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
Parents
14
Annette Miltenberger, Silvia Reynolds, Michael Sprenger · Quarterly Journal of the Royal Meteorological Society · 2016 · 49 citations
1–5 of 14
40
Royal Netherlands Meteorological Institute, Netherlands
2 publications · 179 citations
2
h-index
2
h-index
2
h-index
National Institute of Water and Atmospheric Research, New Zealand
1 publications · 10 citations
1
h-index
1
h-index
1–5 of 40
24
ETH Zurich
Zurich, Switzerland
3 h-index
6 publications
210 citations

Chinese Academy of Sciences
Beijing, China
2 h-index
3 publications
117 citations
Institute for Biomedical Engineering
Zurich, Switzerland
2 h-index
4 publications
172 citations
Institute of Atmospheric Physics
Beijing, China
2 h-index
2 publications
93 citations
Utrecht University
Utrecht, The Netherlands
2 h-index
4 publications
358 citations
Bjerknes Centre for Climate Research
Bergen, Norway
1 h-index
2 publications
48 citations
Federal Department of Home Affairs
Bern, Switzerland
1 h-index
1 publications
49 citations

Université de Sherbrooke
Sherbrooke, Canada
1 h-index
2 publications
202 citations
1–8 of 24
2 publications · 54 citations
2
h-index
2 publications · 179 citations
2
h-index
2 publications · 52 citations
2
h-index
2 publications · 68 citations
2
h-index
PRA · 1 publications · 101 citations
1
h-index
1–5