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CEOS EO HANDBOOK – MEASUREMENTS
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Aerosols


Aerosols are tiny particles suspended in the air, with the majority derived from natural phenomena such as volcanic eruptions, thought it is estimated that some 10–20% are generated by human activities such as burning of fossil fuels. The majority of aerosols form a thin haze in the lower atmosphere and are regularly washed out by precipitation, with the remainder found in the stratosphere where they can remain for many months or years.
Detailed MeasurementDescription*InstrumentsTimeline
Aerosol absorption optical depth (column/profile)Optical depth (OD) is the integral of extinction in the vertical dimension (integral of extinction (km-1) dz). The transmittance of the atmosphere = T = Exp(-OD) = Exp(-Integral(extinction dz)).19 instruments
Aerosol effective radius (column/profile)Vertical profile of the size distribution of aerosol, assimilated to spheres of the same volume. Requested in the troposphere (assumed height: 12 km) and as columnar average - Physical unit: [ mm ] - Accuracy unit: [ mm ].9 instruments
Aerosol Extinction / Backscatter (column/profile)A measure of radiation extinction at the encounter of aerosol particles in the atmosphere.24 instruments
Aerosol layer height-0 instruments
Aerosol optical depth (column/profile)The aerosol optical depth or optical thickness (τ) is defined as the integrated extinction coefficient over a vertical column of unit cross section.35 instruments
Aerosol single scattering albedo-0 instruments
VisibilityThe aerosol optical depth or optical thickness (τ) is defined as the integrated extinction coefficient over a vertical column of unit cross section.1 instrument
Volcanic ashThe location of a volcanic ash cloud. [Unit of measurement – Lat/Long]8 instruments
* Description adapted from WMO.
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