Chinook Winds
Chinook Winds is a meteorological phenomenon characterized as a type of warm, dry downslope wind occurring on the leeward side of mountain ranges, distinguished from other mountain-valley winds by its association with adiabatic warming and the resultant rapid temperature increase and snowmelt.
17
Publications
603
Citations
34
Authors
17
Institutions
Publications per year
2017–2026
1
17
Chinook winds and migraine headache
Lara Cooke, Michael Rose, WJ Becker · Neurology · 2000 · 103 citations
Lawrence C. Nkemdirim · International Journal of Climatology · 1996 · 43 citations
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17

University of Calgary
Calgary, Canada
7 h-index
13 publications
586 citations
NOAA National Weather Service
Silver Spring, United States
2 h-index
2 publications
40 citations

Parks Canada
Ottawa, Canada
1 h-index
3 publications
87 citations
Queen's University
Kingston, Canada
1 h-index
1 publications
29 citations
Geological Survey of Canada
Ottawa, Canada
1 h-index
1 publications
53 citations
Indiana University – Purdue University Indianapolis
Indianapolis, United States
1 h-index
1 publications
17 citations

University of Lethbridge
Lethbridge, Canada
1 h-index
1 publications
53 citations

Instituto Nacional de Pesquisas Espaciais
São José dos Campos, Brazil
1 h-index
3 publications
210 citations
1–8 of 17
2 publications · 97 citations
2
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JRSE · 1 publications · 29 citations
1
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1 publications · 43 citations
1
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1 publications · 36 citations
1
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1 publications · 13 citations
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