The T-S Gradient method
Subtitle: a new method of computing geostrophic currents over large ocean areas
By: by Warren Wilson Denner
Contributors: Naval Postgraduate School (U.S.)
Publisher: Naval Postgraduate School
Published: 1969
Place of publication: Monterey, California
Language: eng
Number of pages: 192
Subjects: Ocean temperature; Ocean currents; Computer programs
Description: Requirements for indirect computation of geostrophic surface currents over large ocean areas are discussed. These requirements point to a need to simplify standard geostrophic computations, and to separate the first order thermal and haline contributions to geostrophic flow. The equations of motion for geostrophic flow are reviewed and the standard geostrophic computations discussed. Errors and limitations in the geostrophic method are reviewed. Previous attempts to simplify geostrophic computations are discussed and shown to be inadequate for synoptic computation over hemispheric ocean areas. It is shown that the Helland-Hansen equation can be rewritten such that the geostrophic velocity is composed of a temperature structure term and a salinity structure term. (Author)
Notes: Title from cover.

"June 1969"--Cover.

"NPS-58DW9072A"--Cover.

Author(s) key words: Surface currents, geostrophic computations, dynamic computations, T-S gradient method.

Includes bibliographical references (p. 100-105).

"Approved for public release; distribution unlimited"--Cover.

Technical report; 1969.

kmc/kmc 9/14/09.