An empirical technique for estimating near-surface air temperature trends in central Greenland from SSM/I brightness temperatures
In central Greenland, near-surface air temperatures can be estimated from long-term satellite passive microwave brightness temperatures supported by limited air-temperature data from automatic weather stations. In this region, brightness temperature depends on snow emissivity, which varies slowly ov...
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Veröffentlicht in: | Remote Sensing of Environment 1995-02, Vol.51 (2), p.245-252 |
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