Chinook Winds

Chinook Winds is a meteorological phenomenon characterized as a type of warm, dry downslope wind occurring on the leeward side of mountain ranges, distinguished from other mountain-valley winds by its association with adiabatic warming and the resultant rapid temperature increase and snowmelt.

17

Publications

603

Citations

34

Authors

17

Institutions

Publications per year

2017–2026

1

Authors

34

  1. LC
    Lawrence C. Nkemdirim

    University of Calgary, Canada

    3 publications · 87 citations

    3

    h-index

  2. MR
    Michael Rose

    Universität Hamburg, Germany

    2 publications · 139 citations

    2

    h-index

  3. GG
    Gary Gelfand

    University of Calgary, Canada

    1 publications · 18 citations

    1

    h-index

  4. WR
    W. R. Henson

    Yale University, United States

    1 publications · 19 citations

    1

    h-index

  5. WB
    WJ Becker

    University of Calgary, Canada

    1 publications · 103 citations

    1

    h-index

1–5 of 34

Venues

  1. Weather and Forecasting

    2 publications · 97 citations

    2

    h-index

  2. Journal of Renewable and Sustainable Energy

    JRSE · 1 publications · 29 citations

    1

    h-index

  3. International Journal of Climatology

    1 publications · 43 citations

    1

    h-index

  4. Headache The Journal of Head and Face Pain

    1 publications · 36 citations

    1

    h-index

  5. Journal of Geography

    1 publications · 13 citations

    1

    h-index

1–5