Abstract
The average monthly variation of the heat and salt balance of the upper 200 m is investigated for eight areas of the Pacific Ocean off California and Baja California. Accuracy of the method and of the nonseasonal variations of the balance is estimated. It is shown that observed heat changes are princiaplly due to radiation and advection, the heat exchange with the atmosphere being rather small and constant....
Recommended Citation
Roden, Gunnar I.. 1959. "On the heat and salt balance of the California Current region." Journal of Marine Research 18, (1). https://elischolar.library.yale.edu/journal_of_marine_research/945
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