Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model
The Labrador Sea is one of the only known locations of deep open ocean convection, a process determined to play a significant role in regulating global thermohaline circulation and climate. The main hypothesis of this study is that low salinity water from the Arctic Ocean, particularly outflow throu...
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ftdtic:ADA536542 2023-05-15T14:28:55+02:00 Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model McGeehan, Timothy P. NAVAL POSTGRADUATE SCHOOL MONTEREY CA 2010-12 text/html http://www.dtic.mil/docs/citations/ADA536542 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA536542 en eng http://www.dtic.mil/docs/citations/ADA536542 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography *ARCTIC OCEAN *LABRADOR SEA GLOBAL OCEAN SURFACE CANADA CONVECTION HIGH RESOLUTION FRESH WATER ICE SCALE CLIMATE HYPOTHESES SALINITY CIRCULATION DEEP OCEANS SEA ICE OPEN WATER ARCTIC REGIONS SALT WATER ARCHIPELAGOES BAFFIN BAY SPATIAL DISTRIBUTION THERMAL PROPERTIES MATHEMATICAL MODELS Text 2010 ftdtic 2016-02-23T05:49:12Z The Labrador Sea is one of the only known locations of deep open ocean convection, a process determined to play a significant role in regulating global thermohaline circulation and climate. The main hypothesis of this study is that low salinity water from the Arctic Ocean, particularly outflow through the Canadian Arctic Archipelago (CAA), may affect Labrador Sea deep convection. To address it, output from a pan-Arctic high-resolution coupled ice-ocean model was examined. Volume and freshwater fluxes through the CAA for 1979-2004 were found in good agreement with the observations. Further analyses suggest that the flow through the major CAA channels depends on the sea surface height gradient between the Arctic Ocean and northern Baffin Bay. Freshwater flux anomalies entering the Labrador Sea through Davis Strait do not immediately affect deep convection. Instead, eddies and sea ice acting on shorter time scales can move freshwater to locations of active convection and halt the process, which underscores the importance of high-resolution. Also, changing ice conditions revealed the Northwest Passage was a possible shipping route in three summers. Finally, preliminary results from an eddy-resolving model configuration suggest that many of the shortcomings in this model may be rectified with higher spatial resolution. Text Arctic Archipelago Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Canadian Arctic Archipelago Davis Strait Labrador Sea Northwest passage Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic Arctic Ocean Baffin Bay Canada Canadian Arctic Archipelago Northwest Passage |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
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ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography *ARCTIC OCEAN *LABRADOR SEA GLOBAL OCEAN SURFACE CANADA CONVECTION HIGH RESOLUTION FRESH WATER ICE SCALE CLIMATE HYPOTHESES SALINITY CIRCULATION DEEP OCEANS SEA ICE OPEN WATER ARCTIC REGIONS SALT WATER ARCHIPELAGOES BAFFIN BAY SPATIAL DISTRIBUTION THERMAL PROPERTIES MATHEMATICAL MODELS |
spellingShingle |
Physical and Dynamic Oceanography *ARCTIC OCEAN *LABRADOR SEA GLOBAL OCEAN SURFACE CANADA CONVECTION HIGH RESOLUTION FRESH WATER ICE SCALE CLIMATE HYPOTHESES SALINITY CIRCULATION DEEP OCEANS SEA ICE OPEN WATER ARCTIC REGIONS SALT WATER ARCHIPELAGOES BAFFIN BAY SPATIAL DISTRIBUTION THERMAL PROPERTIES MATHEMATICAL MODELS McGeehan, Timothy P. Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model |
topic_facet |
Physical and Dynamic Oceanography *ARCTIC OCEAN *LABRADOR SEA GLOBAL OCEAN SURFACE CANADA CONVECTION HIGH RESOLUTION FRESH WATER ICE SCALE CLIMATE HYPOTHESES SALINITY CIRCULATION DEEP OCEANS SEA ICE OPEN WATER ARCTIC REGIONS SALT WATER ARCHIPELAGOES BAFFIN BAY SPATIAL DISTRIBUTION THERMAL PROPERTIES MATHEMATICAL MODELS |
description |
The Labrador Sea is one of the only known locations of deep open ocean convection, a process determined to play a significant role in regulating global thermohaline circulation and climate. The main hypothesis of this study is that low salinity water from the Arctic Ocean, particularly outflow through the Canadian Arctic Archipelago (CAA), may affect Labrador Sea deep convection. To address it, output from a pan-Arctic high-resolution coupled ice-ocean model was examined. Volume and freshwater fluxes through the CAA for 1979-2004 were found in good agreement with the observations. Further analyses suggest that the flow through the major CAA channels depends on the sea surface height gradient between the Arctic Ocean and northern Baffin Bay. Freshwater flux anomalies entering the Labrador Sea through Davis Strait do not immediately affect deep convection. Instead, eddies and sea ice acting on shorter time scales can move freshwater to locations of active convection and halt the process, which underscores the importance of high-resolution. Also, changing ice conditions revealed the Northwest Passage was a possible shipping route in three summers. Finally, preliminary results from an eddy-resolving model configuration suggest that many of the shortcomings in this model may be rectified with higher spatial resolution. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA |
format |
Text |
author |
McGeehan, Timothy P. |
author_facet |
McGeehan, Timothy P. |
author_sort |
McGeehan, Timothy P. |
title |
Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model |
title_short |
Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model |
title_full |
Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model |
title_fullStr |
Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model |
title_full_unstemmed |
Freshwater Export from the Arctic Ocean and its Downstream Effect on Labrador Sea Deep Convection in a High-Resolution Numerical Model |
title_sort |
freshwater export from the arctic ocean and its downstream effect on labrador sea deep convection in a high-resolution numerical model |
publishDate |
2010 |
url |
http://www.dtic.mil/docs/citations/ADA536542 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA536542 |
geographic |
Arctic Arctic Ocean Baffin Bay Canada Canadian Arctic Archipelago Northwest Passage |
geographic_facet |
Arctic Arctic Ocean Baffin Bay Canada Canadian Arctic Archipelago Northwest Passage |
genre |
Arctic Archipelago Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Canadian Arctic Archipelago Davis Strait Labrador Sea Northwest passage Sea ice |
genre_facet |
Arctic Archipelago Arctic Arctic Ocean Baffin Bay Baffin Bay Baffin Canadian Arctic Archipelago Davis Strait Labrador Sea Northwest passage Sea ice |
op_source |
DTIC |
op_relation |
http://www.dtic.mil/docs/citations/ADA536542 |
op_rights |
Approved for public release; distribution is unlimited. |
_version_ |
1766303044007362560 |