Air-sea interactions and deep convection in the Labrador Sea
Deep convection in the oceans, particularly at high latitudes, plays an important role in the climate systems of the world's oceans and atmosphere. This study was conducted to examine atmospheric forcing effects on deep convection in the Labrador Sea. The Naval Postgraduate School one dimension...
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1997
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ftnavalpschool:oai:calhoun.nps.edu:10945/7863 2024-06-09T07:47:31+00:00 Air-sea interactions and deep convection in the Labrador Sea Bramson, Laura S. Guest, Peter Garwood, Roland Naval Postgraduate School Meteorology Oceanography 1997-12 ix, 76 p.;28 cm. application/pdf https://hdl.handle.net/10945/7863 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/7863 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Labrador Sea Deep ocean convection Air-sea interactions Thesis 1997 ftnavalpschool 2024-05-15T00:35:02Z Deep convection in the oceans, particularly at high latitudes, plays an important role in the climate systems of the world's oceans and atmosphere. This study was conducted to examine atmospheric forcing effects on deep convection in the Labrador Sea. The Naval Postgraduate School one dimensional ocean mixed layer model was applied to the Labrador Sea from February 12 to March 10, 1997. The model was initialized and forced with oceanographic and atmospheric data collected onboard the R/V Knorr during the first field program of the Labrador Sea Deep Convection Experiment. An ocean mixed layer depth close to 1300m was predicted and verified using the observed data. A sensitivity study was conducted using deviations from observations as input to determine how variations in atmospheric forcing could lead to the observed and even deepened ocean mixed layer. Observed Conductivity, temperature and depth (CTD) data were used to verify the model's spatial and temporal predictions of mixed layer temperature, salinity and depth. Model predicted mixed layer depths were usually slightly deeper than those observed. The final model output predicted temperature rather accurately, but model predicted salinity values were consistently low. A variety of sensitivity studies gave new insight to the individual influences of surface fluxes, momentum stresses, precipitation, salinity and individual storm variations to the mixed layer temperature, salinity and depth of the Labrador Sea. Approved for public release; distribution is unlimited. Lieutenant Commander, United States Navy http://archive.org/details/airseinteraction109457863 Thesis Labrador Sea Naval Postgraduate School: Calhoun |
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Naval Postgraduate School: Calhoun |
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ftnavalpschool |
language |
English |
topic |
Labrador Sea Deep ocean convection Air-sea interactions |
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Labrador Sea Deep ocean convection Air-sea interactions Bramson, Laura S. Air-sea interactions and deep convection in the Labrador Sea |
topic_facet |
Labrador Sea Deep ocean convection Air-sea interactions |
description |
Deep convection in the oceans, particularly at high latitudes, plays an important role in the climate systems of the world's oceans and atmosphere. This study was conducted to examine atmospheric forcing effects on deep convection in the Labrador Sea. The Naval Postgraduate School one dimensional ocean mixed layer model was applied to the Labrador Sea from February 12 to March 10, 1997. The model was initialized and forced with oceanographic and atmospheric data collected onboard the R/V Knorr during the first field program of the Labrador Sea Deep Convection Experiment. An ocean mixed layer depth close to 1300m was predicted and verified using the observed data. A sensitivity study was conducted using deviations from observations as input to determine how variations in atmospheric forcing could lead to the observed and even deepened ocean mixed layer. Observed Conductivity, temperature and depth (CTD) data were used to verify the model's spatial and temporal predictions of mixed layer temperature, salinity and depth. Model predicted mixed layer depths were usually slightly deeper than those observed. The final model output predicted temperature rather accurately, but model predicted salinity values were consistently low. A variety of sensitivity studies gave new insight to the individual influences of surface fluxes, momentum stresses, precipitation, salinity and individual storm variations to the mixed layer temperature, salinity and depth of the Labrador Sea. Approved for public release; distribution is unlimited. Lieutenant Commander, United States Navy http://archive.org/details/airseinteraction109457863 |
author2 |
Guest, Peter Garwood, Roland Naval Postgraduate School Meteorology Oceanography |
format |
Thesis |
author |
Bramson, Laura S. |
author_facet |
Bramson, Laura S. |
author_sort |
Bramson, Laura S. |
title |
Air-sea interactions and deep convection in the Labrador Sea |
title_short |
Air-sea interactions and deep convection in the Labrador Sea |
title_full |
Air-sea interactions and deep convection in the Labrador Sea |
title_fullStr |
Air-sea interactions and deep convection in the Labrador Sea |
title_full_unstemmed |
Air-sea interactions and deep convection in the Labrador Sea |
title_sort |
air-sea interactions and deep convection in the labrador sea |
publisher |
Monterey, California. Naval Postgraduate School |
publishDate |
1997 |
url |
https://hdl.handle.net/10945/7863 |
genre |
Labrador Sea |
genre_facet |
Labrador Sea |
op_relation |
https://hdl.handle.net/10945/7863 |
op_rights |
This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. |
_version_ |
1801378640368238592 |