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Concept information

This concept has been deprecated.

Preferred term

effective_radius_of_convective_cloud_ice_particle  

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.

Note

  • deprecated

URI

https://vocab.met.no/CFSTDN/effective_radius_of_convective_cloud_ice_particle

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