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- W893500643 abstract "The chlorophyll concentration at the surface of the tropical Pacific has been monitored through the 1982-83 ENSO, owing to the SURTROPAC ships of opportunity network. The event was characterized by a decrease in chlorophyll concentrations at the equator, where a belt of relatively rich water however persisted. The most striking anomaly was observed in the western Pacific between SON and IsoN. In this region, chlorophyll at the surface is generally less than 0.07 mg m-3, caused by a mixed layer exhausted in nutrients and by strong density gradient in the thermocline. From October 1982 to March 1983, higher concentrations up to 0.70 mg m-3 have been recorded by the network. This is consistent with the shallowing of the thermocline which characterizes all ENSO events and was especially well marked in 1982-83. This bloom can be explained by nutrients supplied to the surface mixed layer through the thermocline. Turbulent vertical mixing was indeed made easier during this ENSO event by shallow thermocline, abnormally strong winds, and mixed layer cooler than usual by 2°C. N03 data from this region show that 0.07 moles m-2 of nitrates have been consumed between January 1982 and January 1983; this value which does not take horizontal advection into account is probably underestimated." @default.
- W893500643 created "2016-06-24" @default.
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- W893500643 date "1989-01-01" @default.
- W893500643 modified "2023-09-23" @default.
- W893500643 title "Abnormal bloom of phytoplankton around 10°N in the western Pacific during the 1982-83 ENSO" @default.
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