Slope-driven Wind Systems

Slope-Driven Wind Systems is a meteorological phenomenon characterized by thermally induced airflows that develop along mountain slopes due to differential heating and cooling, distinguishing it from large-scale synoptic winds by its localized topographic dependence and diurnal reversal pattern.

8

Publications

300

Citations

26

Authors

14

Institutions

Publications per year

2017–2026

1

Authors

26

  1. RA
    R. A. Preston‐Whyte

    University of KwaZulu-Natal, South Africa

    1 publications · 40 citations

    1

    h-index

  2. AG
    Alexander Gohm

    Universität Innsbruck, Austria

    1 publications · 53 citations

    1

    h-index

  3. HZ
    Han Zou

    Institute of Atmospheric Physics, China

    1 publications · 43 citations

    1

    h-index

  4. BT
    Bruce T. Anderson

    Boston University, United States

    1 publications · 40 citations

    1

    h-index

  5. AL
    Aiguo Li

    Chinese Academy of Sciences, China

    1 publications · 43 citations

    1

    h-index

1–5 of 26

Venues

  1. Journal of Applied Meteorology and Climatology

    JAMC · 1 publications · 10 citations

    1

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 1 publications · 40 citations

    1

    h-index

  3. Geophysical Research Letters

    1 publications · 43 citations

    1

    h-index

  4. Journal of applied meteorology

    1 publications · 40 citations

    1

    h-index

  5. Boundary-Layer Meteorology

    1 publications · 65 citations

    1

    h-index

1–5