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Chinook winds, or simply Chinooks, are two types of prevailing warm, generally westerly winds in western North America: Coastal Chinooks and interior Chinooks. The coastal Chinooks are persistent seasonal, wet, southwesterly winds blowing in from the ocean. The interior Chinooks are occasional warm, dry föhn winds blowing down the eastern sides of interior mountain ranges. The coastal Chinooks were the original term, used along the northwest coast, and the term in the interior of North ...
Apr 28, 2017 · Chinook winds develop when warm, moist air blows from the Pacific Ocean in the northwest region of North America toward the Rocky Mountain range, according to Rocky Mountain National Park.The air ...
Jul 17, 2024 · Chinook winds got their name from the Chinook Native American people who lived in coastal areas near the Columbia River (in the States of Washington and Oregon), where these winds occur on a regular basis.. Föehn winds originate from the German word "Föhn," which literally means hot, dry wind.
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Chinook, warm, dry wind descending the eastern slopes of the Rocky Mountains, primarily in winter. Winds of the same kind occur in other parts of the world and are known generally as foehns
While strong winds often occur during a storm, there are some instances in western North America where high winds can develop when the sky is clear.
Chinook winds, or simply Chinooks, are a warm, dry wind that blows mostly in the winter along the eastern slopes of the Rocky Mountains. The Chinook is a type of local wind which is part of the Geography syllabus of the UPSC examination.
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Frequency and Intensity. Chinook winds occur in every season but are more distinctive and numerous in the winter when the unseasonable warming it brings differentiates it from the normal cold winter weather. In southwestern Alberta, one in 3 winter days is a chinook day; its frequency drops to one in 5 in the northeast.The maximum daily temperature anomaly associated with the wind ranges from +13°C in the northwest to +25°C in the southeast.
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