High-cloud Feedback
High-Cloud Feedback is a climatological feedback mechanism in which changes in the abundance or properties of high-level clouds modulate the Earth's radiative balance, thereby influencing atmospheric temperature and climate dynamics through alterations in longwave and shortwave radiation trapping.
14
Publications
1K
Citations
35
Authors
22
Institutions
Publications per year
2017–2026
5
Parents
14
An Analysis of the Short-Term Cloud Feedback Using MODIS Data
Chen Zhou, Mark D. Zelinka, A. E. Dessler et al. · Journal of Climate · 2013 · 69 citations · Full text
1–5 of 14
35
NSF National Center for Atmospheric Research, United States
3 publications · 84 citations
3
h-index
3
h-index
3
h-index
NSF National Center for Atmospheric Research, United States
2 publications · 57 citations
2
h-index
2
h-index
1–5 of 35
22
University of Washington
Seattle, United States
4 h-index
9 publications
1.3K citations

NSF National Center for Atmospheric Research
Boulder, United States
3 h-index
7 publications
187 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
2 h-index
7 publications
226 citations

Pacific Northwest National Laboratory
Richland, United States
2 h-index
2 publications
57 citations

Lawrence Livermore National Laboratory
Livermore, United States
2 h-index
2 publications
204 citations
The University of Tokyo
Tokyo, Japan
2 h-index
2 publications
70 citations
NSF NCAR Climate and Global Dynamics Laboratory
Boulder, United States
2 h-index
2 publications
61 citations
California Institute of Technology
Pasadena, United States
1 h-index
1 publications
15 citations
1–8 of 22
4 publications · 186 citations
4
h-index
JGR · 3 publications · 503 citations
3
h-index
JGR · 2 publications · 61 citations
2
h-index
2 publications · 67 citations
2
h-index
JAMES · 1 publications · 54 citations
1
h-index
1–5