Although the MWRP is currently deployed at the ARM Southern Great Plains (SGP) central facility near Lamont, OK, it has also been successfully operated at the ARM North Slope of Alaska (NSA) facility at Barrow, AK. Since its initial deployment at SGP significant biases between measured and modeled brightness temperatures in the five channels between 22-30 GHz have been observed. These brightness temperature biases resulted in significant biases in the retrieved profiles of water vapor and temperature and also adversely affected the vertical resolution. In this paper the brightness temperature biases are eliminated by substituting the air-broadened half width of the 22.235 GHz water vapor line from the HITRAN compilation (Rothman et al., 1992) for the Rosenkranz (1998) half width in the model calculations. An a priori statistical retrieval based on the revised model is shown to yield significant improvements in the accuracy and vertical resolution of the retrieved temperature and water vapor profiles. Additional improvements are then demonstrated by combining the MWRP retrievals with those from the GOES-8 sounder and Rapid Update Cycle (RUC) model.
This work was supported by the Environmental Sciences Division, U. S. Department of Energy, Office of Science, Office of Biological and Environmental Research, under contract W-31-109-Eng-38, as part of the Atmospheric Radiation Measurement Program. Argonne National Laboratory is operated by the University of Chicago for the U. S. Department of Energy.
Supplementary URL: