Boundary Layer Decoupling

Boundary Layer Decoupling is a meteorological phenomenon in which the convective boundary layer becomes stratified into distinct sublayers, characterized by the suppression of turbulent exchange between the surface-driven mixed layer and the overlying air, thereby inhibiting vertical communication of heat, moisture, and momentum in the lower atmosphere.

81

Publications

5.3K

Citations

281

Authors

120

Institutions

Publications per year

2017–2026

18

Authors

281

  1. CS
    Christopher S. Bretherton

    University of Washington, United States

    8 publications · 1.3K citations

    8

    h-index

  2. DA
    David A. Leon

    London School of Hygiene & Tropical Medicine, United Kingdom

    3 publications · 422 citations

    3

    h-index

  3. PG
    Peter G. Duynkerke

    Utrecht University, Netherlands

    3 publications · 206 citations

    3

    h-index

  4. AL
    Adrian Lock

    Met Office, United Kingdom

    3 publications · 249 citations

    3

    h-index

  5. BA
    Bruce Albrecht

    University of Miami, United States

    3 publications · 144 citations

    3

    h-index

1–5 of 281

Venues

  1. Journal of the Atmospheric Sciences

    16 publications · 1.5K citations

    15

    h-index

  2. 10

    h-index

  3. Atmospheric chemistry and physics

    7 publications · 548 citations

    7

    h-index

  4. Journal of Climate

    5 publications · 225 citations

    5

    h-index

  5. Monthly Weather Review

    4 publications · 183 citations

    4

    h-index

1–5