Cloud-topped Boundary Layers

Cloud-Topped Boundary Layer is a meteorological boundary layer regime characterized by the presence of a cloud field at its upper boundary, distinguishing it from cloud-free or decoupled boundary layer structures through the coupling of radiative, turbulent, and microphysical processes that sustain cloud persistence and influence boundary layer depth.

131

Publications

10.8K

Citations

354

Authors

136

Institutions

Publications per year

2017–2026

15

Authors

354

  1. BS
    Björn Stevens

    Max Planck Institute for Meteorology, Germany

    12 publications · 2K citations

    12

    h-index

  2. CS
    Christopher S. Bretherton

    University of Washington, United States

    13 publications · 2.9K citations

    12

    h-index

  3. CM
    Chin‐Hoh Moeng

    NSF National Center for Atmospheric Research, United States

    12 publications · 1.8K citations

    12

    h-index

  4. AS
    Andrew S. Ackerman

    Goddard Institute for Space Studies, United States

    6 publications · 1.2K citations

    6

    h-index

  5. SR
    Stephan R. de Roode

    Delft University of Technology, Netherlands

    6 publications · 184 citations

    6

    h-index

1–5 of 354

Venues

  1. Journal of the Atmospheric Sciences

    58 publications · 4.3K citations

    37

    h-index

  2. 13

    h-index

  3. Atmospheric chemistry and physics

    13 publications · 534 citations

    11

    h-index

  4. Monthly Weather Review

    9 publications · 2.8K citations

    9

    h-index

  5. Boundary-Layer Meteorology

    7 publications · 211 citations

    7

    h-index

1–5