces such as sidewalks roads and roofs means that less of the water from incoming storms is absorbed by the land 38 The destruction of wetlands which act as a natural reservoir by absorbing water can intensify the impact of floods and extreme precipitation 39 This can happen both inland and at the coast However wetland destruction along the coast can mean decreasing an area s natural cushion thus allowing storm surges and flood waters to reach farther inland during hurricanes or cyclones 40 Building homes below sea level or along a floodplain puts residents at increased risk of destruction or injury in an extreme precipitation event More urban areas can also contribute to the rise of extreme or unusual weather events Tall structures can alter the way that wind moves throughout an urban area pushing warmer air upwards and inducing convection creating thunderstorms 38 With these thunderstorms comes increased precipitation which because of the large amounts of impervious surfaces in cities can have devastating impacts 38 Impervious surfaces also absorb energy from the sun and warm the atmosphere causing drastic increases in temperatures in urban areas This along with pollution and heat released from cars and other anthropogenic sources contributes to urban heat islands 41 Attribution research edit Early research in extreme weather focused on statements about predicting certain events Contemporary research focuses more on the attribution of causes to trends in events 5 In particular the field is focusing on climate change alongside other causal factors for these events 5 A 2016 report from the National Academies of Sciences Engineering and Medicine recommended investing in improved shared practices across the field working on attribution research improving the connection between research outcomes and weather forecasting 4 As more research is done in this area scientists have begun to investigate the connection between climate change and extreme weather events and what future impacts may arise Much of this work is done through climate modeling Climate models provide important predictions about the future characteristics of the atmosphere oceans and Earth using data collected in the modern day 30 However while climate models are vital for studying more complex processes such as climate change or ocean acidification they are still only approximations 30 Moreover weather events are complex and cannot be tied to a singular cause there are often many atmospheric variables such as temperature pressure or moisture to note on top of any influences from climate change or natural variability 30 An important record of extreme weather events is gathered statistics from around the world which can help scientists and policymakers to have a better understanding of any changes in weather and climate conditions These statistics can influence climate modeling as well Statistics have shown an increase in extreme weather events throughout the 1900s and into the 2000s citation needed Effects edit nbsp In recent decades new high temperature records have substantially outpaced new low temperature records on a growing portion of Earth s surface 42 nbsp The IPCC Sixth Assessment Report 2021 projects progressively large increases in both the frequency and intensity of extreme weather events for increasing degrees of global warming 43 The effects of extreme weather includes but are not limited to 44 45 Too much rain heavy downpours causing floods and landslides Too much heat and no rain heatwave causing droughts and wildfires Strong winds such as hurricanes and tornadoes causing damage to man made structures and animal habitats Large snowfalls causing avalanches and blizzardsEconomic cost edit See also Climate change adaptation According to IPCC 2011 estimates of annual losses have ranged since 1980 from a few billion to above US 200 billion in 2010 dollars with the highest value for 2005 the year of Hurricane Katrina 46 The global weather related disaster losses such as loss of human lives cultural heritage and ecosystem services