Abstract
Interrelationships of potential temperature-salinity and potential temperature-oxyty are presented for 31 stations along 5°N, the equator, and 5°S during the southwest monsoon, and the volumes of water in bivariate classes of potential temperature against salinity are estimated throughout each section. The sources of different water types and their flow pattern are discussed....
Recommended Citation
Sharma, G. S.. 1976. "Transequatorial movement of water masses in the Indian Ocean." Journal of Marine Research 34, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1352
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