A Process Oriented Study of Shallow Convection in Polar Oceans.
The objectives of this study are to obtain a better understanding of shallow ocean circulations beneath leads in sea ice associated with ice formation and brine rejection. We would also like to access the role of under ice boundary layer turbulence in mixing away the signature of haline convection b...
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ftdtic:ADA299592 2023-05-15T16:36:52+02:00 A Process Oriented Study of Shallow Convection in Polar Oceans. Smith, David C., IV CALIFORNIA UNIV SANTA CRUZ 1994-09-30 text/html http://www.dtic.mil/docs/citations/ADA299592 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA299592 en eng http://www.dtic.mil/docs/citations/ADA299592 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *OCEAN CURRENTS *SEA ICE POLAR REGIONS TURBULENT BOUNDARY LAYER ICE FORMATION FLOW FIELDS HYDROSTATICS CONVECTION(HEAT TRANSFER) MIXED LAYER(MARINE) OCEAN MODELS CONVECTION(ATMOSPHERIC) SHALLOW DEPTH UNDERICE Text 1994 ftdtic 2016-02-19T18:32:29Z The objectives of this study are to obtain a better understanding of shallow ocean circulations beneath leads in sea ice associated with ice formation and brine rejection. We would also like to access the role of under ice boundary layer turbulence in mixing away the signature of haline convection beneath leads. Text Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Physical and Dynamic Oceanography Snow Ice and Permafrost *OCEAN CURRENTS *SEA ICE POLAR REGIONS TURBULENT BOUNDARY LAYER ICE FORMATION FLOW FIELDS HYDROSTATICS CONVECTION(HEAT TRANSFER) MIXED LAYER(MARINE) OCEAN MODELS CONVECTION(ATMOSPHERIC) SHALLOW DEPTH UNDERICE |
spellingShingle |
Physical and Dynamic Oceanography Snow Ice and Permafrost *OCEAN CURRENTS *SEA ICE POLAR REGIONS TURBULENT BOUNDARY LAYER ICE FORMATION FLOW FIELDS HYDROSTATICS CONVECTION(HEAT TRANSFER) MIXED LAYER(MARINE) OCEAN MODELS CONVECTION(ATMOSPHERIC) SHALLOW DEPTH UNDERICE Smith, David C., IV A Process Oriented Study of Shallow Convection in Polar Oceans. |
topic_facet |
Physical and Dynamic Oceanography Snow Ice and Permafrost *OCEAN CURRENTS *SEA ICE POLAR REGIONS TURBULENT BOUNDARY LAYER ICE FORMATION FLOW FIELDS HYDROSTATICS CONVECTION(HEAT TRANSFER) MIXED LAYER(MARINE) OCEAN MODELS CONVECTION(ATMOSPHERIC) SHALLOW DEPTH UNDERICE |
description |
The objectives of this study are to obtain a better understanding of shallow ocean circulations beneath leads in sea ice associated with ice formation and brine rejection. We would also like to access the role of under ice boundary layer turbulence in mixing away the signature of haline convection beneath leads. |
author2 |
CALIFORNIA UNIV SANTA CRUZ |
format |
Text |
author |
Smith, David C., IV |
author_facet |
Smith, David C., IV |
author_sort |
Smith, David C., IV |
title |
A Process Oriented Study of Shallow Convection in Polar Oceans. |
title_short |
A Process Oriented Study of Shallow Convection in Polar Oceans. |
title_full |
A Process Oriented Study of Shallow Convection in Polar Oceans. |
title_fullStr |
A Process Oriented Study of Shallow Convection in Polar Oceans. |
title_full_unstemmed |
A Process Oriented Study of Shallow Convection in Polar Oceans. |
title_sort |
process oriented study of shallow convection in polar oceans. |
publishDate |
1994 |
url |
http://www.dtic.mil/docs/citations/ADA299592 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA299592 |
genre |
Ice permafrost Sea ice |
genre_facet |
Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA299592 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
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1766027182408204288 |