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- W2055706558 abstract "The propagation of radio waves broadcast to the Earth by a satellite is slowed by the total electron content (TEC) of the ionosphere. Spaceborne radar altimeters, like those aboard the Seasat and Geosat satellites, rely on the time delay between the transmission of a radar pulse and its reception, after reflection from the ocean surface, to estimate the range to the surface. The slowing of the electromagnetic waves by the ionosphere will increase the apparent distance between the satellite and the surface. Variations of the TEC of the ionosphere on horizontal spatial scales less than 300 km could potentially be confused for or mask the presence of sea surface height changes associated with mesoscale ocean circulation. Using dual‐frequency broadcasts from Global Positioning System (GPS) satellites, the spatial variability of the ionosphere is estimated. It is shown that for altimetric monitoring of mesoscale ocean circulation, ionospheric variability is not a significant problem. For altimetric studies of ocean circulation on ocean basin scales, compensation for ionospheric variability maybe necessary." @default.
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- W2055706558 date "1991-03-15" @default.
- W2055706558 modified "2023-09-27" @default.
- W2055706558 title "Ionospheric variability and the measurement of ocean mesoscale circulation with a spaceborne radar altimeter" @default.
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- W2055706558 doi "https://doi.org/10.1029/90jc02486" @default.
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