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PREFERRED TERM

UV AEROSOL INDEX  

DEFINITION

  • The relatively simple calculation of the Aerosol Index is based on wavelength dependent changes in Rayleigh scattering in the UV spectral range where ozone absorption is very small. UVAI can also be calculated in the presence of clouds so that daily, global coverage is possible. This is ideal for tracking the evolution of episodic aerosol plumes from dust outbreaks, volcanic ash, and biomass burning.

CHANGE NOTE

  • 2020-06-19 13:45:30.0 [mmorahan] Insert Concept add broader relation (UV AEROSOL INDEX [8d7e5d36-4d81-469d-9318-bf20ba3bae5c,560390] - AEROSOL OPTICAL DEPTH/THICKNESS [61c3b720-abc8-4430-866c-f1da35d2cd0b,552595]);
  • 2020-06-19 13:47:47.0 [mmorahan] insert Definition (id: null text: The relatively simple calculation of the Aerosol Index is based on wavelength dependent changes in Rayleigh scattering in the UV spectral range where ozone absorption is very small. UVAI can also be calculated in the presence of clouds so that daily, global coverage is possible. This is ideal for tracking the evolution of episodic aerosol plumes from dust outbreaks, volcanic ash, and biomass burning. language code: en);

URI

https://gcmd.earthdata.nasa.gov/kms/concept/8d7e5d36-4d81-469d-9318-bf20ba3bae5c

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