Velocity and Temperature Observations During the Seasonal Response of the Equatorial Atlantic Experiment at 0 Degrees, 28 Degrees W

Authors

Robert H. Weisberg, University of South FloridaFollow
J. H. Hickman, University of South Florida
T. Y. Tang, University of South Florida
T. J. Weingartner, University of South Florida

Document Type

Article

Publication Date

5-15-1987

Digital Object Identifier (DOI)

https://doi.org/10.1029/JC092iC05p05061

Abstract

Continuous 2.7‐year time series of upper ocean currents and temperature at 0°, 28°W collected during the Seasonal Response of the Equatorial Atlantic Experiment are presented. The thermocline underwent distinctive annual cycles in response to forcing by the surface wind stress, and the core of the Equatorial Undercurrent tracked the thermocline. While the vertical position of the thermocline and the undercurrent appear to be simply related, the transport of the undercurrent did not show a replicating annual cycle, and the speed at the undercurrent core remained relatively constant. Near surface flow when averaged over the 2.7 years was not statistically different from zero, and a westward flowing South Equatorial Current was rarely established despite strong easterly wind stress in all 3 years. Cross‐equatorial flow was also zero in the mean at this location.

Rights Information

Terms of use for work posted in Scholar Commons.

Was this content written or created while at USF?

Yes

Citation / Publisher Attribution

Journal of Geophysical Research, v. 92, issue C5, p. 5061-5075

Copyright 1987 by the American Geophysical Union.

Scholar Commons Citation

Weisberg, Robert H.; Hickman, J. H.; Tang, T. Y.; and Weingartner, T. J., "Velocity and Temperature Observations During the Seasonal Response of the Equatorial Atlantic Experiment at 0 Degrees, 28 Degrees W" (1987). Marine Science Faculty Publications. 74.
https://digitalcommons.usf.edu/msc_facpub/74