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Home Order Direct Density Flow Models Geology Simulations Water Masses Thermocline Upwelling/Downwelling Halocline/Internal Seiche Junior Model Additional Information
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Upwelling is the upward movement of ocean water that occurs when winds push surface water aside and it is replaced with cold, deep water that originates on the ocean bottom. Downwelling is
the circulation pattern in which surface water moves vertically downward. ( Click Pictures to Enlarge )
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