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- Ocean topography is the deviation of the height of the ocean surface from the geoid, caused by ocean waves, tides, currents, and atmospheric pressure1. It is determined by factors such as ocean currents, heat storage, and the shape of ocean basins and landmasses23. Topographic maps show the physical shape of dry land using elevation values, while bathymetric maps show the physical shape of the seafloor using depth values4. Scientists use multibeam sonar surveys to image the sea-bottom and study underwater features5.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Ocean Surface Topography is the deviation of the height of the ocean surface from the geoid, or 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.podaac.jpl.nasa.gov/OceanSurfaceTopographyWe need to know both ocean currents and heat storage of the ocean. Like winds blow around the highs and lows of atmospheric pressure, ocean currents flow around highs and lows of oceanic pressure. These can be determined from the height of the sea surface, also known as ocean surface topography.sealevel.jpl.nasa.gov/ocean-observation/why-stud…The ocean has an interconnected current, or circulation, system powered by wind, tides, Earth’s rotation (Coriolis effect), the sun (solar energy), and water density differences. The topography and shape of ocean basins and nearby landmasses also influence ocean currents.www.nationalgeographic.org/media/ocean-current…Topographic maps show the physical shape of dry land using elevation values. Bathymetric maps show the physical shape of the seafloor using depth values. Together, topographic and bathymetric maps show the physical features on the Earth’s surface.oceanexplorer.noaa.gov/explainers/mapping.htmlIn other words, it is the underwater equivalent to topography. The ocean’s floor is as complex as it is deep: huge trenches, walls, flatlands and seamounts fill the seascape and have a direct impact on the water bodies above them. By conducting a multibeam sonar survey similar to a medical ultrasound, scientists are able to image the sea-bottom.schmidtocean.org/technology/seafloor-mapping/
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