Inversion for physical characteristics of snow using passive radiometric observations.

S. R. Rotman; A. D. Fisher; D. H. Staelin

doi:10.1017/S0022143000011886

Inversion for physical characteristics of snow using passive radiometric observations.

S. R. Rotman, A. D. Fisher, D. H. Staelin

Research output: Contribution to journal › Article › peer-review

4 Scopus citations

Abstract

The Nimbus-6 Satellite's Scanning Microwave Spectrometer (SCAMS) mapped the terrestrial surface continuously for 11 months at 22.2 and 31.6GHz. A semi-empirical method was devised to process these observations of Greenland and Antarctica and to infer long-term snow accumulation rates; comparison with in situ data suggests the method is generally successful except in certain locations where re- melting is more likely.-Authors

Original language	English
Pages (from-to)	179-185
Number of pages	7
Journal	Journal of Glaciology
Volume	28
Issue number	98
DOIs	https://doi.org/10.1017/S0022143000011886
State	Published - 1 Jan 1982
Externally published	Yes

ASJC Scopus subject areas

Earth-Surface Processes

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10.1017/S0022143000011886

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title = "Inversion for physical characteristics of snow using passive radiometric observations.",

abstract = "The Nimbus-6 Satellite's Scanning Microwave Spectrometer (SCAMS) mapped the terrestrial surface continuously for 11 months at 22.2 and 31.6GHz. A semi-empirical method was devised to process these observations of Greenland and Antarctica and to infer long-term snow accumulation rates; comparison with in situ data suggests the method is generally successful except in certain locations where re- melting is more likely.-Authors",

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AU - Fisher, A. D.

AU - Staelin, D. H.

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N2 - The Nimbus-6 Satellite's Scanning Microwave Spectrometer (SCAMS) mapped the terrestrial surface continuously for 11 months at 22.2 and 31.6GHz. A semi-empirical method was devised to process these observations of Greenland and Antarctica and to infer long-term snow accumulation rates; comparison with in situ data suggests the method is generally successful except in certain locations where re- melting is more likely.-Authors

AB - The Nimbus-6 Satellite's Scanning Microwave Spectrometer (SCAMS) mapped the terrestrial surface continuously for 11 months at 22.2 and 31.6GHz. A semi-empirical method was devised to process these observations of Greenland and Antarctica and to infer long-term snow accumulation rates; comparison with in situ data suggests the method is generally successful except in certain locations where re- melting is more likely.-Authors

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ER -

Inversion for physical characteristics of snow using passive radiometric observations.

Abstract

ASJC Scopus subject areas

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