Upper Ocean Hydrography and Currents in the Japan Sea

The long-term goal of this project is to better understand the properties of the upper portion of the water column in the Japan Sea. It is important to understand the seasonal cycle in the upper 1000 m of the Japan Sea: how the Sea stratifies in spring and summer and how it forms a mixed layer in fa...

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Main Author: Riser, Stephen C.
Other Authors: WASHINGTON UNIV SEATTLE SCHOOL OF OCEANOGRAPHY
Format: Text
Language:English
Published: 1998
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA537365
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA537365
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spelling ftdtic:ADA537365 2023-05-15T18:28:26+02:00 Upper Ocean Hydrography and Currents in the Japan Sea Riser, Stephen C. WASHINGTON UNIV SEATTLE SCHOOL OF OCEANOGRAPHY 1998-09-30 text/html http://www.dtic.mil/docs/citations/ADA537365 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA537365 en eng http://www.dtic.mil/docs/citations/ADA537365 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography Hydrology Limnology and Potamology *OCEAN CURRENTS *HYDROGRAPHY *JAPAN SEA MIXED LAYER(MARINE) SALINITY STRATIFICATION SEASONAL VARIATIONS FLOATS TEMPERATURE CONVECTION(HEAT TRANSFER) UPPER OCEAN WATER COLUMN Text 1998 ftdtic 2016-02-23T06:07:41Z The long-term goal of this project is to better understand the properties of the upper portion of the water column in the Japan Sea. It is important to understand the seasonal cycle in the upper 1000 m of the Japan Sea: how the Sea stratifies in spring and summer and how it forms a mixed layer in fall and winter, sometimes with deep convection occurring. I want to be able to study the circulation and hydrography of the upper 1000 m of the Japan Sea over at least a few complete seasonal cycles in order to understand the process of mixed-layer formation and destruction there. In some ways the Japan Sea behaves as a subtropical ocean, and in other ways it is more like a subarctic one; as a result, it is a useful laboratory for studying many oceanographic processes that occur throughout the world ocean. I plan to use PALACE floats in this study, and the work discussed here will fit into a larger program in the Japan Sea with about 20 PIs. See also ADM002252. Text Subarctic 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
Hydrology
Limnology and Potamology
*OCEAN CURRENTS
*HYDROGRAPHY
*JAPAN SEA
MIXED LAYER(MARINE)
SALINITY
STRATIFICATION
SEASONAL VARIATIONS
FLOATS
TEMPERATURE
CONVECTION(HEAT TRANSFER)
UPPER OCEAN
WATER COLUMN
spellingShingle Physical and Dynamic Oceanography
Hydrology
Limnology and Potamology
*OCEAN CURRENTS
*HYDROGRAPHY
*JAPAN SEA
MIXED LAYER(MARINE)
SALINITY
STRATIFICATION
SEASONAL VARIATIONS
FLOATS
TEMPERATURE
CONVECTION(HEAT TRANSFER)
UPPER OCEAN
WATER COLUMN
Riser, Stephen C.
Upper Ocean Hydrography and Currents in the Japan Sea
topic_facet Physical and Dynamic Oceanography
Hydrology
Limnology and Potamology
*OCEAN CURRENTS
*HYDROGRAPHY
*JAPAN SEA
MIXED LAYER(MARINE)
SALINITY
STRATIFICATION
SEASONAL VARIATIONS
FLOATS
TEMPERATURE
CONVECTION(HEAT TRANSFER)
UPPER OCEAN
WATER COLUMN
description The long-term goal of this project is to better understand the properties of the upper portion of the water column in the Japan Sea. It is important to understand the seasonal cycle in the upper 1000 m of the Japan Sea: how the Sea stratifies in spring and summer and how it forms a mixed layer in fall and winter, sometimes with deep convection occurring. I want to be able to study the circulation and hydrography of the upper 1000 m of the Japan Sea over at least a few complete seasonal cycles in order to understand the process of mixed-layer formation and destruction there. In some ways the Japan Sea behaves as a subtropical ocean, and in other ways it is more like a subarctic one; as a result, it is a useful laboratory for studying many oceanographic processes that occur throughout the world ocean. I plan to use PALACE floats in this study, and the work discussed here will fit into a larger program in the Japan Sea with about 20 PIs. See also ADM002252.
author2 WASHINGTON UNIV SEATTLE SCHOOL OF OCEANOGRAPHY
format Text
author Riser, Stephen C.
author_facet Riser, Stephen C.
author_sort Riser, Stephen C.
title Upper Ocean Hydrography and Currents in the Japan Sea
title_short Upper Ocean Hydrography and Currents in the Japan Sea
title_full Upper Ocean Hydrography and Currents in the Japan Sea
title_fullStr Upper Ocean Hydrography and Currents in the Japan Sea
title_full_unstemmed Upper Ocean Hydrography and Currents in the Japan Sea
title_sort upper ocean hydrography and currents in the japan sea
publishDate 1998
url http://www.dtic.mil/docs/citations/ADA537365
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA537365
genre Subarctic
genre_facet Subarctic
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA537365
op_rights Approved for public release; distribution is unlimited.
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