Assimilating GOES Brightness Temperatures
Selected Abstract
Assimilating GOES Brightness Temperatures. Part II: Assigning Water Vapor Wind Heights Directly from Weighting Functions
ABSTRACT An unsolved problem with water vapor wind estimates from the upper-tropospheric 6.7-m water vapor band on the Geostationary Operational Environmental Satellite (GOES) Imager (channel 3) is its exact placement in the vertical column. Satellite water vapor observations are known to be ... August 1, 2004; Journal of Applied Meteorology
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Assimilating GOES Brightness Temperatures. Part II: Assigning Water Vapor Wind Heights Directly from Weighting Functions
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Assimilating GOES Brightness Temperatures. Part I: Upper-Tropospheric Moisture
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