Surface Radiation Balance is the net flux of radiant energy at the Earth's surface, defined as the difference between incoming and outgoing shortwave and longwave radiation, that governs the energy available for land-atmosphere interactions, including microclimatic phenomena such as fog formation.
362
Publications
30.1K
Citations
1.3K
Authors
459
Institutions
Publications per year
2017–2026
68
Variants
Surface Net Radiation
Publications
362
Cloud-Radiative Forcing and Climate: Results from the Earth Radiation Budget Experiment
V. Ramanathan, R. D. Cess, Edwin F. Harrison et al. · Science · 1989 · 1.9K citations
The Heat Balance of the Earth's Surface
M. I. Budyko · Soviet Geography · 1961 · 891 citations
1–5 of 362
Authors
1.3K
- PM
7
h-index
- WR
6
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- GS
5
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- DL
5
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- MW
5
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1–5 of 1.3K
Institutions
459
Chinese Academy of Sciences
Beijing, China
16 h-index
56 publications
2.5K citations
Langley Research Center
Hampton, United States
13 h-index
23 publications
12.8K citations
University of Washington
Seattle, United States
12 h-index
22 publications
4.7K citations
University of Colorado Boulder
Boulder, United States
9 h-index
19 publications
1.7K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
8 h-index
12 publications
1.6K citations
ETH Zurich
Zurich, Switzerland
7 h-index
17 publications
1.8K citations
Goddard Space Flight Center
Greenbelt, United States
7 h-index
16 publications
3K citations
Met Office
Exeter, United Kingdom
7 h-index
18 publications
1.6K citations
1–8 of 459
Venues
- Journal of Geophysical Research Atmospheres
JGR · 32 publications · 3K citations
27
h-index
- Journal of Climate
20 publications · 3.3K citations
18
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- Geophysical Research Letters
21 publications · 2.4K citations
17
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- Journal of Geophysical Research Atmospheres
JGR · 14 publications · 1.1K citations
14
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- Journal of the Atmospheric Sciences
11 publications · 1.5K citations
11
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1–5