ConceptDEPRECATED
effective_radius_of_stratiform_cloud_liquid_water_particle
| URI | http://vocab.nerc.ac.uk/collection/P07/current/CF12N201/2/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| Alternative Labels | |||
| 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). | ||
| Date | 2019-05-14T17:27:21 | ||
| Identifier | SDN:P07::CF12N201 | ||
| Note | deprecated | ||
| Is Version Of | CF12N201 | ||
| Previous Version | 1 | ||
| version | 2 | ||
| Same As | P07:VVZRYOE6 |
effective_radius_of_stratiform_cloud_liquid_water_particles | |
| MMI | http://mmisw.org/ont/cf/parameter/effective_radius_of_stratiform_cloud_liquid_water_particle | ||
| CF | http://vocab.nerc.ac.uk/standard_name/effective_radius_of_stratiform_cloud_liquid_water_particle/ | ||
| Broader | P02:ATPC |
Atmospheric particulates | |
P04:G269 |
EARTH SCIENCE > Atmosphere > Clouds > Cloud Liquid Water/Ice | ||
P64:G269 |
EARTH SCIENCE > Atmosphere > Clouds > Cloud Liquid Water/Ice | ||
| Related | P06:ULAA |
Metres | |
Alternate Formats
Other formats for this page:
RDF/XML Turtle JSON-LDAlternate Profiles
Other views of this page:
Alternate Profiles ?Different Media Types (HTML, text, RDF, JSON etc.) and different information model views, profiles, are available for this resource.
NVS html view ? Default NVS html view.
