HR: 09:00h
AN: C31A-05    [PDF]
TI: Atmospheric and Surface Reflectance Measurements by the Geoscience Laser Altimeter System
AU: * Spinhirne, J D
EM: James.Spinhirne@nasa.gov
AF: NASA Goddard Space Flight Center, Laboratory for Atmospheres/912, Greenbelt, MD 20771 United States
AU: Palm, S P
EM: spp@virl.gsfc.nasa.gov
AF: Science System Applications Inc, GSFC Code 912, Greenbelt, MD 20771 United States
AU: Hlavka, D L
EM: sgdlh@virl.gsfc.nasa.gov
AF: Science System Applications Inc, GSFC Code 912, Greenbelt, MD 20771 United States
AU: Hart, W D
EM: billhart@virl.gsfc.nasa.gov
AF: Science System Applications Inc, GSFC Code 912, Greenbelt, MD 20771 United States
AU: Mahesh, A
EM: Mahesh@agnes.gsfc.nasa.gov
AF: University of Maryland Baltimore Campus, GSFC Code 912, Greenbelt, MD 20771 United States
AU: Welton, E J
EM: judd.welton@nasa.gov
AF: NASA Goddard Space Flight Center, Laboratory for Atmospheres/912, Greenbelt, MD 20771 United States
AB: The Geoscience Laser Altimeter System launched in early 2003 is the first satellite instrument in space to globally observe the distribution of clouds and aerosol through laser remote sensing. The instrument is a basic backscatter lidar that operates at two wavelengths, 532 and 1064 nm. The mission data products for atmospheric observations include the calibrated, observed, attenuated backscatter cross section for cloud and aerosol; height detection for multiple cloud layers; planetary boundary layer height; cirrus and aerosol optical depth and the height distribution of aerosol and cloud scattering cross section profiles. The data will enhance knowledge in several areas of atmospheric science: the distribution, transport and influence of atmospheric aerosol, significantly more accurate measurements of the coverage and height of cirrus and other clouds, polar cloud climatology and radiation influence, the dynamics planetary boundary layer and others. An overview and summary of initial results are presented. Initial results from the first months of operation show the detailed height structure of clouds and aerosol on a global basis as expected. The 532 nm channel was expected to be the more sensitive and primary channel for aerosol measurements, but extensive aerosol loading in many regions are observed by the 1064 nm channel. Sensitivities are down to a few times 10-6 1/(m-sr), much better than originally expected. The 532 channel adds an order of magnitude addition sensitivity. Initial comparisons to aerosol models have been done. Similarly for global cloud cover, good results are obtained just from the 1064 nm signal and from both channels, a measurement of multiple layers and cloud overlap has been made. Antarctica observations show high levels of total cloud cover including unique low-level cirrus and blowing snow. Data products have been generated for cloud, aerosol and PBL presence and heights in addition to the basic scattering cross section profiles. The received reflected energy of the laser pulse from the surface has applications to characterize atmospheric parameters. The surface pulse reflectance is a function of the atmospheric transmission and the surface properties. The calibration of the surface reflectance and atmospheric transmission retrievals has been analyzed through surface based intercomparison measurements. Pulse reflectance over oceans has been related to wind speed with results that are in agreement with predicted values. Multiple scattering of photons is an important factor for the effective atmospheric transmission, especially for transmissive clouds, and analysis of surface signals provide a test of model generated corrections. Stretching of pulses due to cloud and aerosol scatting is also an important factor for the accuracy of the surface altimetry and the clearing and correction of scattering errors has been initially evaluated.
UR: http://virl.gsfc.nasa.gov
DE: 0300 ATMOSPHERIC COMPOSITION AND STRUCTURE
DE: 0305 Aerosols and particles (0345, 4801)
DE: 0320 Cloud physics and chemistry
DE: 0360 Transmission and scattering of radiation
DE: 0394 Instruments and techniques
SC: Cryosphere [C]
MN: 2003 Fall Meeting