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:	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) Indian Pacific Southern Ocean
Online Access:	http://www.dtic.mil/docs/citations/ADA622494 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA622494

Description
Summary:	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.