. The effect of interior motion on seasonal thermocline evolution. . I I I ' I 1 I âI ' I ' â I I 0 30 60 90 120 . 150 180 210 240 270 300 330 360 TIME DRYS Figure h (meters), One-Year Period Interior Hotion. CD oj a en Q_ to LO.

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Keywords: ., bookcentury1900, booksubjectmeteorology, booksubjectoceanography