Document Type

Article

Publication Date

4-1985

Digital Object Identifier (DOI)

https://doi.org/10.1029/EO066i014p00154

Abstract

Westward traveling waves, with a period of 3 weeks and a wavelength of ∼1000 km, are observed intermittently in the central and eastern equatorial Pacific Ocean (see cover). The waves were first detected in 1975 in satellite measurements of the sea surface temperature [Legeckis, 1977]. Since then, additional measurements (under the auspices of the NOAA program Equatorial Pacific Ocean Climate Studies (EPOCS)) with a variety of instruments—drifting buoys, current meters and temperature sensors on moorings, and inverted echo sounders—have provided considerable information about these waves and have confirmed the hypothesis that they are caused by instabilities associated primarily with the latitudinal shear of the surface currents near the equator [Philander, 1978a; Cox, 1980].

Was this content written or created while at USF?

No

Citation / Publisher Attribution

Eos, Transactions American Geophysical Union, v. 66, issue 14, p. 154

©1985. American Geophysical Union. All Rights Reserved.

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