effective_radius_of_stratiform_cloud_rain_particles

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).
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  • Proposls with this term version:
  • Proposal: Martin Juckes [Some standard name updates to improve co]

    • Aliases for this term

    effective_radius_of_stratiform_cloud_rain_particle

    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).
  • List containing this term version: CF (12) CF (13) CF (14) CF (15) CF (16) CF (17) CF (18) CF (19) CF (20) CF (21) CF (25) CF (22) CF (27) CF (23) CF (24) CF (26) CF (28) CF (29) CF (30) CF (31) CF (32) CF (33) CF (34) CF (35) CF (36) CF (37) CF (38) CF (39) CF (40) CF (41) CF (42) CF (43) CF (44) CF (45) CF (46) CF (47) CF (48) CF (49) CF (50) CF (51) CF (52) CF (53) CF (54) CF (55) CF (56) CF (57) CF (58) CF (59) CF (60) CF (61) CF (62) CF (63) CF (64) CF (65)
  • Proposls with this term version:
  • Proposal: Martin Juckes [Some standard name updates to improve co]
  • Proposal: Martin Juckes [Some standard name updates to improve co]

    • This term is not aliased.