Ocean Surface Topography

نویسنده

  • Lee-Lueng Fu
چکیده

Definition The deviation of the height of the ocean surface from the geoid is known as the ocean surface topography. The geoid is a surface on which the Earth’s gravity field is uniform. The ocean surface topography is caused by ocean waves, tides, currents, and the loading of atmospheric pressure. The main application of ocean surface topography is for the determination of large-scale ocean circulation.

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تاریخ انتشار 2014