Lee-side Eddies

Lee-side eddies is a mesoscale atmospheric phenomenon characterized by the formation of counter-rotating vortices on the leeward side of mountainous terrain, resulting from flow separation and dynamic instability in the boundary layer under stable stratification and moderate to strong cross-mountain winds.

24

Publications

1.5K

Citations

73

Authors

36

Institutions

Publications per year

2017–2026

2

Authors

73

  1. JR
    J. R. E. Lutjeharms

    University of Cape Town, South Africa

    3 publications · 298 citations

    3

    h-index

  2. AH
    Allen H. Whitehead

    Langley Research Center, United States

    2 publications · 34 citations

    2

    h-index

  3. WS
    Won Sang Lee

    Korea Polar Research Institute, South Korea

    1 publications · 20 citations

    1

    h-index

  4. JD
    James D. Doyle

    United States Naval Research Laboratory, United States

    1 publications · 52 citations

    1

    h-index

  5. DR
    David Richmond

    Royal Prince Alfred Hospital, Australia

    1 publications · 41 citations

    1

    h-index

1–5 of 73

Venues

  1. Journal of Geophysical Research Atmospheres

    JGR · 4 publications · 324 citations

    4

    h-index

  2. Geophysical Research Letters

    4 publications · 193 citations

    4

    h-index

  3. AIAA Journal

    2 publications · 34 citations

    2

    h-index

  4. 2

    h-index

  5. Journal of Physical Oceanography

    2 publications · 88 citations

    2

    h-index

1–5