. . . . "These appear to be temperatures, not wind chill corrections."@en . "A squamish (also known as an Arctic outflow wind in winter months) 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\u2013southwest or east\u2013west 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 \u221220 to \u221230 \u00B0C (\u22124 to \u221222 \u00B0F). 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."@en . . "1107496"^^ . . . . . . . . . . . . "Squamish (vent)"@fr . . . . . . . . "Squamish (wind)"@en . . . . . "3050"^^ . . . . . "A squamish (also known as an Arctic outflow wind in winter months) 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\u2013southwest or east\u2013west 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 \u221220 to \u221230 \u00B0C (\u22124 to \u221222 \u00B0F). 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. In Northern Washington including Lynden and Bellingham, and Lower Mainland, including Eastern Vancouver Island, of British Columbia, 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 windsurfing and kiteboarding worlds for its excellent, steady winds. During the Christmas season of 1996, a major blizzard which brought record snowfalls to the Lower Mainland and Eastern Vancouver Island was followed up by hurricane-force winds pouring west through the towns of the Fraser Valley, as the coastal system's strength \u2013 which had brought the snow \u2013 was forced back by the breaking of the interior's cold air mass. Intense outflow winds are relatively common year-round (during stormy weather, and sometimes fair) in the Upper Fraser Valley, particularly on Sumas Prairie between Abbotsford and Chilliwack, and farther upriver towards the mouth of the Fraser Canyon. Known by different names in each region up the Coast, outflow winds or squamishes are also major maritime threats off the openings of the major fjords and up their narrow, deep lengths. Queen Charlotte Strait in particular is known for heavy winds coming out of the mouth of Knight Inlet, at the upper east end of the strait."@en . . . . . . "July 2015"@en . . . . . . . . "1116326961"^^ . . . . . "Le squamish est un vent fort et souvent violent qui souffle parfois en hiver dans de nombreux fjords, baies et vall\u00E9es de la province de Colombie-Britannique au Canada, ce vent est cons\u00E9cutif \u00E0 une pouss\u00E9e d\u2019air arctique. De mani\u00E8re g\u00E9n\u00E9rale, les masses d'air en Colombie-Britannique proviennent de l'oc\u00E9an Pacifique, situ\u00E9 \u00E0 l'ouest de la province. Dans le sud-ouest de la province, ces masses d'air oc\u00E9aniques sont t\u00E9mp\u00E9r\u00E9es et humides. Il arrive cependant que de l'air froid arrive des zones arctiques, situ\u00E9es au nord, et se retrouve coinc\u00E9 par les pentes occidentales des Rocheuses canadiennes. Au fur et \u00E0 mesure de son accumulation, cet air est pouss\u00E9 de plus en plus vers le sud et se retrouve contraint \u00E0 s'engoufrer dans les nombreuses vall\u00E9es, globalement orient\u00E9es d'ouest en est, qui d\u00E9coupent la c\u00F4te montagneuse de la province. Ces vall\u00E9es (souvent des fjords) se retrouvent alors remplies avec un air arctique froid et sec, au lieu de l'air oc\u00E9anique temp\u00E9r\u00E9 et humide, causant des changements radicaux de la temp\u00E9rature. Ce ph\u00E9nom\u00E8ne, d'une fa\u00E7on g\u00E9n\u00E9rale, est appel\u00E9e une \u00AB pouss\u00E9e d'air arctique \u00BB. Lorsque l'air oc\u00E9anique arrive de l'ouest, il rencontre l'air froid, provoquant des chutes de neige et des \u00E9pisodes de gel. Et en chassant l'air froid en dehors de vall\u00E9es, il provoque un vent glacial appel\u00E9 \u00AB squamish \u00BB. Un tel vent s'observe notamment depuis la baie Howe (Howe Sound) vers le d\u00E9troit de G\u00E9orgie. Officiellement la m\u00E9t\u00E9o canadienne d\u00E9finit un squamish lorsque le refroidissement \u00E9olien qu'il provoque atteint la valeur de -20."@fr . . . . . "Le squamish est un vent fort et souvent violent qui souffle parfois en hiver dans de nombreux fjords, baies et vall\u00E9es de la province de Colombie-Britannique au Canada, ce vent est cons\u00E9cutif \u00E0 une pouss\u00E9e d\u2019air arctique."@fr . . . . .