ConceptDEPRECATED
optical_thickness_of_atmosphere_layer_due_to_aerosol
| URI | http://vocab.nerc.ac.uk/collection/P07/current/CFSN0478/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| Definition | 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. 'Layer' means any layer with upper and lower boundaries that have constant values in some vertical coordinate. There must be a vertical coordinate variable indicating the extent of the layer(s). If the layers are model layers, the vertical coordinate can be model_level_number, but it is recommended to specify a physical coordinate (in a scalar or auxiliary coordinate variable) as well. The optical thickness is the integral along the path of radiation of a volume scattering/absorption/attenuation coefficient. The radiative flux is reduced by a factor exp(-optical_thickness) on traversing the path. 'Aerosol' means the suspended liquid or solid particles in air (except cloud droplets). | ||
| Date | 2010-03-11T13:08:04 | ||
| Identifier | SDN:P07::CFSN0478 | ||
| Note | deprecated | ||
| Has Current Version | 1 | ||
| isReplacedBy | optical_thickness_of_atmosphere_layer_due_to_ambient_aerosol_particles | ||
| version | 1 | ||
| Same As | P07:CFV13A5 |
optical_thickness_of_atmosphere_layer_due_to_ambient_aerosol | Mapping: 170876 |
| MMI | http://mmisw.org/ont/cf/parameter/optical_thickness_of_atmosphere_layer_due_to_aerosol | Mapping: 260611 | |
| CF | http://vocab.nerc.ac.uk/standard_name/optical_thickness_of_atmosphere_layer_due_to_aerosol/ | Mapping: 381704 | |
| Broader | |||
| P04 Global Change Master Directory Science Keywords V5 - (2) | |||
| P64 Global Change Master Directory Science Keywords V6 - (2) | |||
| Related | P06:UUUU |
Dimensionless | Mapping: 161474 |
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