Mountain Wave Effects

Mountain Wave Effects is a meteorological phenomenon characterized by oscillating air currents on the leeward side of mountainous terrain, arising from the interaction of stable airflow with topographic barriers, which distinguishes it from other atmospheric turbulence mechanisms by its periodic, wave-like structure and potential to produce lenticular clouds and severe downdrafts affecting aircraft performance and safety.

81

Publications

3.1K

Citations

263

Authors

126

Institutions

Publications per year

2017–2026

14

Authors

263

  1. AD
    Andreas Dörnbrack

    Deutsches Zentrum für Luft- und Raumfahrt e. V. (DLR), Germany

    5 publications · 366 citations

    5

    h-index

  2. RB
    Ronald B. Smith

    Yale University, United States

    5 publications · 466 citations

    5

    h-index

  3. JD
    James D. Doyle

    United States Naval Research Laboratory, United States

    3 publications · 336 citations

    3

    h-index

  4. RM
    R. M. Worthington

    University of Wales, United Kingdom

    3 publications · 67 citations

    3

    h-index

  5. SV
    Simon Vosper

    Met Office, United Kingdom

    3 publications · 242 citations

    3

    h-index

1–5 of 263

Venues

  1. Journal of the Atmospheric Sciences

    11 publications · 485 citations

    11

    h-index

  2. 9

    h-index

  3. Geophysical Research Letters

    7 publications · 166 citations

    7

    h-index

  4. Monthly Weather Review

    5 publications · 306 citations

    5

    h-index

  5. Tellus A Dynamic Meteorology and Oceanography

    5 publications · 80 citations

    5

    h-index

1–5