2008
DOI: 10.5194/acpd-8-2771-2008
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Sea surface wind speed estimation from space-based lidar measurements

Abstract: Abstract. Global satellite observations of lidar backscatter measurements acquired by the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation (CALIPSO) mission and collocated sea surface wind speed data from the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E), are used to investigate the relation between wind driven wave slope variance and sea surface wind speed. The new slope variance – wind speed relation established from this study is similar to the linear relati… Show more

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Cited by 21 publications
(30 citation statements)
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“…Thus, surface losses can generally be neglected, although the surface return can be quite large. 13,28,29 Neglecting the effects of multiple scattering, the depth-dependent lidar signal can be described by the lidar equation.…”
Section: Basic Characteristicsmentioning
confidence: 99%
See 1 more Smart Citation
“…Thus, surface losses can generally be neglected, although the surface return can be quite large. 13,28,29 Neglecting the effects of multiple scattering, the depth-dependent lidar signal can be described by the lidar equation.…”
Section: Basic Characteristicsmentioning
confidence: 99%
“…This excludes some very successful applications that include underwater target detection and identification, [5][6][7] bathymetry, 8,9 laser-induced fluorescence, [10][11][12] and surfaceroughness measurements. [13][14][15] Information about these applications can be found in the cited references.…”
Section: Introductionmentioning
confidence: 99%
“…The ocean surface reflectance depends on the (10-m height) surface wind speed. The Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) mission provides by far the largest study of lidar backscatter from the ocean surface, and we rely on data from Hu et al (2008) for determination of the surface directional reflectance (backscatter) over this region of the Pacific Ocean. We are able to take advantage of the fact that at the JPL LAS nominal 58 off-nadir angle, the surface backscatter is only weakly dependent on surface wind speed in the range from ;(2.5-12) m s 21 (see Menzies et al 1998, their Figs.…”
Section: Spectral Reflectances Of Surface Materials and Abovegrounmentioning
confidence: 99%
“…Figure 9 shows model results from a TMFL instrument for various wind speeds taken at 2000 ft above water level. The model 19 predicts the relationship between the variance of the slope of the wind-driven waves and surface wind speed. Such studies have shown good agreement using CALIPSO lidar data.…”
Section: Water Surfacementioning
confidence: 99%
“…For example, the lidar return profile can be correlated with water surface roughness which in turn can be used to derive wind speeds 19 . When the laser footprint is small, very high spatial resolution wind maps can be measured.…”
Section: Introductionmentioning
confidence: 99%