Laser methods for the atmospheric correction of marine radiance data sensed from a satellite

Satellite remote sensing of sea color is a powerful instrument to perform oceanic studies. Unfortunately, the present data processing algorithms are not exempt from uncertainties, especially because the marine radiance must be separated from the atmospheric contributions, which typically represent about 80% of the total. In this paper we suggest the development of observation methods based on the optical radar or lidar. In fact, the numerical simulation of a sea-level optical radar demonstrates that, if applied to restricted areas, such system is a precise and versatile tool for the atmospheric correction of marine radiance data sensed from satellite (accuracy better than 10% for typical conditions). Moreover, the lidar is effective even in environments that would be severe for the standard corrective schemes. Finally, the feasibility of a spaceborne system is discussed.

[1]  H. Gordon,et al.  Removal of atmospheric effects from satellite imagery of the oceans. , 1978, Applied optics.

[2]  S. Hooker An overview of SeaWiFS and ocean color , 1992 .

[3]  Philip B. Russell,et al.  Lidar measurement of particles and gases by elastic backscattering and differential absorption , 1976 .

[4]  Luca Fiorani,et al.  A combined determination of wind velocities and ozone concentrations for a first measurement of ozone fluxes with a DIAL instrument during the MEDCAPHOT-TRACE campaign , 1998 .

[5]  J. Fischer,et al.  Sun-stimulated chlorophyll fluorescence 1: Influence of oceanic properties , 1990 .

[6]  V. Derr,et al.  A comparison of remote sensing of the clear atmosphere by optical, radio, and acoustic radar techniques. , 1970, Applied optics.

[7]  W. Munk,et al.  Measurement of the Roughness of the Sea Surface from Photographs of the Sun’s Glitter , 1954 .

[8]  R. Collis,et al.  Lidar: A new atmospheric probe , 1966 .

[9]  R. J. Lataitis,et al.  Ground-based remote profiling in atmospheric studies: an overview , 1994, Proc. IEEE.

[10]  David M. Winker,et al.  An overview of LITE: NASA's Lidar In-space Technology Experiment , 1996, Proc. IEEE.

[11]  J. Klett Stable analytical inversion solution for processing lidar returns. , 1981, Applied optics.

[12]  J. W. Brown,et al.  Phytoplankton pigment concentrations in the Middle Atlantic Bight: comparison of ship determinations and CZCS estimates. , 1983, Applied optics.

[13]  Construction of a Multi-wavelength Lidar System for Satellite Data Atmospheric Correction , 1997 .

[14]  Jacques Pelon,et al.  Ozone monitoring in the troposphere and lower stratosphere: Evaluation and operation of a ground-based lidar station , 1982 .

[15]  S. Mukai Atmospheric correction of remote sensing images of the ocean based on multiple scattering calculations , 1990, IEEE Transactions on Geoscience and Remote Sensing.

[16]  K. Baker,et al.  Ship and Satellite Bio-Optical Research in the California Bight , 1981 .

[17]  A. Morel,et al.  Atmospheric corrections and interpretation of marine radiances in czcs imagery, revisited , 1991 .

[18]  H. Gordon,et al.  Clear water radiances for atmospheric correction of coastal zone color scanner imagery. , 1981, Applied optics.

[19]  Valentin Mitev,et al.  Development of a pseudorandom noise modulation, continuous-wave (PRN-cw) total backscatter lidar , 1995, Other Conferences.

[20]  T. D. Allan The marine environment , 1992 .

[21]  F. G. Fernald Analysis of atmospheric lidar observations: some comments. , 1984, Applied optics.

[22]  Howard R. Gordon,et al.  Remote Assessment of Ocean Color for Interpretation of Satellite Visible Imagery , 1983, Lecture Notes on Coastal and Estuarine Studies.

[23]  B. Calpini,et al.  Tropospheric ozone measurements over the Great Athens Area during the medcaphot-trace campaign with a new shot-per-shot dial instrument: experimental system and results , 1998 .