Physics
Scientific paper
Dec 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994georl..21.2681e&link_type=abstract
Geophysical Research Letters, Volume 21, Issue 24, p. 2681-2684
Physics
17
Oceanography: General: Equatorial Oceanography, Oceanography: Physical: Currents, Oceanography: Physical: Upper Ocean Processes, Information Related To Geographic Region: Pacific Ocean
Scientific paper
From December 1992 to February 1993, 18 meridional sections of temperature, salinity, and current were collected along 156°E, from 5°S to 5°N, during the Intensive Observation Period of the Coupled Ocean-Atmosphere Response Experiment. The average conditions were characteristic of the ongoing El Niño event, with a relatively shallow thermocline and fresh surface waters. Alternating westerly and easterly wind forcing was observed, and the warm surface layer (the ``Warm Pool'') responded in a time scale of a few days by corresponding alternating flows; the equatorial current system was less affected at depth. The upper-layer oceanic temperature variability involved several mechanisms, including surface cooling by evaporation during westerly winds and entrainment from the thermocline.
Delcroix Thierry
du Penhoat Yves
Eldin Gerard
Hénin Christian
Picaut Joel
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