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- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c 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." @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c id "1663259" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_id 1eb0ea0a-312c-4d74-8d42-6f1ad758f999 @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_id 2e5a401b-1507-4f57-82b8-36557c13b154 @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_id 61c3b720-abc8-4430-866c-f1da35d2cd0b @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_id c47f6052-634e-40ef-a5ac-13f69f6f4c2a @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_id e9f67a66-e9fc-435c-b720-ae32a2c3d8f5 @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_label "AEROSOL OPTICAL DEPTH/THICKNESS" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_label "AEROSOLS" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_label "ATMOSPHERE" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_label "EARTH SCIENCE" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c path_label "Science Keywords" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c prefLabel "UV AEROSOL INDEX" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c reference "http://www.tropomi.eu/data-products/uv-aerosol-index" @default.
- 8d7e5d36-4d81-469d-9318-bf20ba3bae5c tag "Science Keywords" @default.