Cold-air Damming

Cold-Air Damming is a mesoscale meteorological phenomenon characterized by the persistence of a shallow, stable layer of cold air trapped against elevated terrain, typically east of mountain barriers, as a result of synoptic-scale anticyclonic flow that inhibits mixing and displacement, thereby distinguishing it from transient cold-air advection or frontal passage.

31

Publications

1.4K

Citations

68

Authors

28

Institutions

Publications per year

2017–2026

0

Variants

Cold Air Damming

Authors

68

  1. TT
    Thomas T. Warner

    University College London, United Kingdom

    3 publications · 82 citations

    3

    h-index

  2. LF
    Lance F. Bosart

    University at Albany, State University of New York, United States

    3 publications · 263 citations

    3

    h-index

  3. GM
    Gary M. Lackmann

    North Carolina State University, United States

    3 publications · 65 citations

    3

    h-index

  4. JD
    James D. Doyle

    United States Naval Research Laboratory, United States

    2 publications · 50 citations

    2

    h-index

  5. QX
    Qin Xu

    NOAA National Severe Storms Laboratory, United States

    2 publications · 46 citations

    2

    h-index

1–5 of 68

Venues

  1. Monthly Weather Review

    12 publications · 578 citations

    11

    h-index

  2. Weather and Forecasting

    10 publications · 440 citations

    10

    h-index

  3. Journal of the Atmospheric Sciences

    3 publications · 78 citations

    3

    h-index

  4. Bulletin of the American Meteorological Society

    BAMS · 1 publications · 108 citations

    1

    h-index

  5. Physical Geography

    1 publications · 31 citations

    1

    h-index

1–5