Hydrographic and biological changes in the Taiwan Strait during the 1997-1998 El Niño winter

Details Hydrographic and biological changes in the Taiwan Strait during the 1997-1998 El Niño winter Hydrographic and biological changes in the Taiwan Strait during the 1997-1998 El Niño winter

Jun 2005

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005georl..3211601s&link_type=abstract

Geophysical Research Letters, Volume 32, Issue 11, CiteID L11601

Mathematics

Logic

6

Oceanography: General: Climate And Interannual Variability (1616, 1635, 3305, 3309, 4513), Oceanography: General: Descriptive And Regional Oceanography, Oceanography: General: Marginal And Semi-Enclosed Seas, Oceanography: General: Physical And Biogeochemical Interactions

Scientific paper

During the 1997-1998 El Niño event, the average sea surface temperature (SST) in the Taiwan Strait (TWS) in the winter was ~1.4°C higher than that of the winter climatological mean. The areal ratio of the warm water (>=2°C above the regional mean) to the cold water (>=2°C below the regional mean) in the TWS increased by 25% while the area of the eutrophic water (chlorophyll a >1 mg m-3) was halved. Field observations also indicate that the mixed layer in the TWS became more nutrient-poor during this winter. These observations are consistent with a diminished advection of the cold and eutrophic Zhe-Min Coastal Water, and, concomitantly, an expansive intrusion of the warm and oligotrophic South China Sea Warm Current/Kuroshio Branch Water to the TWS as the northeast monsoon was weakened. Thus, El Niño events potentially can have significant ecological impacts on the TWS.

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