Temperature Gradient Forcing
Temperature Gradient Forcing is a meteorological mechanism that belongs to the class of atmospheric forcing processes, differentially characterized by the induction of anabatic winds through the localized heating contrast between a sloped surface and the adjacent air layer, thereby generating upward-directed buoyancy-driven airflow.
181
Publications
8.1K
Citations
513
Authors
244
Institutions
Publications per year
2017–2026
21
Parents
181
Jaap S. Sinninghe Damsté, Elisabeth C. van Bentum, Gert‐Jan Reichart et al. · Earth and Planetary Science Letters · 2010 · 187 citations
Convective thermocapillary instabilities in liquid bridges
J-J. Xu, S. H. Davis · The Physics of Fluids · 1984 · 154 citations
1–5 of 181
513
6
h-index
5
h-index
4
h-index
3
h-index
3
h-index
1–5 of 513
244

Centre National de la Recherche Scientifique
Paris, France
10 h-index
22 publications
1.2K citations
Columbia University
New York, United States
10 h-index
19 publications
2.9K citations
The University of Texas at Austin
Austin, United States
7 h-index
17 publications
636 citations
Fusion (United States)
Houston, United States
6 h-index
18 publications
930 citations

NSF National Center for Atmospheric Research
Boulder, United States
5 h-index
8 publications
694 citations
Université Claude Bernard Lyon 1
Villeurbanne, France
5 h-index
10 publications
544 citations
Massachusetts Institute of Technology
Cambridge, United States
5 h-index
8 publications
241 citations
Met Office
Exeter, United Kingdom
4 h-index
12 publications
552 citations
1–8 of 244
PRL · 11 publications · 817 citations
11
h-index
11 publications · 1.3K citations
10
h-index
9 publications · 478 citations
9
h-index
9 publications · 290 citations
9
h-index
7 publications · 280 citations
8
h-index
1–5