Cloud Microphysical Growth

Cloud Microphysical Growth is a cloud microphysical process that describes the growth of hydrometeors through in-cloud mechanisms such as condensation, deposition, and collision-coalescence, distinguished from other growth processes by its exclusive dependence on microscale interactions between water vapor, cloud droplets, and ice particles within a supersaturated atmospheric environment.

120

Publications

5.9K

Citations

310

Authors

145

Institutions

Publications per year

2017–2026

24

Authors

310

  1. LR
    L. Randall Koenig

    RAND Corporation, United States

    5 publications · 369 citations

    5

    h-index

  2. GF
    Graham Feingold

    NOAA Earth System Research Laboratory, United States

    4 publications · 452 citations

    4

    h-index

  3. WR
    William R. Cotton

    Colorado State University, United States

    3 publications · 236 citations

    3

    h-index

  4. DR
    Daniel Rosenfeld

    Hebrew University of Jerusalem, Israel

    3 publications · 51 citations

    3

    h-index

  5. EJ
    E. J. Jensen

    Ames Research Center, United States

    3 publications · 108 citations

    3

    h-index

1–5 of 310

Venues

  1. Journal of the Atmospheric Sciences

    35 publications · 2.2K citations

    24

    h-index

  2. 10

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 8 publications · 472 citations

    8

    h-index

  4. Monthly Weather Review

    6 publications · 146 citations

    6

    h-index

  5. The Astrophysical Journal

    ApJ · 5 publications · 617 citations

    5

    h-index

1–5