Atmospheric Forcing of Ocean Convection in the Labrador Sea
My long-term goal is to improve our ability to model and predict dynamic and thermodynamic ocean processes in high-latitude regions. Specifically, I seek to understand and predict how atmospheric forcing such as surface momentum, heat and salinity fluxes affects the ocean. The ultimate objective of...
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ftdtic:ADA550953 2023-05-15T17:05:59+02:00 Atmospheric Forcing of Ocean Convection in the Labrador Sea Guest, Peter NAVAL POSTGRADUATE SCHOOL MONTEREY CA DEPT OF METEOROLOGY 1998-01 text/html http://www.dtic.mil/docs/citations/ADA550953 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA550953 en eng http://www.dtic.mil/docs/citations/ADA550953 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography Thermodynamics *ATMOSPHERES *LABRADOR SEA *OCEANOGRAPHIC DATA *THERMODYNAMICS CONVECTION FEEDBACK HEAT HIGH LATITUDES INPUT LONG RANGE(TIME) MATHEMATICAL MODELS MOMENTUM REGIONS SALINITY SCALE SURFACES Text 1998 ftdtic 2016-02-23T09:27:55Z My long-term goal is to improve our ability to model and predict dynamic and thermodynamic ocean processes in high-latitude regions. Specifically, I seek to understand and predict how atmospheric forcing such as surface momentum, heat and salinity fluxes affects the ocean. The ultimate objective of this study is to understand the relation between atmospheric forcing and deep convection in high-latitude seas, in particular, the Labrador Sea. The atmosphere provides the crucial input into the upper ocean, which results in destabilization and convection in the ocean. A necessary component of this objective is to verify and improve the parameterizations which numerical models use to specify surface fluxes over high-latitude marine regions. Another objective is to enhance our understanding of how these surface fluxes are related to upper-level and large scale atmospheric features. Finally, I seek to quantify the various feedbacks that occur between the ocean and atmosphere in the Labrador Sea and other high-latitude, oceans. See also ADM002252. Text Labrador Sea Defense Technical Information Center: DTIC Technical Reports database |
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Defense Technical Information Center: DTIC Technical Reports database |
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English |
topic |
Physical and Dynamic Oceanography Thermodynamics *ATMOSPHERES *LABRADOR SEA *OCEANOGRAPHIC DATA *THERMODYNAMICS CONVECTION FEEDBACK HEAT HIGH LATITUDES INPUT LONG RANGE(TIME) MATHEMATICAL MODELS MOMENTUM REGIONS SALINITY SCALE SURFACES |
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Physical and Dynamic Oceanography Thermodynamics *ATMOSPHERES *LABRADOR SEA *OCEANOGRAPHIC DATA *THERMODYNAMICS CONVECTION FEEDBACK HEAT HIGH LATITUDES INPUT LONG RANGE(TIME) MATHEMATICAL MODELS MOMENTUM REGIONS SALINITY SCALE SURFACES Guest, Peter Atmospheric Forcing of Ocean Convection in the Labrador Sea |
topic_facet |
Physical and Dynamic Oceanography Thermodynamics *ATMOSPHERES *LABRADOR SEA *OCEANOGRAPHIC DATA *THERMODYNAMICS CONVECTION FEEDBACK HEAT HIGH LATITUDES INPUT LONG RANGE(TIME) MATHEMATICAL MODELS MOMENTUM REGIONS SALINITY SCALE SURFACES |
description |
My long-term goal is to improve our ability to model and predict dynamic and thermodynamic ocean processes in high-latitude regions. Specifically, I seek to understand and predict how atmospheric forcing such as surface momentum, heat and salinity fluxes affects the ocean. The ultimate objective of this study is to understand the relation between atmospheric forcing and deep convection in high-latitude seas, in particular, the Labrador Sea. The atmosphere provides the crucial input into the upper ocean, which results in destabilization and convection in the ocean. A necessary component of this objective is to verify and improve the parameterizations which numerical models use to specify surface fluxes over high-latitude marine regions. Another objective is to enhance our understanding of how these surface fluxes are related to upper-level and large scale atmospheric features. Finally, I seek to quantify the various feedbacks that occur between the ocean and atmosphere in the Labrador Sea and other high-latitude, oceans. See also ADM002252. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA DEPT OF METEOROLOGY |
format |
Text |
author |
Guest, Peter |
author_facet |
Guest, Peter |
author_sort |
Guest, Peter |
title |
Atmospheric Forcing of Ocean Convection in the Labrador Sea |
title_short |
Atmospheric Forcing of Ocean Convection in the Labrador Sea |
title_full |
Atmospheric Forcing of Ocean Convection in the Labrador Sea |
title_fullStr |
Atmospheric Forcing of Ocean Convection in the Labrador Sea |
title_full_unstemmed |
Atmospheric Forcing of Ocean Convection in the Labrador Sea |
title_sort |
atmospheric forcing of ocean convection in the labrador sea |
publishDate |
1998 |
url |
http://www.dtic.mil/docs/citations/ADA550953 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA550953 |
genre |
Labrador Sea |
genre_facet |
Labrador Sea |
op_source |
DTIC |
op_relation |
http://www.dtic.mil/docs/citations/ADA550953 |
op_rights |
Approved for public release; distribution is unlimited. |
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1766060874102996992 |