Extreme surface and near-bottom currents in the northwest Atlantic

This study presents a methodology for estimating extreme current speeds from numerical model results using extremal analysis techniques. This method is used to estimate the extreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with 50-year return periods from 17 years o...

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Main Authors: Eric Oliver, Jinyu Sheng, Keith Thompson, Jorge Blanco
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://hdl.handle.net/10.1007/s11069-012-0303-5
id ftrepec:oai:RePEc:spr:nathaz:v:64:y:2012:i:2:p:1425-1446
record_format openpolar
spelling ftrepec:oai:RePEc:spr:nathaz:v:64:y:2012:i:2:p:1425-1446 2023-05-15T17:45:26+02:00 Extreme surface and near-bottom currents in the northwest Atlantic Eric Oliver Jinyu Sheng Keith Thompson Jorge Blanco http://hdl.handle.net/10.1007/s11069-012-0303-5 unknown http://hdl.handle.net/10.1007/s11069-012-0303-5 article ftrepec 2020-12-04T13:32:26Z This study presents a methodology for estimating extreme current speeds from numerical model results using extremal analysis techniques. This method is used to estimate the extreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with 50-year return periods from 17 years of model output. The non-tidal currents produced by a three-dimensional ocean circulation model for the 1988–2004 period were first used to estimate and map the 17-year return period extreme current speeds at the surface and near the bottom. Extremal analysis techniques (i.e., fitting the annual maxima to the Type I probability distribution) are used to estimate and map the 50-year extreme current speeds. Tidal currents are dominant in some parts of the northwest Atlantic, and a Monte Carlo-based methodology is developed to take into account the fact that large non-tidal extrema may occur at different tidal phases. The inclusion of tidal currents in this way modifies the estimated 50-year extreme current speeds, and this is illustrated along several representative transects and depth profiles. Seasonal variations are examined by calculating the extreme current speeds for fall-winter and spring–summer. Finally, the distribution of extreme currents is interpreted taking into account (1) variability about the time-mean current speeds, (2) wind-driven Ekman currents, and (3) flow along isobaths. Copyright Springer Science+Business Media B.V. 2012 Extreme current speeds, Extremal analysis, Northwest Atlantic, Ocean circulation model, Monte Carlo methods Article in Journal/Newspaper Northwest Atlantic RePEc (Research Papers in Economics)
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description This study presents a methodology for estimating extreme current speeds from numerical model results using extremal analysis techniques. This method is used to estimate the extreme near-surface and near-bottom current speeds of the northwest Atlantic Ocean with 50-year return periods from 17 years of model output. The non-tidal currents produced by a three-dimensional ocean circulation model for the 1988–2004 period were first used to estimate and map the 17-year return period extreme current speeds at the surface and near the bottom. Extremal analysis techniques (i.e., fitting the annual maxima to the Type I probability distribution) are used to estimate and map the 50-year extreme current speeds. Tidal currents are dominant in some parts of the northwest Atlantic, and a Monte Carlo-based methodology is developed to take into account the fact that large non-tidal extrema may occur at different tidal phases. The inclusion of tidal currents in this way modifies the estimated 50-year extreme current speeds, and this is illustrated along several representative transects and depth profiles. Seasonal variations are examined by calculating the extreme current speeds for fall-winter and spring–summer. Finally, the distribution of extreme currents is interpreted taking into account (1) variability about the time-mean current speeds, (2) wind-driven Ekman currents, and (3) flow along isobaths. Copyright Springer Science+Business Media B.V. 2012 Extreme current speeds, Extremal analysis, Northwest Atlantic, Ocean circulation model, Monte Carlo methods
format Article in Journal/Newspaper
author Eric Oliver
Jinyu Sheng
Keith Thompson
Jorge Blanco
spellingShingle Eric Oliver
Jinyu Sheng
Keith Thompson
Jorge Blanco
Extreme surface and near-bottom currents in the northwest Atlantic
author_facet Eric Oliver
Jinyu Sheng
Keith Thompson
Jorge Blanco
author_sort Eric Oliver
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
url http://hdl.handle.net/10.1007/s11069-012-0303-5
genre Northwest Atlantic
genre_facet Northwest Atlantic
op_relation http://hdl.handle.net/10.1007/s11069-012-0303-5
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