Low-stratus Boundary Layers

Low-Stratus Boundary Layers is a meteorological construct denoting a type of atmospheric boundary layer characterized by the persistent presence of a shallow, horizontally extensive stratus cloud deck that forms and sustains within a stably stratified layer near the Earth's surface, primarily driven by radiative cooling, turbulent mixing, and cloud-top entrainment processes unique to low-cloud regimes.

25

Publications

2.2K

Citations

44

Authors

25

Institutions

Publications per year

2017–2026

1

Authors

44

  1. SA
    S. A. Kitaigorodskii

    Johns Hopkins University, United States

    4 publications · 116 citations

    4

    h-index

  2. SM
    Sylvain M. Joffre

    Finnish Meteorological Institute, Finland

    2 publications · 89 citations

    2

    h-index

  3. MT
    Michael Tjernström

    Stockholm University, Sweden

    2 publications · 27 citations

    2

    h-index

  4. LM
    L. Mahrt

    Oregon State University, United States

    2 publications · 961 citations

    2

    h-index

  5. GW
    GR Walker

    2 publications · 80 citations

    1

    h-index

1–5 of 44

Venues

  1. Boundary-Layer Meteorology

    5 publications · 1.1K citations

    5

    h-index

  2. Tellus A Dynamic Meteorology and Oceanography

    4 publications · 116 citations

    4

    h-index

  3. Atmospheric Research

    3 publications · 180 citations

    3

    h-index

  4. Monthly Weather Review

    2 publications · 23 citations

    2

    h-index

  5. Journal of Geophysical Research Atmospheres

    JGR · 2 publications · 101 citations

    2

    h-index

1–5