Backscatter

From Glossary of Meteorology

Hemispheric backscatter (also referred to as backscattering or backward scatter) is the scattering of radiant energy into the hemisphere of space bounded by a plane normal to the direction of the incident radiation and lying on the same side as the incident ray; the opposite of forward scatter. Atmospheric backscattering depends greatly on wavelength and polarization considered, as well as atmospheric composition, including the presence of aerosols, clouds, and precipitation.

In radar and lidar usage, backscatter refers only to that radiation scattered at 180° to the direction of the incident wave; the units of the backscatter coefficient, that is, the physical quantity used to describe the backscattering process, are m−1 sr−1 (per meter and steradian).



Term edited 15 June 2019.

Copyright 2024 American Meteorological Society (AMS). For permission to reuse any portion of this work, please contact permissions@ametsoc.org. Any use of material in this work that is determined to be “fair use” under Section 107 of the U.S. Copyright Act (17 U.S. Code § 107) or that satisfies the conditions specified in Section 108 of the U.S.Copyright Act (17 USC § 108) does not require AMS’s permission. Republication, systematic reproduction, posting in electronic form, such as on a website or in a searchable database, or other uses of this material, except as exempted by the above statement, require written permission or a license from AMS. Additional details are provided in the AMS Copyright Policy statement.