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Namespace Prefixes

PrefixIRI
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n2http://vocab.nerc.ac.uk/collection/P07/current/CFV13N41/
n13http://mmisw.org/ont/cf/parameter/
n10http://vocab.nerc.ac.uk/standard_name/atmosphere_absorption_optical_thickness_due_to_sulfate_ambient_aerosol/

Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
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owl:sameAs
n10: n13:atmosphere_absorption_optical_thickness_due_to_sulfate_ambient_aerosol
skos:prefLabel
atmosphere_absorption_optical_thickness_due_to_sulfate_ambient_aerosol
dcterms:identifier
SDN:P07::CFV13N41
dc:identifier
SDN:P07::CFV13N41
dcterms:date
2015-01-07 15:23:08.0
skos:definition
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. A coordinate variable of radiation_wavelength or radiation_frequency can be specified to indicate that the optical thickness applies at specific wavelengths or frequencies. "Absorption optical thickness" means that part of the atmosphere optical thickness that is caused by the absorption of incident radiation. "Aerosol" means the suspended liquid or solid particles in air (except cloud droplets). "Ambient aerosol" is aerosol that has taken up ambient water through hygroscopic growth. The extent of hygroscopic growth depends on the relative humidity and the composition of the aerosol. 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.
skos:notation
SDN:P07::CFV13N41
skos:altLabel
owl:deprecated
true
skos:note
deprecated
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n11:
void:inDataset
n4:void
skos:related
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n5:authoredOn
2015-01-07 15:23:08.0
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n6:
n5:version
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