are difficult to value and monetize and thus they are poorly reflected in estimates of losses 47 48 Yet recent abnormally intense storms hurricanes floods heatwaves droughts and associated large scale wildfires have led to unprecedented negative ecological consequences for tropical forests and coral reefs around the world 49 Loss of human lives edit The death toll from natural disasters has declined over 90 percent since the 1920s according to the International Disaster Database even as the total human population on Earth quadrupled and temperatures rose 1 3 C In the 1920s 5 4 million people died from natural disasters while in the 2010s just 400 000 did 50 The most dramatic and rapid declines in deaths from extreme weather events have taken place in south Asia Where a tropical cyclone in 1991 in Bangladesh killed 135 000 people and a 1970 cyclone killed 300 000 the similarly sized Cyclone Ampham which struck India and Bangladesh in 2020 killed just 120 people in total 51 52 53 On July 23 2020 Munich Re announced that the 2 900 total global deaths from natural disasters for the first half of 2020 were a record low and much lower than the average figures for both the last 30 years and the last 10 years 54 A 2021 study found that 9 4 of global deaths between 2000 and 2019 5 million annually can be attributed to extreme temperature with cold related ones making up the larger share and decreasing and heat related ones making up 0 91 and increasing 55 56 Droughts and floods edit See also Effects of climate change Effects on weather and Effects of climate change on the water cycle nbsp A dry lakebed in California which is in 2022 experiencing its most serious drought in 1 200 years worsened by climate change 57 Climate change has led to an increase in the frequency and or intensity of certain types of extreme weather 58 Storms such as hurricanes or tropical cyclones may experience greater rainfall causing major flooding events or landslides by saturating soil This is because warmer air is able to hold more moisture due to the water molecules having increased kinetic energy and precipitation occurs at a greater rate because more molecules have the critical speed needed to fall as rain drops 59 A shift in rainfall patterns can lead to greater amounts of precipitation in one area while another experiences much hotter drier conditions which can lead to drought 60 This is because an increase in temperatures also lead to an increase in evaporation at the surface of the earth so more precipitation does not necessarily mean universally wetter conditions or a worldwide increase in drinking water 59 See also edit nbsp Weather portalHeat burst Lists of tornadoes and tornado outbreaks List of weather records Downburst Rogue wave Severe weather List of severe weather phenomena Extreme weather events of 535 536 Year Without a SummerReferences edit Has Climate Variability or have Climate Extremes Changed Intergovernmental Panel on Climate Change Archived from the original on 2005 11 01 Retrieved 13 April 2007 a b c d IPCC 2022 Annex II Glossary Moller V R van Diemen J B R Matthews C Mendez S Semenov J S Fuglestvedt A Reisinger eds In Climate Change 2022 Impacts Adaptation and Vulnerability Contribution of Working Group II to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change H O Portner D C Roberts M Tignor E S Poloczanska K Mintenbeck A Alegria M Craig S Langsdorf S Loschke V Moller A Okem B Rama eds Cambridge University Press Cambridge UK and New York NY US pp 2897 2930 doi 10 1017 9781009325844 029 Seneviratne Sonia I Zhang Xuebin Adnan M Badi W et al 2021 Chapter 11 Weather and climate extreme events in a changing climate PDF Climate Change 2021 The Physical Science Basis Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Cambridge University Press p 1517 a b Attribution of Extreme Weather Events in the Context of Climate Change Report Washington DC The National Academies Press 2016 pp 127 136 doi 10 17226 21852 ISBN 978 0 309 38094 2 Archived from the original on 2022 02 15 Retrieved 2020 02 22 a b c d e