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- W2045708587 abstract "In contrast to many uses of multispectral data such as furnished by the satellites of the LANDSAT series, the exploitation of the thermal, and also albedo, data provided by the Heat Capacity Mapping Radiometer (HCMR) requires proper calibration relative to values measured on the ground. The reason for this apparent difference between multispectral and thermal data resides in the fact that the interpretation of thermal data requires an understanding of the physical processes responsible for a certain surface temperature or surface temperature difference (NASA, 1978) and, therefore, the temperatures or temperature differences both spatial and temporal as measured on the ground have to be known. The difference between the interpretation of MSS and thermal data is only apparent, because a deeper and deterministic analysis of MSS data encounters the same problems as that of thermal data. The interpretation of the multispectral data of the CZCS of theNIMBUS-7 satellite (Sturm, 1980) is an example of the development in this direction. Prior to the HCMM, the calibration of satellite thermal data, or more generally, its comparison with ground measured temperatures has mostly been carried out for sea water temperatures. A comparison between sea surface temperature (SST) measurements from the NOAA-4 satellite and from an underflight with an airborne radiometer was carried out in the Gulf of Lyon (Albuisson et al., 1979)." @default.
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- W2045708587 date "1986-01-01" @default.
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- W2045708587 title "HCMM satellite data calibration and atmospheric corrections" @default.
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- W2045708587 doi "https://doi.org/10.1080/02757258609532074" @default.
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