Stratospheric Cooling
Stratospheric Cooling is a climatological phenomenon characterized by the long-term decrease in temperature within the stratosphere, primarily distinguished from tropospheric warming by its association with increased radiative heat loss due to rising concentrations of greenhouse gases, particularly carbon dioxide, under conditions of reduced solar absorption and stratospheric ozone depletion.
558
Publications
42.8K
Citations
1.5K
Authors
454
Institutions
Publications per year
2017–2026
116
Parents
558
1–5 of 558
1.5K
National Oceanic and Atmospheric Administration, United States
18 publications · 2.7K citations
18
h-index
NSF National Center for Atmospheric Research, United States
18 publications · 2.7K citations
17
h-index
15
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15
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15
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1–5 of 1.5K
454

NSF National Center for Atmospheric Research
Boulder, United States
40 h-index
147 publications
16.6K citations
Goddard Space Flight Center
Greenbelt, United States
31 h-index
94 publications
7.8K citations
University of Washington
Seattle, United States
25 h-index
55 publications
10.9K citations
Met Office
Exeter, United Kingdom
22 h-index
52 publications
4.5K citations
Columbia University
New York, United States
22 h-index
39 publications
3.2K citations
University of Colorado Boulder
Boulder, United States
22 h-index
46 publications
5.1K citations

University of Leeds
Leeds, United Kingdom
21 h-index
38 publications
4.7K citations
University of Reading
Reading, United Kingdom
20 h-index
43 publications
5.3K citations
1–8 of 454
124 publications · 7.8K citations
48
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JGR · 66 publications · 6.2K citations
43
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60 publications · 6.2K citations
37
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JGR · 31 publications · 1.7K citations
26
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35 publications · 2.8K citations
24
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