Stable Boundary Layer Effects

Stable Boundary Layer Effects is a meteorological phenomenon characterized by the suppression of turbulent mixing in the atmospheric boundary layer due to a temperature inversion, typically occurring at night or in valley bottoms, which enhances the persistence and structure of downslope and down-valley winds.

49

Publications

5.9K

Citations

169

Authors

93

Institutions

Publications per year

2017–2026

13

Authors

169

  1. JE
    John Edwards

    Met Office, United Kingdom

    3 publications · 115 citations

    3

    h-index

  2. PS
    P. S. Anderson

    British Antarctic Survey, United Kingdom

    3 publications · 92 citations

    3

    h-index

  3. AA
    Andrey A. Grachev

    Cooperative Institute for Research in Environmental Sciences, United States

    2 publications · 78 citations

    2

    h-index

  4. DB
    David B. Parsons

    NSF National Center for Atmospheric Research, United States

    2 publications · 99 citations

    2

    h-index

  5. CW
    C. W. Fairall

    NOAA Earth System Research Laboratory, United States

    2 publications · 78 citations

    2

    h-index

1–5 of 169

Venues

  1. Boundary-Layer Meteorology

    18 publications · 1.2K citations

    17

    h-index

  2. Bulletin of the American Meteorological Society

    BAMS · 3 publications · 91 citations

    3

    h-index

  3. 3

    h-index

  4. Journal of Geophysical Research Atmospheres

    JGR · 2 publications · 3.3K citations

    2

    h-index

  5. Monthly Weather Review

    2 publications · 124 citations

    2

    h-index

1–5