Concept
Effective radius of stratiform cloud liquid water particles
| URI | http://vocab.nerc.ac.uk/standard_name/effective_radius_of_stratiform_cloud_liquid_water_particles/ | ||
|---|---|---|---|
| Within Vocab | Climate and Forecast Standard Names | ||
| 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). "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. | ||
| Date | None | ||
| Note | accepted | ||
| modified | 2020-03-09 15:56:08.0 | ||
| Exact Match | http://mmisw.org/ont/cf/parameter/effective_radius_of_stratiform_cloud_liquid_water_particles | ||
| http://vocab.nerc.ac.uk/standard_name/effective_radius_of_stratiform_cloud_liquid_water_particles/ | |||
| P07 Climate and Forecast Standard Names - (2) | |||
| 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.
