Secondary Fronts
Secondary Fronts is a meteorological phenomenon classified as a type of weather front that develops within the broader circulation of a primary frontal system, distinguished by its formation along zones of enhanced baroclinic instability downstream of the parent front, often associated with the maturation of mid-latitude cyclones.
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Institutions
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2017–2026
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G. W. K. Moore, W. R. Peltier · Journal of the Atmospheric Sciences · 1987 · 55 citations · Full text
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University of Reading
Reading, United Kingdom
3 h-index
5 publications
302 citations
Princeton University
Princeton, United States
2 h-index
2 publications
149 citations
Columbia University
New York, United States
2 h-index
2 publications
120 citations
ETH Zurich
Zurich, Switzerland
2 h-index
2 publications
56 citations

University of Toronto
Toronto, Canada
2 h-index
3 publications
162 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
2 h-index
2 publications
120 citations

Kyoto University
Kyoto, Japan
1 h-index
1 publications
39 citations
National Marine Environmental Forecasting Center
Beijing, China
1 h-index
1 publications
42 citations
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4 publications · 182 citations
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2 publications · 149 citations
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2 publications · 45 citations
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1 publications · 55 citations
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ApJ · 1 publications · 26 citations
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