British Columbia Mountains Ripple

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During winter, on the coast, rainfall, sometimes relentless heavy rain, dominates because of consistent barrages of cyclonic low-pressure systems from the North Pacific. Average snowfall on the coast during an average winter is between 25 and 50 cm (9. 8 and 19. 7 in), but on occasion (and not every winter) heavy snowfalls with more than 20 cm (7. 9 in) and well below freezing temperatures arrive when modified arctic air reaches coastal areas, typically for short periods, and can take temperatures below −10 °C (14 °F), even at sea level, and arctic outflow winds can make wind chill temperatures at or even below −17. 8 °C (0. 0 °F) for a couple of mornings. While winters are very wet, coastal areas are generally milder and dry during summer under the influence of stable anti-cyclonic high pressure. Southern Interior valleys are hot in summer; for example in Osoyoos the July maximum temperature averages 31. 7 °C (89 °F) the hottest month of any place in Canada, this hot weather sometimes spreads towards the coast or to the far north of the province. Temperatures often exceed 40 °C (104 °F) in the lower elevations of valleys in the Interior during mid-summer, with the record high of 44. 4 °C (111. 9 °F) being held in Lytton on July 16, 1941.

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Photogallery British Columbia Mountains Ripple:


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple


British Columbia Mountains Ripple