This HTML5 document contains 23 embedded RDF statements represented using HTML+Microdata notation.

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Namespace Prefixes

PrefixIRI
dctermshttp://purl.org/dc/terms/
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n14http://vocab.nerc.ac.uk/collection/P06/current/ULAA/
n9http://vocab.nerc.ac.uk/collection/P07/current/CF12N201/1/
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n2http://vocab.nerc.ac.uk/collection/P07/current/CF12N201/
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n16http://vocab.nerc.ac.uk/collection/P64/current/G269/
n12http://mmisw.org/ont/cf/parameter/

Statements

Subject Item
n2:
rdf:type
skos:Concept
owl:versionInfo
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owl:sameAs
n6: n10: n12:effective_radius_of_stratiform_cloud_liquid_water_particle
skos:broader
n11: n13: n16:
skos:prefLabel
effective_radius_of_stratiform_cloud_liquid_water_particle
dcterms:identifier
SDN:P07::CF12N201
dc:identifier
SDN:P07::CF12N201
dcterms:date
2019-05-14 17:27:21.0
skos:definition
The effective radius of a size distribution of particles, such as aerosols, cloud droplets or ice crystals, is the area weighted mean radius of particle size. It is calculated as the ratio of the third to the second moment of the particle size distribution. In an atmosphere model, stratiform cloud is that produced by large-scale convergence (not the convection schemes).
skos:notation
SDN:P07::CF12N201
skos:altLabel
owl:deprecated
true
skos:note
deprecated
void:inDataset
n18:void
skos:related
n14:
n5:authoredOn
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n9:
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