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- Sea surface height above geoid refers to the sea surface height (SSH) relative to the marine geoid1. The marine geoid is the equipotential surface, and the SSH is the distance between the sea surface and the geoid, with waves and tides filtered out1. The sea surface height can be computed by subtracting the distance measured to the water surface from the known altitude of the satellite’s orbit above the Ellipsoid2. The geoid surface cannot be directly observed, so heights above or below the geoid surface are inferred by making gravity measurements and modeling the surface mathematically3.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.The absolute dynamic ocean topography (hereafter referred to as DOT) ˆD is the sea surface height (SSH, waves and tides filtered out) relative to the marine geoid (i.e., the equipotential surface), ˆD = S - ˆN, where S is the SSH; ˆN is the marine geoid height above the reference ellipsoid (Fig. 1).os.copernicus.org/articles/14/947/2018/With this information the sensor is able to compute the sea surface height by subtracting the distance measured to the water surface,from the known altitude of the satellite’s orbit above the Ellipsoid (reference level). The sea surface can then be expressed in terms of its position with respect to the geoid (sea surface height above the geoid).www.esa.int/SPECIALS/Eduspace_Weather_EN/S…Because the geoid surface cannot be directly observed, heights above or below the geoid surface can't be directly measured and are inferred by making gravity measurements and modeling the surface mathematically.www.esri.com/news/arcuser/0703/geoid1of3.html
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