Upslope Flows

Upslope Flows is a thermally driven atmospheric boundary-layer wind phenomenon characterized by the ascent of air parallel to terrain slope during daytime heating, distinguishing it from other slope wind regimes by its diurnal timing, directionality, and reliance on surface-induced convective instability.

181

Publications

14.3K

Citations

548

Authors

244

Institutions

Publications per year

2017–2026

31

Variants

Anabatic Flows

Authors

548

  1. MS
    M. Segal

    Colorado State University, United States

    6 publications · 746 citations

    6

    h-index

  2. YC
    Yi‐Leng Chen

    University of Hawaiʻi at Mānoa, United States

    4 publications · 147 citations

    4

    h-index

  3. RA
    Roger A. Pielke

    Colorado State University, United States

    4 publications · 454 citations

    4

    h-index

  4. CD
    C. David Whiteman

    University of Utah, United States

    3 publications · 323 citations

    3

    h-index

  5. LU
    Lars Umlauf

    Leibniz Institute for Baltic Sea Research Warnemünde, Germany

    3 publications · 123 citations

    3

    h-index

1–5 of 548

Venues

  1. Monthly Weather Review

    22 publications · 1.4K citations

    19

    h-index

  2. Journal of Geophysical Research Atmospheres

    JGR · 18 publications · 1.6K citations

    17

    h-index

  3. Journal of the Atmospheric Sciences

    15 publications · 962 citations

    15

    h-index

  4. Journal of Physical Oceanography

    8 publications · 373 citations

    8

    h-index

  5. Journal of Fluid Mechanics

    8 publications · 375 citations

    8

    h-index

1–5