Interaction With Synoptic-scale Flow
Interaction with Synoptic-Scale Flow is a meteorological phenomenon within the study of boundary-layer dynamics wherein the diurnally driven land-breeze circulation is modulated in structure, intensity, or propagation by the prevailing large-scale synoptic wind patterns.
30
Publications
2.3K
Citations
98
Authors
51
Institutions
Publications per year
2017–2026
4
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1–5 of 30
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University at Albany, State University of New York, United States
3 publications · 329 citations
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2
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1
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1–5 of 98
51
University of Washington
Seattle, United States
3 h-index
7 publications
420 citations
NOAA National Weather Service
Silver Spring, United States
3 h-index
4 publications
781 citations
Massachusetts Institute of Technology
Cambridge, United States
2 h-index
3 publications
581 citations

Bureau of Meteorology
Melbourne, Australia
2 h-index
2 publications
81 citations
University at Albany, State University of New York
Albany, United States
2 h-index
4 publications
498 citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
2 h-index
10 publications
390 citations

City University of Hong Kong
Hong Kong, Hong Kong
1 h-index
2 publications
184 citations
Laboratoire de Météorologie Dynamique
Palaiseau, France
1 h-index
1 publications
52 citations
1–8 of 51
9 publications · 880 citations
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4 publications · 747 citations
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2 publications · 63 citations
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2 publications · 69 citations
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2 publications · 71 citations
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