ConceptDEPRECATED
Volume scattering coefficient in air due to dried aerosol particles
| URI | http://vocab.nerc.ac.uk/standard_name/volume_scattering_coefficient_in_air_due_to_dried_aerosol_particles/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Definition | The volume scattering/absorption/attenuation coefficient is the fractional change of radiative flux per unit path length due to the stated process. Coefficients with canonical units of m2 s-1 i.e. multiplied by density have standard names with "specific_" instead of "volume_". The scattering/absorption/attenuation coefficient is assumed to be an integral over all wavelengths unless a coordinate of "radiation_wavelength" or "radiation_frequency" is included to specify the wavelength. "Aerosol" means the system of suspended liquid or solid particles in air (except cloud droplets) and their carrier gas, the air itself. "Dried_aerosol" means that the aerosol sample has been dried from the ambient state before sizing, but that the dry state (relative humidity less than 40 per cent) has not necessarily been reached. To specify the relative humidity at which the sample was measured, provide a scalar coordinate variable with the standard name of "relative_humidity". The specification of a physical process by the phrase "due_to_" process means that the quantity named is a single term in a sum of terms which together compose the general quantity named by omitting the phrase. | ||
| Date | None | ||
| Note | deprecated | ||
| modified | 2018-05-15 09:59:17.0 | ||
| Exact Match | http://mmisw.org/ont/cf/parameter/volume_scattering_coefficient_in_air_due_to_dried_aerosol_particles | ||
| http://vocab.nerc.ac.uk/standard_name/volume_scattering_coefficient_in_air_due_to_dried_aerosol_particles/ | |||
| P07 Climate and Forecast Standard Names - (2) | |||
| Related | P06:UPRM |
per metre | |
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