Interaction with Background Wind is a meteorological phenomenon in which the sea-breeze circulation modifies and is modified by the prevailing synoptic-scale wind flow, altering the strength, depth, and inland penetration of the sea breeze depending on the angle and magnitude of the background wind relative to the coastline.
99
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294
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163
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2017–2026
24
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Publications
99
1–5 of 99
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294
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5
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3
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163
NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
6 publications
650 citations
Kyoto University
Kyoto, Japan
4 h-index
7 publications
355 citations
University of Colorado Boulder
Boulder, United States
4 h-index
6 publications
209 citations
Northwest Research Associates
Redmond, United States
4 h-index
6 publications
449 citations
University of Hong Kong
Pok Fu Lam, Hong Kong
3 h-index
9 publications
194 citations
Aberystwyth University
Aberystwyth, United Kingdom
3 h-index
4 publications
191 citations
NSF NCAR High Altitude Observatory
Boulder, United States
3 h-index
3 publications
362 citations
Wuhan University
Wuhan, China
3 h-index
7 publications
120 citations
1–8 of 163
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- Journal of Geophysical Research Atmospheres
JGR · 22 publications · 1.9K citations
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- Journal of the Atmospheric Sciences
14 publications · 667 citations
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- Geophysical Research Letters
11 publications · 588 citations
11
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- Annales Geophysicae
7 publications · 118 citations
7
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- Quarterly Journal of the Royal Meteorological Society
5 publications · 176 citations
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