| 1. | The difference between the ocean surface and the actual geoid gives ocean surface topography.
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| 2. | The surface topography is commonly displayed as a pseudocolor plot.
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| 3. | The van der Waals force of adhesion is also dependent on the surface topography.
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| 4. | Additionally, the incident angle and the scattered angle help determine the sample surface topography.
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| 5. | The permanent deviation between the geoid and mean sea level is called ocean surface topography.
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| 6. | Ocean surface topography can be derived from ship-going measurements of temperature and salinity at depth.
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| 7. | These included sea surface topography, sea surface temperature, atmospheric water vapor, and ocean surface imaging.
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| 8. | In this situation, the feedback output equals the sample surface topography to within a small error.
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| 9. | Beyond the effects of convectively driven motion, deep processes have other influences on the surface topography.
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| 10. | Ocean surface topography is caused by ocean waves, tides, currents, and the loading of atmospheric pressure.
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