Observations of particle size distributions of single crystal and aggregate frozen hydrometeors
Currently, Greenland ice sheet mass loss is increasing at a rate near 1000 Gt yr-1, making the ice sheets top contributors to current sea level rise. Errors in constraining the mass balance of the Antarctic and Greenland ice sheets are primarily from measurement of frozen precipitation. In this stud...
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Language: | en |
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VANDERBILT
2015
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Online Access: | http://etd.library.vanderbilt.edu/available/etd-07172015-130214/ |