The Tsushima Warm Current and its Various Branches

The goal of this project is to (i) determine why the Tsushima Warm Current (TWC) splits into three separate branches; and (ii) understand how and why the Ulleung Warm Eddy (UWE) is formed.

Bibliographic Details
Main Author: Nof, Doron
Other Authors: FLORIDA STATE UNIV TALLAHASSEE DEPT OF OCEANOGRAPHY
Format: Text
Language:English
Published: 2001
Subjects:
Online Access:http://www.dtic.mil/docs/citations/ADA622494
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA622494
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record_format openpolar
spelling ftdtic:ADA622494 2023-05-15T18:24:53+02:00 The Tsushima Warm Current and its Various Branches Nof, Doron FLORIDA STATE UNIV TALLAHASSEE DEPT OF OCEANOGRAPHY 2001-09-30 text/html http://www.dtic.mil/docs/citations/ADA622494 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA622494 en eng http://www.dtic.mil/docs/citations/ADA622494 Approved for public release; distribution is unlimited. DTIC Physical and Dynamic Oceanography *OCEAN CURRENTS INDIAN OCEAN JAPAN SEA OCEAN BOTTOM TOPOGRAPHY PACIFIC OCEAN VELOCITY INDONESIAN THROUGHFLOW WATERS REDDIES SOUTHERN OCEAN TWC(TSUSHIMA WARM CURRENT) UWE(ULLEUNG WARM EDDY) Text 2001 ftdtic 2016-02-24T18:54:06Z The goal of this project is to (i) determine why the Tsushima Warm Current (TWC) splits into three separate branches; and (ii) understand how and why the Ulleung Warm Eddy (UWE) is formed. Text Southern Ocean Defense Technical Information Center: DTIC Technical Reports database Indian Pacific Southern Ocean
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Physical and Dynamic Oceanography
*OCEAN CURRENTS
INDIAN OCEAN
JAPAN SEA
OCEAN BOTTOM TOPOGRAPHY
PACIFIC OCEAN
VELOCITY
INDONESIAN THROUGHFLOW WATERS
REDDIES
SOUTHERN OCEAN
TWC(TSUSHIMA WARM CURRENT)
UWE(ULLEUNG WARM EDDY)
spellingShingle Physical and Dynamic Oceanography
*OCEAN CURRENTS
INDIAN OCEAN
JAPAN SEA
OCEAN BOTTOM TOPOGRAPHY
PACIFIC OCEAN
VELOCITY
INDONESIAN THROUGHFLOW WATERS
REDDIES
SOUTHERN OCEAN
TWC(TSUSHIMA WARM CURRENT)
UWE(ULLEUNG WARM EDDY)
Nof, Doron
The Tsushima Warm Current and its Various Branches
topic_facet Physical and Dynamic Oceanography
*OCEAN CURRENTS
INDIAN OCEAN
JAPAN SEA
OCEAN BOTTOM TOPOGRAPHY
PACIFIC OCEAN
VELOCITY
INDONESIAN THROUGHFLOW WATERS
REDDIES
SOUTHERN OCEAN
TWC(TSUSHIMA WARM CURRENT)
UWE(ULLEUNG WARM EDDY)
description The goal of this project is to (i) determine why the Tsushima Warm Current (TWC) splits into three separate branches; and (ii) understand how and why the Ulleung Warm Eddy (UWE) is formed.
author2 FLORIDA STATE UNIV TALLAHASSEE DEPT OF OCEANOGRAPHY
format Text
author Nof, Doron
author_facet Nof, Doron
author_sort Nof, Doron
title The Tsushima Warm Current and its Various Branches
title_short The Tsushima Warm Current and its Various Branches
title_full The Tsushima Warm Current and its Various Branches
title_fullStr The Tsushima Warm Current and its Various Branches
title_full_unstemmed The Tsushima Warm Current and its Various Branches
title_sort tsushima warm current and its various branches
publishDate 2001
url http://www.dtic.mil/docs/citations/ADA622494
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA622494
geographic Indian
Pacific
Southern Ocean
geographic_facet Indian
Pacific
Southern Ocean
genre Southern Ocean
genre_facet Southern Ocean
op_source DTIC
op_relation http://www.dtic.mil/docs/citations/ADA622494
op_rights Approved for public release; distribution is unlimited.
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