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squamish

A squamish is a strong and often violent wind occurring in many of the fjords, inlets and valleys of British Columbia. Squamishes occur in those fjords oriented in a northeast-southwest or east-west direction where cold polar air can be funneled westward, the opposite of how the wind generally flows on the Coast. These winds in winter can create high windchills by coastal standards of −20 to −30 °C. They are notable in Jervis, Toba, and Bute Inlets and in Dean Channel and the Portland Canal. Squamishes lose their strength when free of the confining fjords and are not noticeable more than 25 km offshore. On the Lower Mainland and Eastern Vancouver Island of British Columbia, where they are mainly referred to as outflow winds, they are noticeable especially in the winter, when a cold Arctic air mass holding in the high plateau country of the interior flows down to the sea through the canyons and lower passes piercing the Coast Mountains and crossing the Strait of Georgia. The town of Squamish, British Columbia, is named for the wind, and upper Howe Sound, just off the Squamish River estuary, is known widely in the sailboarding world for its excellent, steady winds.

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