Adiabatic Descent

Adiabatic Descent is a thermodynamic process in which a parcel of air descends in the atmosphere without exchanging heat with its surroundings, resulting in compression and a rise in temperature due to increasing ambient pressure.

14

Publications

600

Citations

40

Authors

24

Institutions

Publications per year

2017–2026

3

Authors

40

  1. JP
    J. P. F. Fortuin

    Royal Netherlands Meteorological Institute, Netherlands

    2 publications · 179 citations

    2

    h-index

  2. JO
    J. Oerlemans

    Utrecht University, Netherlands

    2 publications · 179 citations

    2

    h-index

  3. MS
    Michael Sprenger

    ETH Zurich, Switzerland

    2 publications · 44 citations

    2

    h-index

  4. RT
    Richard Turner

    National Institute of Water and Atmospheric Research, New Zealand

    1 publications · 10 citations

    1

    h-index

  5. LJ
    Lukas Jansing

    ETH Zurich, Switzerland

    1 publications · 19 citations

    1

    h-index

1–5 of 40

Venues

  1. Monthly Weather Review

    2 publications · 54 citations

    2

    h-index

  2. Annals of Glaciology

    2 publications · 179 citations

    2

    h-index

  3. Journal of Climate

    2 publications · 52 citations

    2

    h-index

  4. 2

    h-index

  5. Physical Review A

    PRA · 1 publications · 101 citations

    1

    h-index

1–5