A note on "Why does the Ballenas Channel have the coldest SST in the Gulf of California?"

Geophysical Research Letters

Volumn 34, Issue 2, 2007, Pages

  Marinone, S G ^a  

^a CENTRO DE INVESTIGACIÓN CIENTÍFICA Y DE EDUCACIÓN SUPERIOR DE ENSENADA   (Mexico)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC TEMPERATURE; CATCHMENTS; CHANNEL FLOW; OCEAN CURRENTS;

SEA SURFACE TEMPERATURE; THREE-DIMENSIONAL NONLINEAR BAROCLINIC MODEL;

GEOPHYSICS;

BAROCLINIC MOTION; CIRCULATION MODELING; MIXED LAYER; OCEAN BASIN; OCEANIC CIRCULATION; SEA SURFACE TEMPERATURE; THREE-DIMENSIONAL MODELING; UPWELLING;

BAJA CALIFORNIA [(STT) MEXICO]; BALLENAS CHANNEL; GULF OF CALIFORNIA; MEXICO [NORTH AMERICA]; NORTH AMERICA; PACIFIC OCEAN;

EID: 34548040194     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2006GL028589     Document Type: Article

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