Attribution of Extreme Weather Events in the Context of Climate Change Report Washington DC The National Academies Press 2016 pp 21 24 doi 10 17226 21852 ISBN 978 0 309 38094 2 a b c d Mogil H Michael 2007 Extreme Weather New York Black Dog amp Leventhal Publishers pp 210 211 ISBN 978 1 57912 743 5 NOAA NWS Heat A Major Killer Archived from the original on 2014 07 05 Retrieved 2014 06 16 Casey Thornbrugh Asher Ghertner Shannon McNeeley Olga Wilhelmi Robert Harriss 2007 Heat Wave Awareness Project National Center for Atmospheric Research Archived from the original on 2018 08 01 Retrieved 2009 08 18 It s not just the heat it s the ozone Study highlights hidden dangers University of York 2013 Archived from the original on 2018 07 29 Retrieved 2014 06 16 Brucker G 2005 Vulnerable populations Lessons learnt from the summer 2003 heatwaves in europe Eurosurveillance 10 7 1 2 doi 10 2807 esm 10 07 00551 en Epstein Paul R 2005 Climate Change and Human Health The New England Journal of Medicine 353 14 1433 1436 doi 10 1056 nejmp058079 PMC 2636266 PMID 16207843 Doan Lynn Covarrubias Amanda 2006 07 27 Heat Eases but Thousands of Southern Californians Still Lack Power Los Angeles Times Archived from the original on 2023 04 16 Retrieved June 16 2014 T R Oke 1982 The energetic basis of the urban heat island Quarterly Journal of the Royal Meteorological Society 108 455 1 24 Bibcode 1982QJRMS 108 1O doi 10 1002 qj 49710845502 S2CID 120122894 Glossary of Meteorology 2009 Cold Wave American Meteorological Society Archived from the original on 2011 05 14 Retrieved 2009 08 18 Climate change Arctic warming linked to colder winters BBC News 2 September 2021 Archived from the original on 20 October 2021 Retrieved 20 October 2021 Cohen Judah Agel Laurie Barlow Mathew Garfinkel Chaim I White Ian 3 September 2021 Linking Arctic variability and change with extreme winter weather in the United States Science 373 6559 1116 1121 Bibcode 2021Sci 373 1116C doi 10 1126 science abi9167 PMID 34516838 S2CID 237402139 Irfan Umair 18 February 2021 Scientists are divided over whether climate change is fueling extreme cold events Vox Archived from the original on 23 October 2021 Retrieved 24 October 2021 Climate change impacts of heat and cold extremes on humans PDF Archived PDF from the original on 21 August 2021 Retrieved 25 October 2021 He Yongli Wang Xiaoxia Zhang Boyuan Wang Zhanbo Wang Shanshan 2023 05 13 Contrast responses of strong and weak winter extreme cold events in the Northern Hemisphere to global warming Climate Dynamics 61 9 10 4533 4550 Bibcode 2023ClDy 61 4533H doi 10 1007 s00382 023 06822 7 ISSN 1432 0894 S2CID 258681375 Global Guide to Tropical Cyclone Forecasting 2017 PDF Report World Meteorological Organization April 17 2018 Archived PDF from the original on July 14 2019 Retrieved September 6 2020 a b Trenberth Kevin E November 2011 Attribution of climate variations and trends to human influences and natural variability Attribution of the human influence Wiley Interdisciplinary Reviews Climate Change 2 6 925 930 doi 10 1002 wcc 142 S2CID 140147654 Climate Change 2021 The Physical Science Basis Working Group I contribution to the WGI Sixth Assessment Report of the Intergovernmental Panel on Climate Change Summary for Policymakers PDF Intergovernmental Panel on Climate Change 9 August 2021 Fig SPM 6 p 18 23 Archived PDF from the original on 4 November 2021 Francis Jennifer A Vavrus Stephen J 2012 Evidence linking Arctic amplification to extreme weather in mid latitudes Geophysical Research Letters 39 6 L06801 Bibcode 2012GeoRL 39 6801F doi 10 1029 2012GL051000 Vladimir Petoukhov Vladimir A Semenov November 2010 A link between reduced Barents Kara sea ice and cold winter extremes over northern continents PDF Journal of Geophysical Research Atmospheres 115 21 D21111 Bibcode 2010JGRD 11521111P doi 10 1029 2009JD013568 Archived PDF from the original on 2017 08 09 Retrieved 2019 09 24 J A Screen November 2013 Influence of Arctic sea ice on European summer precipitation Environmental Research Letters 8 4 044015 Bibcode 2013ERL 8d4015S doi 10 1088 1748 9326 8 4 044015 hdl 10871 14835 Qiuhong Tang Xuejun Zhang Jennifer A Francis December 2013 Extreme summer weather in northern mid latitudes linked to a vanishing cryosphere Nature Climate Change 4 1 45 50 Bibcode 2014NatCC 4 45T doi 10 1038 nclimate2065 Golledge Nicholas R Keller Elizabeth D Gomez Natalya Naughten Kaitlin A Bernales Jorge Trusel Luke D Edwards Tamsin L February 2019 Global environmental consequences of twenty first century ice sheet melt Nature 566 7742 65 72 Bibcode 2019Natur 566 65G doi 10 1038 s41586 019 0889 9 ISSN 0028 0836 PMID 30728520 S2CID 59606358 Archived from the original on 2021 06 19 Retrieved 2021 05 05 a b c Caesar L McCarthy G D Thornalley D J R Cahill N Rahmstorf S March 2021 Current Atlantic Meridional Overturning Circulation weakest in last millennium Nature Geoscience 14 3 118 120 Bibcode 2021NatGe 14 118C doi 10 1038 s41561 021 00699 z ISSN 1752 0894 S2CID 232052381 Archived from the original on 2021 06 17 Retrieved 2021 05 05 a b c d Human Cost of Disasters United Nations 2020 doi 10 18356 79b92774 en ISBN 978 92 1 005447 8 S2CID 243258946 a b c d Oreskes Naomi 2018 02 19 Why Believe a Computer Models Measures and Meaning in the Natural World The Earth Around Us Routledge pp 70 82 doi 10 4324 9780429496653 8 ISBN 978 0 429 49665 3 Extreme heat waves in a warming world don t just break records they shatter them PBS NewsHour 28 July 2021 Archived from the original on 12 August 2021 Retrieved 13 August 2021 Fischer E M Sippel S Knutti R August 2021 Increasing probability of record shattering climate extremes Nature Climate Change 11 8 689 695 Bibcode 2021NatCC 11 689F doi 10 1038 s41558 021 01092 9 ISSN 1758 6798 S2CID 236438374 Knutson Tom Global Warming and Hurricanes www gfdl noaa gov Archived from the original on 2020 04 16 Retrieved 2020 08 29 a b Knutson Thomas Camargo Suzana J Chan Johnny C L Emanuel Kerry Ho Chang Hoi Kossin James Mohapatra Mrutyunjay Satoh Masaki Sugi Masato Walsh Kevin Wu Liguang August 6 2019 Tropical Cyclones and Climate Change Assessment Part II Projected Response to Anthropogenic Warming Bulletin of the American Meteorological Society 101 3 BAMS D 18 0194 1 Bibcode 2020BAMS 101E 303K doi 10 1175 BAMS D 18 0194 1 Major tropical cyclones have become 15 more likely over past 40 years Carbon Brief May 18 2020 Archived from the original on August 8 2020 Retrieved August 31 2020 Kossin James P Knapp Kenneth R Olander Timothy L Velden Christopher S May 18 2020 Global increase in major tropical cyclone exceedance probability over the past four decades Proceedings of the National Academy of Sciences 117 22 11975 11980 Bibcode 2020PNAS 11711975K doi 10 1073 pnas 1920849117 PMC 7275711 PMID 32424081 Collins M Sutherland M Bouwer L Cheong S M et al 2019 Chapter 6 Extremes Abrupt Changes and Managing Risks PDF IPCC Special Report on the Ocean and Cryosphere in a Changing Climate p 602 Archived PDF from the original on December 20 2019 Retrieved October 6 2020 a b c Douglas Ian Goode David Houck Michael C Maddox David eds 2010 The Routledge Handbook of Urban Ecology doi 10 4324 9780203839263 hdl 11603 25230 ISBN 978 1 136 88341 5 Rome Adam 2001 The Bulldozer in the Countryside Cambridge University Press doi 10 1017 cbo9780511816703 ISBN 978 0 521 80490 5 Louisiana Resiliency Assistance Program Louisiana Resiliency Assistance Program Archived from the original on 2021 05 07 Retrieved 2021 05 05 Kleerekoper Laura van Esch Marjolein Salcedo Tadeo Baldiri July 2012 How to make a city climate proof addressing the urban heat island effect Resources Conservation and Recycling 64 30 38 doi 10 1016 j resconrec 2011 06 004 Archived from the original on 2022 01 20 Retrieved 2021 05 05 Mean Monthly Temperature Records Across the Globe Timeseries of Global Land and Ocean Areas at Record Levels for July from 1951 2023 NCEI NOAA gov National Centers for Environmental Information NCEI of the National Oceanic and Atmospheric Administration NOAA August 2023 Archived from the original on 14 August 2023 change 202307 in URL to see years