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Entry: Aerosol optical depth, TSP

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URI: http://codes.wmo.int/wmdr/ObservedVariableAtmosphere/325    

The AOD is the effective depth of the aerosol over a specified distance, from the viewpoint of radiation propagation: Vertical integral of spectral aerosol extinction coefficient AOD = exp(-K. Δz) where K is the extinction coefficient [km-1 ] and Δz the vertical path [km].

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is a Concept
changed on 4 Nov 2021 10:19:00.600
submitted bykurt-hectic
accepted on 29 Apr 2020 14:25:47.527 | 29 Apr 2020 14:26:24.504

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date accepted 29 Apr 2020 14:25:47.527 | 29 Apr 2020 14:26:24.504
date submitted 21 Oct 2019 09:47:40.016
definition
entity Aerosol optical depth, TSP
source graph graph

description The AOD is the effective depth of the aerosol over a specified distance, from the viewpoint of radiation propagation: Vertical integral of spectral aerosol extinction coefficient AOD = exp(-K. Δz) where K is the extinction coefficient [km-1 ] and Δz the vertical path [km].
item class Concept
label Aerosol optical depth, TSP
modified 4 Nov 2021 10:19:00.600
notation 325
register observed variable atmosphere
status status stable
submitter
account name https://api.github.com/users/kurt-hectic
name kurt-hectic

type register item
version info 4
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Definition

description The AOD is the effective depth of the aerosol over a specified distance, from the viewpoint of radiation propagation: Vertical integral of spectral aerosol extinction coefficient AOD = exp(-K. Δz) where K is the extinction coefficient [km-1 ] and Δz the vertical path [km].
label Aerosol optical depth, TSP
notation 325
type Concept