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Volumn 30, Issue 2, 2003, Pages
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How do high-latitude North Atlantic climate signals the crossover between the Deep Western Boundary current and the Gulf stream?
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Author keywords
[No Author keywords available]
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Indexed keywords
BATHYMETRY;
WATER WAVES;
OCEAN CURRENTS;
SEAWATER;
WAVE PROPAGATION;
CLIMATE SIGNALS;
CONTINENTAL SLOPE;
DEEP WESTERN BOUNDARY CURRENTS;
LABRADOR SEA WATERS;
TOPOGRAPHIC WAVES;
TRANSIENT SIGNAL;
WATER MASS TRANSPORT;
WESTERN BOUNDARY;
WIND DRIVEN GYRES;
CLIMATOLOGY;
OCEANOGRAPHY;
AIR-SEA INTERACTION;
CLIMATE SIGNAL;
GYRE;
WATER MASS;
WESTERN BOUNDARY CURRENT;
ATLANTIC OCEAN;
GULF STREAM;
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EID: 0037590988
PISSN: 00948276
EISSN: None
Source Type: Journal
DOI: 10.1029/2002GL015366 Document Type: Article |
Times cited : (3)
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References (9)
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