CIMSS-NOAA Weekly Report
[ Archive ] |
IN THE PRESS:
ITEMS FOR THE ADMINISTRATOR:
ITEMS FOR THE ASSISTANT ADMINISTRATOR:
CRAS Forecast Images Compared to Observed GOES
Imagery: Imagery corresponding to that observed in the 11
micrometer infrared window can be simulated with forward model
radiative calculations for the atmospheric states forecast by the CIMSS
(Cooperative Institute for Meteorological Satellite Studies) Regional
Assimilation System (CRAS). The CRAS forecasts are run at 00 and
12 UTC and assimilate cloud top pressure and three layers of
precipitable water retrieved from Geostationary Operational
Environmental Satellite (GOES) Sounder measurements. Daily image
examples over the north central U.S., comparing the GOES observations
with the CRAS 20 km resolution forecasts, varying here from 6 to 18
hours in duration, are available on the web at http://cimss.ssec.wisc.edu/goes/realtime/cf/.
Features and patterns generally match well, although some work in
radiative and cloud physics modeling is needed to help reduce excessive
CRAS cloud amounts at the colder ranges. (G.S. Wade, E/RA2,
608-263-4743, R.M. Aune E/RA2, 608-262-1071)
ITEMS FOR THE DIVISION CHIEF, ARAD
Seminar Given on Satellite Derived Multi-layer Cloud Distributions: A Heidinger presented results of the application of new multi-layer detection algorithm to data from NOAA's Advanced Very High Resolution Radiometer at a seminar given to the University of Wisconsin Atmospheric and Oceanic Sciences Department. The results present the first global look of the occurrence of multi-layer cloud derived from a satellite. Versions of the algorithm are also applicable to instruments on the geostationary satellites including the Advanced Baseline Imager. (A. Heidinger, E/RA2, 608-263-6757)
GOES-R Advanced Baseline Imager Mock Spectral Response Functions Now Available: The Geostationary Operational Environmental Satellite (GOES)-R Advanced Baseline Imager (ABI) is planned to have 16 bands, 6 in the visible/near-infrared, and 10 in the infrared. Researchers at the Cooperative Institute for Meteorological Satellite Studies (CIMSS) have simulated spectral response functions for the planned ABI bands and made them available to the rest of the GOES user community for experimentation. They can be used in fast forward models such as Optical Path Transmittance (OPTRAN) or Pressure Layered Optical Depth (PLOD) to simulate radiances from atmospheric profiles or to be convolved with high spectral resolution data such as Atmospheric Infrared Sounder (AIRS) data. The spectra response functions are available at ftp://ftp.ssec.wisc.edu/ABI/SRF. (M. Gunshor, CIMSS, 608-263-1146)