other than 2023 and months other than 07 July Climate Change 2021 The Physical Science Basis Summary for Policymakers PDF Intergovernmental Panel on Climate Change 9 August 2021 p SPM 23 Archived PDF from the original on 4 November 2021 Fun Facts for Kids on Animals Earth History and more DK Find Out Archived from the original on 2021 07 22 Retrieved 2020 05 26 Extreme Weather and Climate Change Center for Climate and Energy Solutions 2019 08 14 Archived from the original on 2021 06 16 Retrieved 2020 05 26 Billion Dollar Weather and Climate Disasters Summary Stats National Centers for Environmental Information NCEI Archived from the original on 2018 07 13 Retrieved 2015 03 23 Smith A B R Katz 2013 U S Billion dollar Weather and Climate Disasters Data sources Trends Accuracy and Biases PDF Natural Hazards 67 2 387 410 Bibcode 2013NatHa 67 387S doi 10 1007 s11069 013 0566 5 S2CID 30742858 Archived from the original PDF on 2016 03 04 Retrieved 2015 03 23 IPCC Intergovernmental Panel on Climate Change PDF Archived from the original on November 24 2011 Franca Filipe 2020 Climatic and local stressor interactions threaten tropical forests and coral reefs Philosophical Transactions of the Royal Society B 375 1794 doi 10 1098 rstb 2019 0116 PMC 7017775 PMID 31983328 The international disasters database EM DAT Archived from the original on 2021 06 18 Retrieved 2020 08 29 Bangladesh cyclone of 1991 History com 29 April 2019 Archived from the original on 2021 05 07 Retrieved 2020 08 29 The Deadliest Tropical Cyclone on Record Killed 300 000 People The Weather Channel Archived from the original on 2021 06 24 Retrieved 2020 08 29 Amphan s Toll More Than 100 Killed billions in Damage Hundreds of Thousands Homeless www wunderground com Archived from the original on 2020 10 14 Retrieved 2020 08 29 Very high losses from thunderstorms The natural disaster figures for the first half of 2020 www munichre com Archived from the original on 2021 06 24 Retrieved 2020 08 29 Extreme temperatures kill 5 million people a year with heat related deaths rising study finds The Guardian 7 July 2021 Archived from the original on 14 August 2021 Retrieved 14 August 2021 Zhao Qi et al 1 July 2021 Global regional and national burden of mortality associated with non optimal ambient temperatures from 2000 to 2019 a three stage modelling study The Lancet Planetary Health 5 7 e415 e425 doi 10 1016 S2542 5196 21 00081 4 hdl 2158 1285803 ISSN 2542 5196 PMID 34245712 S2CID 235791583 Irina Ivanova June 2 2022 California is rationing water amid its worst drought in 1 200 years CBS News Archived from the original on January 13 2023 Retrieved June 2 2022 Seneviratne Sonia I Zhang Xuebin Adnan M Badi W et al 2021 Chapter 11 Weather and climate extreme events in a changing climate PDF IPCC AR6 WG1 2021 p 1517 Archived PDF from the original on 2022 05 29 Retrieved 2022 05 13 in IPCC 2021 Masson Delmotte V Zhai P Pirani A Connors S L et al eds Climate Change 2021 The Physical Science Basis PDF Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change Cambridge University Press In Press Archived PDF from the original on 2021 08 13 Retrieved 2022 05 13 a b US EPA OAR 2016 06 27 Climate Change Indicators U S and Global Precipitation US EPA Archived from the original on 2021 06 16 Retrieved 2021 05 05 US EPA OAR 2016 06 27 Climate Change Indicators Drought US EPA Archived from the original on 2021 06 16 Retrieved 2021 05 05 External links editNOAA NCDC Billion Dollar Weather and Climate Disasters Statistics of Weather and Climate Extremes Archived 2018 09 10 at the Wayback Machine The University Corporation for Atmospheric Research UCAR Research forecasts increased chances for stormy weather Archived 2020 03 16 at the Wayback Machine Purdue University study Severe world weather overview Retrieved from https en wikipedia org w index php title Extreme weather amp oldid 1197967134, wikipedia, wiki, book, books, library,

article

, read, download, free, free download, mp3, video, mp4, 3gp, jpg, jpeg, gif, png, picture, music, song, movie, book, game, games.