Downslope Windstorms

Downslope Windstorms is a type of regional atmospheric phenomenon within mountain wind systems characterized by strong, gusty, and often turbulent winds that descend from mountainous terrain through the acceleration of air masses forced over topographic barriers and amplified by gravity-driven flow and resonance effects in stably stratified layers.

121

Publications

5.6K

Citations

269

Authors

114

Institutions

Publications per year

2017–2026

32

Authors

269

  1. WR
    W. R. Peltier

    University of Toronto, Canada

    10 publications · 665 citations

    10

    h-index

  2. RG
    Robert G. Fovell

    University of California, Los Angeles, United States

    6 publications · 265 citations

    6

    h-index

  3. CD
    C. David Whiteman

    University of Utah, United States

    6 publications · 321 citations

    6

    h-index

  4. JS
    John Scinocca

    Environment and Climate Change Canada, Canada

    5 publications · 151 citations

    5

    h-index

  5. TL
    Terry L. Clark

    NSF National Center for Atmospheric Research, United States

    5 publications · 955 citations

    5

    h-index

1–5 of 269

Venues

  1. Journal of the Atmospheric Sciences

    27 publications · 2.4K citations

    19

    h-index

  2. Monthly Weather Review

    15 publications · 632 citations

    15

    h-index

  3. Weather and Forecasting

    14 publications · 564 citations

    13

    h-index

  4. 6

    h-index

  5. Atmosphere

    7 publications · 218 citations

    5

    h-index

1–5