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).
Keywords: water movements, marine sediments, continental shelf
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