Synoptic-scale Divergence
Synoptic-Scale Divergence is a meteorological quantity representing the horizontal spreading of air masses at the synoptic scale, distinguished by its characterization of large-scale atmospheric flow patterns associated with weather systems such as highs, lows, and fronts.
21
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1.1K
Citations
42
Authors
28
Institutions
Publications per year
2017–2026
3
Parents
21
Results of Detailed Synoptic Studies of Squall Lines
Tetsuya Theodore. Fujita · Tellus · 1955 · 68 citations
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Max Planck Institute for Meteorology
Hamburg, Germany
2 h-index
3 publications
113 citations
Japan Agency for Marine-Earth Science and Technology
Yokosuka, Japan
1 h-index
2 publications
132 citations
Bjerknes Centre for Climate Research
Bergen, Norway
1 h-index
1 publications
26 citations

Centre National de la Recherche Scientifique
Paris, France
1 h-index
1 publications
61 citations
Meteorological Research Institute
Tsukuba, Japan
1 h-index
2 publications
34 citations
Met Office
Exeter, United Kingdom
1 h-index
1 publications
14 citations

Instituto Nacional de Pesquisas Espaciais
São José dos Campos, Brazil
1 h-index
1 publications
22 citations
Naval Research Laboratory Marine Meteorology Division
Monterey, United States
1 h-index
2 publications
416 citations
1–8 of 28
8 publications · 495 citations
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JGR · 2 publications · 78 citations
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2 publications · 151 citations
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2 publications · 43 citations
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1 publications · 11 citations
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