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Perigean spring tide

A perigean spring tide is a tide that occurs three or four times per year when a perigee (the point nearest Earth reached by the Moon during its 27.3-day elliptic orbit) coincides with a spring tide (when the Sun, the Moon, and Earth are nearly aligned every two weeks).[1] This has a slight but measurable impact on the spring tide, usually adding no more than a couple of inches.[1]

Astronomical causes Edit

The Moon's orbit around Earth is elliptical, which causes the Moon to be closer to Earth and farther away at different times. The Moon and the Sun are aligned every two weeks, which results in spring tides, which are 20% higher than normal. During the period of the new moon, the Moon and Sun are on the same side of Earth, so the high tides or bulges produced independently by each reinforce each other (and has nothing to do with the spring season). Tides of maximum height and depression produced during this period are known as spring tide. Spring tides that coincide with the moon's closest approach to Earth ("perigee") have been called perigean spring tides and generally increase the normal tidal range by a couple of inches.[2]

The Ash Wednesday Storm of 1962 coincided with a perigean spring tide. It inundated the entire Atlantic coastline of the United States, from the Carolinas to Cape Cod, resulting in a loss of 40 lives and over US$500 million of property damage.[3]

See also Edit

Notes Edit

  1. ^ a b "A perigean spring tide occurs when the moon is either new or full and closest to Earth". National Ocean Service. National Oceanic and Atmospheric Administration. July 18, 2013. Retrieved February 2, 2014.
  2. ^ . National Oceanic and Atmospheric Administration. Archived from the original on 25 June 2017. Retrieved 15 August 2018.
  3. ^ "The strategic role of perigean spring tides in nautical history and North American coastal flooding, 1635-1976". Gpo.gov. Retrieved 2012-03-11.

References Edit

  • Easterbrook, D.J. (1999). Surface Process and Landforms. 2nd ed. Upper Saddle River, NJ: Prentice Hall.
  • Duxbury, A.B., Duxbury, A.C., Sverdrup, K.A. (2002). Fundamentals of Oceanography. 4th ed. New York, NY: McGraw Hill.
  • http://co-ops.nos.noaa.gov/faq2.html#15 2008-05-13 at the Wayback Machine
  • Wood, Fergus J. (2001). Tidal Dynamics Volume I: Theory and Analysis of Tidal Forces; Volume II Extreme Tidal Peaks and Coastal Flooding. 3rd ed. West Palm Beach, Fl: The Coastal Education and Research Foundation [CERF] ISBN 0-938415-10-7

External links Edit

  • Apogee & Perigee Tables

perigean, spring, tide, perigean, spring, tide, tide, that, occurs, three, four, times, year, when, perigee, point, nearest, earth, reached, moon, during, elliptic, orbit, coincides, with, spring, tide, when, moon, earth, nearly, aligned, every, weeks, this, s. A perigean spring tide is a tide that occurs three or four times per year when a perigee the point nearest Earth reached by the Moon during its 27 3 day elliptic orbit coincides with a spring tide when the Sun the Moon and Earth are nearly aligned every two weeks 1 This has a slight but measurable impact on the spring tide usually adding no more than a couple of inches 1 Contents 1 Astronomical causes 2 See also 3 Notes 4 References 5 External linksAstronomical causes EditThe Moon s orbit around Earth is elliptical which causes the Moon to be closer to Earth and farther away at different times The Moon and the Sun are aligned every two weeks which results in spring tides which are 20 higher than normal During the period of the new moon the Moon and Sun are on the same side of Earth so the high tides or bulges produced independently by each reinforce each other and has nothing to do with the spring season Tides of maximum height and depression produced during this period are known as spring tide Spring tides that coincide with the moon s closest approach to Earth perigee have been called perigean spring tides and generally increase the normal tidal range by a couple of inches 2 The Ash Wednesday Storm of 1962 coincided with a perigean spring tide It inundated the entire Atlantic coastline of the United States from the Carolinas to Cape Cod resulting in a loss of 40 lives and over US 500 million of property damage 3 See also EditKing tideNotes Edit a b A perigean spring tide occurs when the moon is either new or full and closest to Earth National Ocean Service National Oceanic and Atmospheric Administration July 18 2013 Retrieved February 2 2014 Tide Predictions amp Data Tidal Current Predictions and Data Data Access Problems FAQ Tide Predictions and Data National Oceanic and Atmospheric Administration Archived from the original on 25 June 2017 Retrieved 15 August 2018 The strategic role of perigean spring tides in nautical history and North American coastal flooding 1635 1976 Gpo gov Retrieved 2012 03 11 References EditEasterbrook D J 1999 Surface Process and Landforms 2nd ed Upper Saddle River NJ Prentice Hall Duxbury A B Duxbury A C Sverdrup K A 2002 Fundamentals of Oceanography 4th ed New York NY McGraw Hill http co ops nos noaa gov faq2 html 15 Archived 2008 05 13 at the Wayback Machine Wood Fergus J 2001 Tidal Dynamics Volume I Theory and Analysis of Tidal Forces Volume II Extreme Tidal Peaks and Coastal Flooding 3rd ed West Palm Beach Fl The Coastal Education and Research Foundation CERF ISBN 0 938415 10 7External links EditApogee amp Perigee Tables Retrieved from https en wikipedia org w index php title Perigean spring tide amp oldid 1140281397, wikipedia, wiki, book, books, library,

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