We attempt to bound microphysical properties of cirrus clouds via complementary satellite, rawinsonde, and lidar data analysis and radiative transfer modeling. Data acquired during the 1991 FIRE (First ISSCP Regional Experiment) Cirrus IFO (intensive field operation) includes AVHRR (advanced very high resolution radiometer) LAC (local area coverage), satellite imagery, high temporal resolution rawinsonde data, and lidar backscatter and depolarization information. We use the complementary rawinsonde and lidar data to generate profiles of the atmosphere, to place clouds at the correct height, and to verify the complex mixed phase nature of high altitude cirrus. Using the DISORT radiative transfer model (Stamnes et al., 1988), we generate brightness temperatures for a range of optical depths for single- and/or multi-level cloud systems composed of water or ice spheres or ice hexagons.
[1]
K. Liou,et al.
Solar Radiative Transfer in Cirrus Clouds. Part I: Single-Scattering and Optical Properties of Hexagonal Ice Crystals
,
1989
.
[2]
F. Bretherton,et al.
Cloud cover from high-resolution scanner data - Detecting and allowing for partially filled fields of view
,
1982
.
[3]
Bruce A. Wielicki,et al.
Cloud Retrieval Using Infrared Sounder Data: Error Analysis
,
1981
.
[4]
A. C. Dilley,et al.
Remote Sounding of High Clouds. Part VI: Optical Properties of Midlatitude and Tropical Cirrus
,
1987
.
[5]
Robert S. Stone,et al.
The Remote Sensing of Thin Cirrus Cloud Using Satellites, Lidar and Radiative Transfer Theory
,
1990
.