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Volumn 279, Issue 5355, 1998, Pages 1341-1344

The role of ocean-atmosphere interactions in tropical cooling during the Last Glacial Maximum

Author keywords

[No Author keywords available]

Indexed keywords

GROUND WATER;

EID: 0032570688     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.279.5355.1341     Document Type: Article
Times cited : (129)

References (30)
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    • note
    • The horizontal redistribution of warm surface waters during El Niño alters the topography of the thermocline - it deepens in some regions and shoals in others - while leaving unchanged the spatially averaged depth of and the temperature difference across the thermocline. That is why two-layer models of the ocean are effective tools for studying El Niño.
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    • note
    • This work was supported by a Natural Sciences and Engineering Research Council of Canada grant OGP0194151 (A.B.G.B.) and by the National Oceanic and Atmospheric Administration under contract NOAA-NA56GP0226 (S.G.H.P.). We thank the staff of the Geophysical Fluid Dynamics Laboratory for making this work possible.


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