Extreme surface and near-bottom currents in the northwest Atlantic
This study presents a methodology for estimating extreme current speeds fromnumerical model results using extremal analysis techniques. This method is used to estimate theextreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with50-year return periods from 17 years of m...
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ftunivtasecite:oai:ecite.utas.edu.au:82914 2023-05-15T17:45:28+02:00 Extreme surface and near-bottom currents in the northwest Atlantic Oliver, ECJ Sheng, J Thompson, KR Urrego Blanco, JR 2012 https://doi.org/10.1007/s11069-012-0303-5 http://ecite.utas.edu.au/82914 en eng Springer http://dx.doi.org/10.1007/s11069-012-0303-5 Oliver, ECJ and Sheng, J and Thompson, KR and Urrego Blanco, JR, Extreme surface and near-bottom currents in the northwest Atlantic, Natural Hazards, 64, (2) pp. 1425-1446. ISSN 0921-030X (2012) [Refereed Article] http://ecite.utas.edu.au/82914 Earth Sciences Oceanography Physical Oceanography Refereed Article PeerReviewed 2012 ftunivtasecite https://doi.org/10.1007/s11069-012-0303-5 2019-12-13T21:47:42Z This study presents a methodology for estimating extreme current speeds fromnumerical model results using extremal analysis techniques. This method is used to estimate theextreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with50-year return periods from 17 years of model output.The non-tidal currents produced by a threedimensionalocean circulation model for the 19882004 period were first used to estimate andmap the 17-year return period extreme current speeds at the surface and near the bottom. Extremalanalysis techniques (i.e., fitting the annualmaxima to the Type I probability distribution) are usedto estimate and map the 50-year extreme current speeds. Tidal currents are dominant in someparts of the northwest Atlantic, and a Monte Carlo-based methodology is developed to take intoaccount the fact that large non-tidal extrema may occur at different tidal phases. The inclusion oftidal currents in this way modifies the estimated 50-year extreme current speeds, and this isillustrated along several representative transects and depth profiles. Seasonal variations areexamined by calculating the extreme current speeds for fall-winter and springsummer. Finally,the distribution of extreme currents is interpreted taking into account (1) variability about thetime-mean current speeds, (2) wind-driven Ekman currents, and (3) flow along isobaths. Article in Journal/Newspaper Northwest Atlantic eCite UTAS (University of Tasmania) Natural Hazards 64 2 1425 1446 |
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eCite UTAS (University of Tasmania) |
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ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Physical Oceanography |
spellingShingle |
Earth Sciences Oceanography Physical Oceanography Oliver, ECJ Sheng, J Thompson, KR Urrego Blanco, JR Extreme surface and near-bottom currents in the northwest Atlantic |
topic_facet |
Earth Sciences Oceanography Physical Oceanography |
description |
This study presents a methodology for estimating extreme current speeds fromnumerical model results using extremal analysis techniques. This method is used to estimate theextreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with50-year return periods from 17 years of model output.The non-tidal currents produced by a threedimensionalocean circulation model for the 19882004 period were first used to estimate andmap the 17-year return period extreme current speeds at the surface and near the bottom. Extremalanalysis techniques (i.e., fitting the annualmaxima to the Type I probability distribution) are usedto estimate and map the 50-year extreme current speeds. Tidal currents are dominant in someparts of the northwest Atlantic, and a Monte Carlo-based methodology is developed to take intoaccount the fact that large non-tidal extrema may occur at different tidal phases. The inclusion oftidal currents in this way modifies the estimated 50-year extreme current speeds, and this isillustrated along several representative transects and depth profiles. Seasonal variations areexamined by calculating the extreme current speeds for fall-winter and springsummer. Finally,the distribution of extreme currents is interpreted taking into account (1) variability about thetime-mean current speeds, (2) wind-driven Ekman currents, and (3) flow along isobaths. |
format |
Article in Journal/Newspaper |
author |
Oliver, ECJ Sheng, J Thompson, KR Urrego Blanco, JR |
author_facet |
Oliver, ECJ Sheng, J Thompson, KR Urrego Blanco, JR |
author_sort |
Oliver, ECJ |
title |
Extreme surface and near-bottom currents in the northwest Atlantic |
title_short |
Extreme surface and near-bottom currents in the northwest Atlantic |
title_full |
Extreme surface and near-bottom currents in the northwest Atlantic |
title_fullStr |
Extreme surface and near-bottom currents in the northwest Atlantic |
title_full_unstemmed |
Extreme surface and near-bottom currents in the northwest Atlantic |
title_sort |
extreme surface and near-bottom currents in the northwest atlantic |
publisher |
Springer |
publishDate |
2012 |
url |
https://doi.org/10.1007/s11069-012-0303-5 http://ecite.utas.edu.au/82914 |
genre |
Northwest Atlantic |
genre_facet |
Northwest Atlantic |
op_relation |
http://dx.doi.org/10.1007/s11069-012-0303-5 Oliver, ECJ and Sheng, J and Thompson, KR and Urrego Blanco, JR, Extreme surface and near-bottom currents in the northwest Atlantic, Natural Hazards, 64, (2) pp. 1425-1446. ISSN 0921-030X (2012) [Refereed Article] http://ecite.utas.edu.au/82914 |
op_doi |
https://doi.org/10.1007/s11069-012-0303-5 |
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Natural Hazards |
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64 |
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1425 |
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1446 |
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1766148488218804224 |