Ocean Surface Salinity from Aircraft Microwave Radiometer and Radar Measurements
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Engineering topics
Publications and source records attributed to Yueh, S..
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Over the ocean, in situ observations in a hurricane are extremely sparse, and conventional satellite data provide only cloud imagery at the top of the storm.
A set of geophysical error sources for the microwave remote sensing of ocean surface salinity have been examined.
The feasibility of Quikscat for the measurements of tropical cyclone wind fields has been investigated with the data from seven hurricanes.
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A technique based on microwave passive polarimetry for the estimates of ionospheric Faraday rotation for microwave remote sensing of earth surfaces is described.
There has been a question on whether it is possible to measure the surface wind speeds of tropical cyclones with a spaceborne Ku-band scatterometer.
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Microwave radiometry and scatterometry are established techniques for surface remote sensing applications.
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This study shows that: 1) the NSCAT backscatter fields provide an estimate of the PIZ coverage of the Arctic Ocean; and, 2) the decrease in PIZ area over the winter gives an indication of the PIZ area exported through Fram Strait.
In this study we have examined techniques and technology options for achieving desired microwave system performance (high spatial resolution and accuracy) using low-mass deployable antennas.
It is necessary to know sea ice surface thermal states under cloud cover to evaluate cloud effects in the overall climatic feedback mechanisms in polar regions.
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NSCAT is the NASA Scatterometer to be launched on the Japanese ADEOS in 1996 for global ocean wind remote sensing.