1993
DOI: 10.1117/12.152595
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<title>Advanced microwave precipitation radiometer (AMPR): improved calibration and data collection</title>

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“…Instead of directly measuring updraft strength for thunderstorms across the globe, we might infer updraft characteristics by measuring a quantity related to the amount of ice within the clouds that is lofted by the updraft. For example, passive microwave imagers (Draper et al., 2015; Hollinger et al., 1990; James et al., 1993; Kummerow et al., 1998) sense the amount of upwelling microwave radiation that escapes the atmosphere to space. Ice particles are efficient scatterers of microwave radiation at higher frequencies (i.e., 85 GHz), resulting in depressed brightness temperatures relative to clear air.…”
Section: Introductionmentioning
confidence: 99%
“…Instead of directly measuring updraft strength for thunderstorms across the globe, we might infer updraft characteristics by measuring a quantity related to the amount of ice within the clouds that is lofted by the updraft. For example, passive microwave imagers (Draper et al., 2015; Hollinger et al., 1990; James et al., 1993; Kummerow et al., 1998) sense the amount of upwelling microwave radiation that escapes the atmosphere to space. Ice particles are efficient scatterers of microwave radiation at higher frequencies (i.e., 85 GHz), resulting in depressed brightness temperatures relative to clear air.…”
Section: Introductionmentioning
confidence: 99%