1993•Proceedings of SPIE, the International Society for Optical Engineering/Proceedings of SPIERequires access

Bispectral and brightness temperature difference analysis of 1991 FIRE cirrus IFO satellite data

Eric O. Schmidt, Robert F. Arduini, Bruce A. Wielicki, Bryan A. Baum

Open publisher page 0 citations

Abstract

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.

About this research paper

What this paper is about

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.

Why it matters

A significance statement is not available in the OpenAlex record.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

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.

Key concepts: Cirrus, Radiosonde, Lidar, Brightness temperature, Radiative transfer, Remote sensing, Environmental science, Advanced very-high-resolution radiometer

Related papers

Back to paper searchBrowse research topicsOriginal source
Bispectral and brightness temperature difference analysis of 1991 FIRE cirrus IFO satellite data — Research Paper | ScholarLens