Return to search

The T-S gradient method, a new method of computing geostrophic currents over large ocean areas

Graduation date: 1969 / Best scan available for p.126-158. Original is a black and white photocopy.

Identiferoai:union.ndltd.org:ORGSU/oai:ir.library.oregonstate.edu:1957/28296
Date14 April 1969
CreatorsDenner, Warren Wilson
ContributorsNeshyba, Stephen
Source SetsOregon State University
Languageen_US
Detected LanguageEnglish
TypeThesis/Dissertation

Page generated in 0.0339 seconds