Global climate change and intensification of coastal ocean upwelling

Science

Volumn 247, Issue 4939, 1990, Pages 198-201

  Bakun, Andrew ^a  

^a NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATIC CHANGE; COAST; GLOBAL; GREENHOUSE EFFECT; MARINE ECOSYSTEM; OCEAN UPWELLING; UPWELLING;

USA, CALIFORNIA;

ARTICLE; CLIMATE; NONHUMAN; PRIORITY JOURNAL; SEA; TEMPERATURE; THEORETICAL STUDY;

EID: 0025198330     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.247.4939.198     Document Type: Article

References (29)

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28. On the other hand, the trade winds in the tropical Pacific likewise seem to have increased during this same period [K. D. B. Whysall, N. S. Cooper, G. R. Bigg, Nature 327, 216 (1987)]. Whether seasonally increased alongshore winds along the continental boundaries (equatorward along the eastern ocean boundary, poleward along the western boundary) resulting from enhanced onshore-offshore temperature contrasts could contribute to an increased trade wind circulation is a matter for further study.
29. Indicated significance levels are taken directly from standard tables of the Student's t distribution, without adjustment for residual autocorrelation.