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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Bibliographic Details
Main Author: Smith, David C., IV
Other Authors: CALIFORNIA UNIV SANTA CRUZ
Format: Text
Language:English
Published: 1994
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA299592
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA299592
id ftdtic:ADA299592
record_format openpolar
spelling 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
institution Open Polar
collection 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
_version_ 1766027182408204288