Ridge-top Flow

Ridge-Top Flow is a meteorological phenomenon characterized by the accelerated and often turbulent airflow that occurs when wind passes over the crest of a topographic ridge, distinguished from surrounding wind patterns by its enhancement due to orographic lifting and flow compression at the summit.

51

Publications

2.7K

Citations

115

Authors

52

Institutions

Publications per year

2017–2026

8

Authors

115

  1. JF
    John Finnigan

    Commonwealth Scientific and Industrial Research Organisation, Australia

    3 publications · 182 citations

    3

    h-index

  2. TI
    Takeshi Ishihara

    The University of Tokyo, Japan

    2 publications · 119 citations

    2

    h-index

  3. SC
    Stuart Cameron

    University of Aberdeen, United Kingdom

    2 publications · 95 citations

    2

    h-index

  4. RI
    R. I. Sykes

    Met Office, United Kingdom

    2 publications · 248 citations

    2

    h-index

  5. MS
    Michael S. Shipman

    Geophex (United States), United States

    2 publications · 67 citations

    2

    h-index

1–5 of 115

Venues

  1. Boundary-Layer Meteorology

    8 publications · 380 citations

    8

    h-index

  2. Journal of the Atmospheric Sciences

    3 publications · 55 citations

    3

    h-index

  3. Atmospheric Environment (1967)

    3 publications · 86 citations

    3

    h-index

  4. 3

    h-index

  5. Journal of Applied Meteorology

    2 publications · 310 citations

    2

    h-index

1–5