This HTML5 document contains 20 embedded RDF statements represented using HTML+Microdata notation.

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Namespace Prefixes

Prefix	IRI
dcterms	http://purl.org/dc/terms/
n2	http://vocab.nerc.ac.uk/collection/P07/current/N3D94CVE/
n7	http://vocab.nerc.ac.uk/collection/P07/current/CF12N196/
n9	http://vocab.nerc.ac.uk/collection/P06/current/ULAA/
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n11	http://vocab.nerc.ac.uk/.well-known/
owl	http://www.w3.org/2002/07/owl#
n14	http://vocab.nerc.ac.uk/standard_name/effective_radius_of_convective_cloud_liquid_water_particles/
xsdh	http://www.w3.org/2001/XMLSchema#
n8	http://purl.org/pav/
n13	http://vocab.nerc.ac.uk/collection/P07/current/N3D94CVE/1/
n6	http://mmisw.org/ont/cf/parameter/
n15	http://vocab.nerc.ac.uk/collection/P07/current/N3D94CVE/2/

Statements

Subject Item

n2:

rdf:type

skos:Concept

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n6:effective_radius_of_convective_cloud_liquid_water_particles n7: n14:

skos:prefLabel

effective_radius_of_convective_cloud_liquid_water_particles

dcterms:identifier

SDN:P07::N3D94CVE

dc:identifier

SDN:P07::N3D94CVE

dcterms:date

2020-03-09 15:56:08.0

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. Convective cloud is that produced by the convection schemes in an atmosphere model. "Cloud liquid water" refers to the liquid phase of cloud water. A diameter of 0.2 mm has been suggested as an upper limit to the size of drops that shall be regarded as cloud drops; larger drops fall rapidly enough so that only very strong updrafts can sustain them. Any such division is somewhat arbitrary, and active cumulus clouds sometimes contain cloud drops much larger than this. Reference: AMS Glossary http://glossary.ametsoc.org/wiki/Cloud_drop.

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SDN:P07::N3D94CVE

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false

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2020-03-09 15:56:08.0

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