Stratiform Cloud Condensation

Stratiform Cloud Condensation is a meteorological process in which widespread, horizontally uniform cloud formation occurs through the gradual cooling of moist air masses below their dew point, distinguished from convective condensation by its stable, layered structure and large-scale, synoptic forcing mechanisms.

25

Publications

2.8K

Citations

66

Authors

35

Institutions

Publications per year

2017–2026

3

Authors

66

  1. HS
    Hilding Sundqvist

    Stockholm University, Sweden

    3 publications · 905 citations

    3

    h-index

  2. PV
    Peter V. Hobbs

    University of Washington, United States

    3 publications · 229 citations

    3

    h-index

  3. RA
    Robert A. Houze

    University of Washington, United States

    2 publications · 187 citations

    2

    h-index

  4. OB
    O. B. Toon

    Ames Research Center, United States

    2 publications · 208 citations

    2

    h-index

  5. JF
    John F. Gamache

    National Oceanic and Atmospheric Administration, United States

    2 publications · 187 citations

    2

    h-index

1–5 of 66

Venues

  1. Journal of the Atmospheric Sciences

    4 publications · 253 citations

    4

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 470 citations

    3

    h-index

  3. Monthly Weather Review

    3 publications · 927 citations

    3

    h-index

  4. Tellus A Dynamic Meteorology and Oceanography

    2 publications · 22 citations

    2

    h-index

  5. Journal of Climate

    2 publications · 87 citations

    2

    h-index

1–5