Concept
effective_radius_of_stratiform_cloud_graupel_particles
| URI | http://vocab.nerc.ac.uk/collection/P07/current/WSOOVDAH/ | ||
|---|---|---|---|
| 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 | 2019-05-14T17:27:19 | ||
| Identifier | SDN:P07::WSOOVDAH | ||
| Note | accepted | ||
| Has Current Version | 1 | ||
| version | 1 | ||
| Same As | P07:CF12N199 |
effective_radius_of_stratiform_cloud_graupel_particle | Mapping: 1590417 |
| MMI | http://mmisw.org/ont/cf/parameter/effective_radius_of_stratiform_cloud_graupel_particles | Mapping: 341223 | |
| CF | http://vocab.nerc.ac.uk/standard_name/effective_radius_of_stratiform_cloud_graupel_particles/ | Mapping: 379275 | |
| Related | P06:ULAA |
Metres | Mapping: 1590416 |
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