Frontal Cloud Formation

Frontal Cloud Formation is a meteorological phenomenon constituting a specific type of cloud development that occurs when warm and cold air masses converge along a frontal boundary, distinguished by the systematic lifting of warm air over a denser cold air mass, leading to adiabatic cooling, condensation, and the formation of stratiform or nimboform cloud systems.

40

Publications

3K

Citations

133

Authors

68

Institutions

Publications per year

2017–2026

2

Authors

133

  1. TA
    T. Akiyama

    Meteorological Research Institute

    3 publications · 124 citations

    3

    h-index

  2. UL
    Ulrike Lohmann

    ETH Zurich, Switzerland

    3 publications · 223 citations

    3

    h-index

  3. AD
    Anthony D. Del Genio

    Goddard Institute for Space Studies, United States

    3 publications · 207 citations

    3

    h-index

  4. SA
    Stephen A. Klein

    Lawrence Livermore National Laboratory, United States

    3 publications · 622 citations

    3

    h-index

  5. RA
    Robert A. Houze

    University of Washington, United States

    2 publications · 1K citations

    2

    h-index

1–5 of 133

Venues

  1. Monthly Weather Review

    10 publications · 755 citations

    10

    h-index

  2. 6

    h-index

  3. 6

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 3 publications · 268 citations

    3

    h-index

  5. Journal of Climate

    2 publications · 39 citations

    2

    h-index

1–5