Frontal Cloud Formation
Frontal Cloud Formation is a meteorological phenomenon constituting a specific type of cloud development that occurs when warm and cold air masses converge along a frontal boundary, distinguished by the systematic lifting of warm air over a denser cold air mass, leading to adiabatic cooling, condensation, and the formation of stratiform or nimboform cloud systems.
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Orographic effects on precipitating clouds
Robert A. Houze · Reviews of Geophysics · 2011 · 951 citations · Full text
Shaocheng Xie, Minghua Zhang, Mark Branson et al. · Journal of Geophysical Research Atmospheres · 2005 · 119 citations · Full text
Richard J. Reed, Mark T. Stoelinga, Ying‐Hwa Kuo · Monthly Weather Review · 1992 · 118 citations · Full text
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Goddard Institute for Space Studies, United States
3 publications · 207 citations
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University of Washington
Seattle, United States
4 h-index
9 publications
1.4K citations
Meteorological Research Institute
Tsukuba, Japan
4 h-index
4 publications
206 citations

Goddard Institute for Space Studies
New York, United States
4 h-index
10 publications
570 citations
Met Office
Exeter, United Kingdom
4 h-index
7 publications
299 citations
Dalhousie University
Halifax, Canada
3 h-index
5 publications
407 citations

China Meteorological Administration
Beijing, China
2 h-index
8 publications
249 citations
University of Reading
Reading, United Kingdom
2 h-index
4 publications
520 citations

Lawrence Livermore National Laboratory
Livermore, United States
2 h-index
7 publications
671 citations
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10 publications · 755 citations
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6 publications · 174 citations
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6 publications · 334 citations
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JGR · 3 publications · 268 citations
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2 publications · 39 citations
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