Mountain Inversions
Mountain Inversions is a meteorological phenomenon characterized by a temperature inversion layer that forms within the mountain boundary layer, in which atmospheric temperature increases with altitude due to radiative cooling of mountain surfaces and subsequent cold air pooling in valleys, distinguishing it from free-atmospheric lapse rate patterns.
27
Publications
1.5K
Citations
75
Authors
47
Institutions
Publications per year
2017–2026
8
Variants
Mountain Temperature Inversions
27
1–5 of 27
75
5
h-index
3
h-index
Cooperative Institute for Research in Environmental Sciences, United States
1 publications · 23 citations
1
h-index
Khalifa University of Science and Technology, United Arab Emirates
1 publications · 31 citations
1
h-index
1
h-index
1–5 of 75
47
Colorado State University
Fort Collins, United States
3 h-index
4 publications
178 citations

Pacific Northwest National Laboratory
Richland, United States
2 h-index
2 publications
183 citations
ETH Zurich
Zurich, Switzerland
2 h-index
2 publications
59 citations

Eötvös Loránd University
Budapest, Hungary
1 h-index
1 publications
25 citations

Utah State University
Logan, United States
1 h-index
5 publications
135 citations
Ludwig-Maximilians-Universität München
Munich, Germany
1 h-index
1 publications
30 citations

Macquarie University
Sydney, Australia
1 h-index
1 publications
93 citations

University of Leeds
Leeds, United Kingdom
1 h-index
1 publications
31 citations
1–8 of 47
3 publications · 432 citations
3
h-index
2 publications · 44 citations
2
h-index
2 publications · 65 citations
2
h-index
1 publications · 30 citations
1
h-index
1 publications · 163 citations
1
h-index
1–5