Upslope Flow Dynamics

Upslope Flow Dynamics is a meteorological process in which moist air is forced to ascend along a topographic slope, leading to adiabatic cooling, condensation, and orographic precipitation, and is distinguished from other atmospheric lifting mechanisms by its direct dependence on terrain-induced vertical motion.

73

Publications

4K

Citations

221

Authors

111

Institutions

Publications per year

2017–2026

9

Authors

221

  1. MS
    M. Segal

    Colorado State University, United States

    4 publications · 385 citations

    4

    h-index

  2. CD
    C. David Whiteman

    University of Utah, United States

    3 publications · 323 citations

    3

    h-index

  3. LU
    Lars Umlauf

    Leibniz Institute for Baltic Sea Research Warnemünde, Germany

    3 publications · 123 citations

    3

    h-index

  4. RA
    Roger A. Pielke

    Colorado State University, United States

    2 publications · 93 citations

    2

    h-index

  5. RF
    Roger F. Reinking

    Cooperative Institute for Research in Environmental Sciences, United States

    2 publications · 38 citations

    2

    h-index

1–5 of 221

Venues

  1. Monthly Weather Review

    15 publications · 1.1K citations

    15

    h-index

  2. Journal of the Atmospheric Sciences

    9 publications · 442 citations

    9

    h-index

  3. Journal of Geophysical Research Atmospheres

    JGR · 7 publications · 446 citations

    7

    h-index

  4. 3

    h-index

  5. Weather and Forecasting

    3 publications · 56 citations

    3

    h-index

1–5