The effects of rainfall on temperature and salinity in the surface layer of the equatorial Pacific
Measurements of temperature and salinity in the upper 5 m of the ocean along the equator showed cool fresh anomalies due to rain showers. The measurements were made between 140 W and 110 W during April 1987, an El Nino year. The eastern equatorial Pacific was characterized by weak winds (3 m/s avera...
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Language: | en_US |
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2012
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Online Access: | http://hdl.handle.net/1957/27797 |