Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.

The air-sea drag coefficient controls the transfer of momentum from wind to water. In modeling storm surge, this coefficient is a crucial parameter for estimating the surge height. This study uses two strong wind events on Lake Erie to calibrate the drag coefficient using the Coupled Ocean Atmospher...

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Autor principal: Carl Drews
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Lenguaje:EN
Publicado: Public Library of Science (PLoS) 2013
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Acceso en línea:https://doaj.org/article/25ab580b31fa4b539d24839e6b2253eb
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spelling oai:doaj.org-article:25ab580b31fa4b539d24839e6b2253eb2021-11-18T08:58:57ZUsing wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.1932-620310.1371/journal.pone.0072510https://doaj.org/article/25ab580b31fa4b539d24839e6b2253eb2013-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/23977309/?tool=EBIhttps://doaj.org/toc/1932-6203The air-sea drag coefficient controls the transfer of momentum from wind to water. In modeling storm surge, this coefficient is a crucial parameter for estimating the surge height. This study uses two strong wind events on Lake Erie to calibrate the drag coefficient using the Coupled Ocean Atmosphere Wave Sediment Transport (COAWST) modeling system and the the Regional Ocean Modeling System (ROMS). Simulated waves are generated on the lake with Simulating WAves Nearshore (SWAN). Wind setdown provides the opportunity to eliminate wave setup as a contributing factor, since waves are minimal at the upwind shore. The study finds that model results significantly underestimate wind setdown and storm surge when a typical open-ocean formulation without waves is used for the drag coefficient. The contribution of waves to wind setdown and storm surge is 34.7%. Scattered lake ice also increases the effective drag coefficient by a factor of 1.1.Carl DrewsPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 8, Iss 8, p e72510 (2013)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Carl Drews
Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.
description The air-sea drag coefficient controls the transfer of momentum from wind to water. In modeling storm surge, this coefficient is a crucial parameter for estimating the surge height. This study uses two strong wind events on Lake Erie to calibrate the drag coefficient using the Coupled Ocean Atmosphere Wave Sediment Transport (COAWST) modeling system and the the Regional Ocean Modeling System (ROMS). Simulated waves are generated on the lake with Simulating WAves Nearshore (SWAN). Wind setdown provides the opportunity to eliminate wave setup as a contributing factor, since waves are minimal at the upwind shore. The study finds that model results significantly underestimate wind setdown and storm surge when a typical open-ocean formulation without waves is used for the drag coefficient. The contribution of waves to wind setdown and storm surge is 34.7%. Scattered lake ice also increases the effective drag coefficient by a factor of 1.1.
format article
author Carl Drews
author_facet Carl Drews
author_sort Carl Drews
title Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.
title_short Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.
title_full Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.
title_fullStr Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.
title_full_unstemmed Using wind setdown and storm surge on Lake Erie to calibrate the air-sea drag coefficient.
title_sort using wind setdown and storm surge on lake erie to calibrate the air-sea drag coefficient.
publisher Public Library of Science (PLoS)
publishDate 2013
url https://doaj.org/article/25ab580b31fa4b539d24839e6b2253eb
work_keys_str_mv AT carldrews usingwindsetdownandstormsurgeonlakeerietocalibratetheairseadragcoefficient
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