what are chinook winds

Om 7:32 was het, dankzij een plotseling opgestoken chinook, +7 °C. The ideal setup for a Chinook wind occurs when a strong west to east pressure gradient sets up perpendicular to a mountain range. Deze wind waait vanuit het westen over de Rocky Mountains en over de prairies in het westen van Canada en de Verenigde Staten ().De naam chinook komt van het Chinook-indianenvolk in het noordwesten van Noord-Amerika.. Het chinookfenomeen ontstaat als gevolg van bepaalde klimatologische omstandigheden. De universiteit van Calgary heeft bij de ingang een grote boog staan. Chinooks are generally called föhn winds by meteorologists and climatologists, and, regardless of name, can occur in most places on the leeward side of a nearby mountain range. Deze pagina is voor het laatst bewerkt op 11 sep 2017 om 16:27. De tekst is beschikbaar onder de licentie. As is the case with any wind that descends down the side of a mountain range, these winds are warm and dry. Updated April 28, 2017. The counterclockwise wind flow around the low and the clockwise wind flow around the high work together to produce gusty westerly winds between the systems. The Chinook Winds is the resident wind quintet of the Great Falls Symphony in Montana. Hoewel de hoge temperatuur de sneeuw uiteindelijk zal doen smelten, wordt deze door de harde wind eerst opgewaaid wat eveneens verkeershinder geeft. Een (meestal hard waaiende) chinook kan 's winters de temperatuur in vrij korte tijd enige tientallen graden dramatisch doen stijgen: van bijvoorbeeld -20 °C naar +10 °C of zelfs +20 °C in een paar uur. The term "Chinook wind" is named after the Chinook Indians that traditionally inhabited the Pacific Northwest region along the Columbia River in Oregon and Washington State. Chinook winds are most common in a region called the Livingston Box, a broad zone extending from north central Montana to southeast Wyoming, centered near Livingston, Montana. Chinook winds are common in Colorado and New Mexico, as well as in Alberta and even the Northwest Territories. Door deze condensatie wordt de lucht steeds droger en tegelijkertijd komt de latente warmte vrij uit het vocht. Montana, in particular, has a significant amount of föhn winds across much of the state during the winter months, but particularly coming off the Rocky Mountain Front in the northern and west-central areas of the state. The winds are caused by moist weather patterns, originating off the Pacific coast, cooling as they climb the western slopes, and then rapidly warming as they drop down the eastern side of the mountains. Its name, Chinook, is from the Native American Chinook people of Washington state. Their programs include classic wind quintet literature, works featuring local composers and artists, and unique arrangements of popular songs—all executed with a captivating sense of … Professor Paul Thursday- The Strongest Winds Ever Recorded. The Chinook usually begins with a sudden change in wind direction towards the west or southwest, and a rapid increase in wind speed. Then, as the winds descend down the eastern slopes, the air is compressed and warms. Deze verhoogde temperatuur kan een aantal dagen aanhouden waarna deze weer naar het lage niveau terugvalt.

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