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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Published in:Natural Hazards
Main Authors: Oliver, ECJ, Sheng, J, Thompson, KR, Urrego Blanco, JR
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2012
Subjects:
Online Access:https://doi.org/10.1007/s11069-012-0303-5
http://ecite.utas.edu.au/82914
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spelling 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
institution Open Polar
collection eCite UTAS (University of Tasmania)
op_collection_id 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
container_title Natural Hazards
container_volume 64
container_issue 2
container_start_page 1425
op_container_end_page 1446
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