Laser pulse reflectance of the ocean surface from the GLAS satellite lidar
The world's oceans can potentially be used as an extended target for achieving a radiometric calibration of space borne lidar if the reflective properties of the surface can be accurately predicted from available environmental data such as wind speed. To test current understanding of ocean refl...
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Published in | Geophysical research letters Vol. 32; no. 22; pp. L22S10 - n/a |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
American Geophysical Union
01.11.2005
Blackwell Publishing Ltd |
Subjects | |
Online Access | Get full text |
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Summary: | The world's oceans can potentially be used as an extended target for achieving a radiometric calibration of space borne lidar if the reflective properties of the surface can be accurately predicted from available environmental data such as wind speed. To test current understanding of ocean reflectance we compare surface pulse returns measured with the 1064 nm altimetry channel of the Geoscience Laser Altimeter System (GLAS) on the Ice, Cloud and land Elevation Satellite (ICESat) with the predictions of near‐IR reflectance from current ocean models. Measurements of wind speed retrieved from the SeaWinds database of the QuikSCAT satellite provide the model input. We find that while ocean models do not provide a full description of the nadir lidar observations this calibration technique yields a precision that exceeds that accomplished using White Sands as a target and that does not require the coordination that accompanies specialized calibration experiments. |
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Bibliography: | ArticleID:2005GL023732 Tab-delimited Table 1. istex:0FCEB8188BED7D436ABF38B989644406A8BEBC0F ark:/67375/WNG-DT94R74D-0 |
ISSN: | 0094-8276 1944-8007 |
DOI: | 10.1029/2005GL023732 |