Hurricane wake restratification rates of one-, two- and three-dimensional processes

The restratification of the cold wakes of Tropical Cyclones Fanapi, Frances, Igor and Katrina are examined based on derived scalings for processes that can restore the hurricane wake toward the precyclone conditions. The different restoration processes depend on the parameters of the wake: depth, wi...

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Main Authors: Haney, S., Bachman, S., Cooper, B., Kupper, S., McCaffrey, Katherine, Van Roekel, L., Stevenson, S., Fox-Kemper, Baylor, Ferrari, Raffaele
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Language:en_US
Published: Sears Foundation for Marine Research, Yale University 2014
Online Access:http://hdl.handle.net/1721.1/87709
https://orcid.org/0000-0002-3736-1956
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author Haney, S.
Bachman, S.
Cooper, B.
Kupper, S.
McCaffrey, Katherine
Van Roekel, L.
Stevenson, S.
Fox-Kemper, Baylor
Ferrari, Raffaele
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Haney, S.
Bachman, S.
Cooper, B.
Kupper, S.
McCaffrey, Katherine
Van Roekel, L.
Stevenson, S.
Fox-Kemper, Baylor
Ferrari, Raffaele
author_sort Haney, S.
collection MIT
description The restratification of the cold wakes of Tropical Cyclones Fanapi, Frances, Igor and Katrina are examined based on derived scalings for processes that can restore the hurricane wake toward the precyclone conditions. The different restoration processes depend on the parameters of the wake: depth, width, buoyancy anomaly and wind stress. The parameters needed are derived for each wake from satellite and climatological data. The scalings are based on model results and existing parameterizations, including air-sea heat fluxes (one-dimensional) Ekman buoyancy fluxes (two-dimensional) and mixed layer eddies (three-dimensional). The dominant surface restoration occurs by a combination of surface fluxes and Ekman buoyancy fluxes, while the submesoscale mixed layer eddy bolus fluxes are the dominant subsurface effect.
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spelling mit-1721.1/877092022-09-26T15:55:14Z Hurricane wake restratification rates of one-, two- and three-dimensional processes Haney, S. Bachman, S. Cooper, B. Kupper, S. McCaffrey, Katherine Van Roekel, L. Stevenson, S. Fox-Kemper, Baylor Ferrari, Raffaele Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Ferrari, Raffaele The restratification of the cold wakes of Tropical Cyclones Fanapi, Frances, Igor and Katrina are examined based on derived scalings for processes that can restore the hurricane wake toward the precyclone conditions. The different restoration processes depend on the parameters of the wake: depth, width, buoyancy anomaly and wind stress. The parameters needed are derived for each wake from satellite and climatological data. The scalings are based on model results and existing parameterizations, including air-sea heat fluxes (one-dimensional) Ekman buoyancy fluxes (two-dimensional) and mixed layer eddies (three-dimensional). The dominant surface restoration occurs by a combination of surface fluxes and Ekman buoyancy fluxes, while the submesoscale mixed layer eddy bolus fluxes are the dominant subsurface effect. National Science Foundation (U.S.) (NSF 0934737) National Science Foundation (U.S.) (NSF grant 0855010) United States. National Aeronautics and Space Administration (NASA NNX09AF38G) United States. National Aeronautics and Space Administration (NASA NNX09AO20H) National Science Foundation (U.S.) (NSF 0825614) Cooperative Institute for Research in Environmental Sciences (Fellowship) National Science Foundation (U.S.) (NSF REU 0913800) University of Colorado Boulder (Undergraduate Research Opportunities Program) 2014-06-09T20:13:20Z 2014-06-09T20:13:20Z 2012-11 2012-08 Article http://purl.org/eprint/type/JournalArticle 00222402 15439542 http://hdl.handle.net/1721.1/87709 Haney, S., S. Bachman, B. Cooper, S. Kupper, K. McCaffrey, L. Van Roekel, S. Stevenson, B. Fox-Kemper, and R. Ferrari. “Hurricane Wake Restratification Rates of One-, Two- and Three-Dimensional Processes.” Journal of Marine Research 70, no. 6 (November 1, 2012): 824–850. https://orcid.org/0000-0002-3736-1956 en_US http://dx.doi.org/10.1357/002224012806770937 Journal of Marine Research Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. application/pdf Sears Foundation for Marine Research, Yale University Prof. Ferrari via Chris Sherratt
spellingShingle Haney, S.
Bachman, S.
Cooper, B.
Kupper, S.
McCaffrey, Katherine
Van Roekel, L.
Stevenson, S.
Fox-Kemper, Baylor
Ferrari, Raffaele
Hurricane wake restratification rates of one-, two- and three-dimensional processes
title Hurricane wake restratification rates of one-, two- and three-dimensional processes
title_full Hurricane wake restratification rates of one-, two- and three-dimensional processes
title_fullStr Hurricane wake restratification rates of one-, two- and three-dimensional processes
title_full_unstemmed Hurricane wake restratification rates of one-, two- and three-dimensional processes
title_short Hurricane wake restratification rates of one-, two- and three-dimensional processes
title_sort hurricane wake restratification rates of one two and three dimensional processes
url http://hdl.handle.net/1721.1/87709
https://orcid.org/0000-0002-3736-1956
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