Deep Convective Cloud Processes

Deep Convective Cloud Processes is a meteorological phenomenon characterized by intense, vertically developed cloud systems that transport heat, moisture, and momentum from the lower to the upper troposphere through strong updrafts and downdrafts, distinguishing it from shallow and mid-level convection by its significant vertical extent, anvil formation, and role in tropical weather and climate dynamics.

161

Publications

9.3K

Citations

765

Authors

269

Institutions

Publications per year

2017–2026

50

Authors

765

  1. AM
    Annica M. L. Ekman

    Stockholm University, Sweden

    7 publications · 233 citations

    7

    h-index

  2. RK
    Radovan Krejčí

    Stockholm University, Sweden

    5 publications · 397 citations

    5

    h-index

  3. MC
    M. C. Barth

    NSF National Center for Atmospheric Research, United States

    5 publications · 404 citations

    5

    h-index

  4. CW
    Chien Wang

    Massachusetts Institute of Technology, United States

    4 publications · 238 citations

    4

    h-index

  5. JS
    Joanne Simpson

    Goddard Space Flight Center, United States

    4 publications · 270 citations

    4

    h-index

1–5 of 765

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 21 publications · 2K citations

    20

    h-index

  2. Journal of the Atmospheric Sciences

    16 publications · 994 citations

    14

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 14 publications · 446 citations

    12

    h-index

  4. Atmospheric Research

    14 publications · 472 citations

    12

    h-index

  5. Atmospheric chemistry and physics

    14 publications · 583 citations

    12

    h-index

1–5