Gravity-driven Airflow

Gravity-Driven Airflow is a meteorological phenomenon characterized by the downslope movement of dense, cool air masses under the influence of gravity, distinguishing it from other atmospheric flows by its thermally induced density contrast and topographic channeling.

16

Publications

484

Citations

59

Authors

29

Institutions

Publications per year

2017–2026

4

Variants

Katabatic Wind

Authors

59

  1. SJ
    S. J. D. D’Alessio

    University of Waterloo, Canada

    2 publications · 36 citations

    2

    h-index

  2. JP
    J. P. Pascal

    Toronto Metropolitan University, Canada

    2 publications · 36 citations

    2

    h-index

  3. BJ
    Benjamin J. Glasser

    Rutgers, The State University of New Jersey, United States

    1 publications · 42 citations

    1

    h-index

  4. TJ
    Travis Jay Miller

    Department of Atomic Energy, India

    1 publications · 15 citations

    1

    h-index

  5. TJ
    T. J. Mountziaris

    University at Buffalo, State University of New York, United States

    1 publications · 24 citations

    1

    h-index

1–5 of 59

Venues

  1. 1

    h-index

  2. Journal of Thermal Analysis and Calorimetry

    1 publications · 67 citations

    1

    h-index

  3. Nuclear Engineering and Design

    1 publications · 23 citations

    1

    h-index

  4. Pharmaceutical technology

    1 publications · 42 citations

    1

    h-index

  5. Energies

    1 publications · 18 citations

    1

    h-index

1–5