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Updated: Jul 26, 2026

A Robotic Platform to Study the Foreflipper of the California Sea Lion
Published on: January 10, 2017
Internal swash and surf
1Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543.
Abstract:
114 temperature sections, each containing an average of 10 bathythermograms, show that internal waves commonly become altered on crossing the shoaling bottom of the continental shelf in Santa Monica Bay, Calif. The alteration takes the form of internal swash (in which the lower isotherms reach farther landward than would be expected from their depth above the outer shelf or above deeper bottom) and of internal surf (that is, denoted by temperature inversions, isolated boluses of colder water at the bottom, and complex short wave-length variations of isotherms).
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