Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea

The main goal of this objective is to use coupled ocean-ice numerical models to study the basin scale ocean circulation and ocean-ice interaction in the Okhotsk Sea, and to examine important processes that maintain the unique oceanographic setting, such as the ODTL in this large marginal sea. We use...

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Bibliographic Details
Main Author: Yang, Jiayan
Other Authors: WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
Format: Text
Language:English
Published: 1998
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA353929
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA353929
id ftdtic:ADA353929
record_format openpolar
spelling ftdtic:ADA353929 2023-05-15T16:37:07+02:00 Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea Yang, Jiayan WOODS HOLE OCEANOGRAPHIC INSTITUTION MA 1998-09-21 text/html http://www.dtic.mil/docs/citations/ADA353929 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA353929 en eng http://www.dtic.mil/docs/citations/ADA353929 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Physical and Dynamic Oceanography Snow Ice and Permafrost *OCEAN CURRENTS *SEA ICE WIND ATMOSPHERIC TEMPERATURE SEASONAL VARIATIONS HYDROGRAPHY BASINS(GEOGRAPHIC) OKHOTSK SEA OKHOTSK DICHOTHERMAL LAYER ODTL(OKHOTSK DICHOTHERMAL LAYER) *OCEAN ICE INTERACTIONS Text 1998 ftdtic 2016-02-20T00:23:23Z The main goal of this objective is to use coupled ocean-ice numerical models to study the basin scale ocean circulation and ocean-ice interaction in the Okhotsk Sea, and to examine important processes that maintain the unique oceanographic setting, such as the ODTL in this large marginal sea. We use a hierarchy of models, from a basin-averaged column model of ocean-ice interactions (Yang and Honjo, 1996) to a 3-D primitive equation ocean general circulation models coupled with a dynamical and thermodynamical sea-ice model. Meanwhile, we have analyzed some unpublished in situ observations (mainly hydrography records from the Japanese Hydrography Office), satellite SSM/I data of sea-ice concentration, and meteorological observations (from Comprehensive Ocean and Atmosphere Data Sets (COADS) and from the Japan Meteorology Agency) to examine ocean-ice interactions and mechanisms for interannual variations. Text Ice okhotsk sea permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Okhotsk
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
WIND
ATMOSPHERIC TEMPERATURE
SEASONAL VARIATIONS
HYDROGRAPHY
BASINS(GEOGRAPHIC)
OKHOTSK SEA
OKHOTSK DICHOTHERMAL LAYER
ODTL(OKHOTSK DICHOTHERMAL LAYER)
*OCEAN ICE INTERACTIONS
spellingShingle Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*OCEAN CURRENTS
*SEA ICE
WIND
ATMOSPHERIC TEMPERATURE
SEASONAL VARIATIONS
HYDROGRAPHY
BASINS(GEOGRAPHIC)
OKHOTSK SEA
OKHOTSK DICHOTHERMAL LAYER
ODTL(OKHOTSK DICHOTHERMAL LAYER)
*OCEAN ICE INTERACTIONS
Yang, Jiayan
Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea
topic_facet Physical and Dynamic Oceanography
Snow
Ice and Permafrost
*OCEAN CURRENTS
*SEA ICE
WIND
ATMOSPHERIC TEMPERATURE
SEASONAL VARIATIONS
HYDROGRAPHY
BASINS(GEOGRAPHIC)
OKHOTSK SEA
OKHOTSK DICHOTHERMAL LAYER
ODTL(OKHOTSK DICHOTHERMAL LAYER)
*OCEAN ICE INTERACTIONS
description The main goal of this objective is to use coupled ocean-ice numerical models to study the basin scale ocean circulation and ocean-ice interaction in the Okhotsk Sea, and to examine important processes that maintain the unique oceanographic setting, such as the ODTL in this large marginal sea. We use a hierarchy of models, from a basin-averaged column model of ocean-ice interactions (Yang and Honjo, 1996) to a 3-D primitive equation ocean general circulation models coupled with a dynamical and thermodynamical sea-ice model. Meanwhile, we have analyzed some unpublished in situ observations (mainly hydrography records from the Japanese Hydrography Office), satellite SSM/I data of sea-ice concentration, and meteorological observations (from Comprehensive Ocean and Atmosphere Data Sets (COADS) and from the Japan Meteorology Agency) to examine ocean-ice interactions and mechanisms for interannual variations.
author2 WOODS HOLE OCEANOGRAPHIC INSTITUTION MA
format Text
author Yang, Jiayan
author_facet Yang, Jiayan
author_sort Yang, Jiayan
title Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea
title_short Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea
title_full Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea
title_fullStr Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea
title_full_unstemmed Modeling the Wind and Buoyancy Driven Circulation and Ice Interaction in the Okhotsk Sea
title_sort modeling the wind and buoyancy driven circulation and ice interaction in the okhotsk sea
publishDate 1998
url http://www.dtic.mil/docs/citations/ADA353929
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA353929
geographic Okhotsk
geographic_facet Okhotsk
genre Ice
okhotsk sea
permafrost
Sea ice
genre_facet Ice
okhotsk sea
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA353929
op_rights APPROVED FOR PUBLIC RELEASE
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