SBIR-STTR Award

Remote sensing of global cirrus clouds using satellite data
Award last edited on: 9/10/02

Sponsored Program
SBIR
Awarding Agency
DOD : AF
Total Award Amount
$542,099
Award Phase
2
Solicitation Topic Code
-----

Principal Investigator
Dr Liou

Company Information

Liou & Associates

4480 Adonis Drive
Salt Lake City, UT 84124
   (801) 581-3336
   N/A
   N/A
Location: Single
Congr. District: 04
County: Salt Lake

Phase I

Contract Number: ----------
Start Date: 00/00/00    Completed: 00/00/00
Phase I year
1990
Phase I Amount
$46,500
The objective of the proposed study in Phase I is to develop a novel and comprehensive algorithm for the retrieval of the compositions and structure of cirrus clouds using data gathered from orbiting meteorological satellites. In the proposed program, the temperature, emissivity and fractional cover of cirrus clouds are first determined from NOAA-AVHRR and DMSP-OLS radiance data. Once the cirrus cloud temperature is known, the mean ice crystal size distribution and ice water content may be determined through parameterized equations derived from aircraft cloud microphysical data. Subsequently, the scattering and absorption properties of ice crystals for the wavelengths of scientific and technological interest can be computed from light scattering programs. Finally, using the scattering and absorption properties of ice crystals, simulation of the radiation attenuation for a target-sensor system associated with the military electro-optics requirement may be carried out.

Phase II

Contract Number: ----------
Start Date: 00/00/00    Completed: 00/00/00
Phase II year
1991
Phase II Amount
$495,599
The objective of the proposed study in Phase II is to develop a novel, logical and coherent algorithm which will provide the specialized cloud information required for an accurate assessment of radiance degradation under typical cirrus cloud conditions, using data gathered from satellites. The proposed program includes (1) synthetic analyses for the retrieval of temperature, emissivity and fractional cover of cirrus clouds from NOAA AVHRR channels based on the theory of radiative transfer, (2) removal of 3.7 micrometer solar radiances during daytime based on 0.63 micrometer channel radiances and radiative transfer parameterizations, (3) application and verification of the cirrus retrieval algorithm to selected AVHRR data, and (4) preparation of computer software for the cirrus retrieval algorithm and ice crystal extinction program. Once the cirrus cloud temperature is retrieved, mean ice crystal size distribution can be computed from the light-scattering programs developed for hexagonal particles. It is anticipated that the end-product of Phase II will be a module in equation forms and in appropriate computer codes for spectral cirrus cloud extinction, using the cirrusparameters inferred from an effective satellite retrieval algorithm.