A plea for radar brightness

Geoscience and Remote Sensing Symposium, 1994. IGARSS '94. Surface and Atmospheric Remote Sensing: Technologies, Data Analysis and Interpretation., International(1994)

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摘要
The radar reflectivity coefficient of a distributed scatterer, expressed either as σ0 or γ, depends on local incidence angle. Prior to incidence angle projection, the reflectivity coefficient may be called "radar brightness", denoted by "beta nought" β0. In most practical situations, the local incidence angle is not known, so the image radiometrics cannot be corrected for it. It follows that β0 is almost always the more appropriate radiometric attribute of radar imagery, whether calibrated or uncalibrated It is recommended that σ0 (or γ) be reserved for situations in which both the local terrain slope and the illumination incidence angles are known, and the image file has been adjusted to take both angles into account. Otherwise, radar brightness is correct, which should be adopted as the standard both as concept and as working terminology. This has been endorsed by the CEOS SAR Calibration Working Group.
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关键词
geophysical techniques,radar applications,radar cross-sections,radar imaging,radar theory,remote sensing by radar,synthetic aperture radar,SAR,calibration,distributed scatterer,geophysical measurement technique,land surface terrain mapping,local incidence angle,radar brightness,radar imagery,radar imaging,radar reflectivity coefficient,radar remote sensing,radar scattering theory,radiometric attribute,synthetic aperture radar
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