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Due to the rain shadow effect of the nearby Olympic Mountains, Victoria is the driest location on the British Columbia coast and one of the driest in the region. Average precipitation amounts in the Greater Victoria area range from 608 mm (23.9 in) [ a ] at the Gonzales observatory [ 31 ] in the City of Victoria to 661 mm (26.0 in) at the ...
Lying in the rain shadow of both the Vancouver Island Ranges and the Olympic Mountains, Saanich Peninsula is the driest part of Vancouver Island. [citation needed] The driest recording station in the provincial capital city of Victoria averages only 635 millimetres (25 in) of precipitation annually. Precipitation increases from east to west ...
Most rain falls in winter, though heavy summer falls can occur, the most famous of which was the thunderstorm that dumped 133.2 millimetres (5.24 in) on Nhill in mid-January 1974. [ citation needed ] Temperatures are hot in summer, ranging typically from a maximum of 30 °C (86 °F) to a minimum of 14 °C (57 °F), whilst extremes can be as ...
In Victoria, the annual average temperature is 11.2 °C (52.2 °F), the warmest in Canada. [ 8 ] Due to the blocking presence of successive mountain ranges, the climate of some of the interior valleys of the province is semi-arid with certain locations receiving less than 300 mm (12 in) in annual precipitation.
[39] [7] Tofino saw only a quarter of its usual rainfall between July and Oct 21; Vancouver had less than 10% of its usual rainfall; and Victoria, British Columbia recorded only 2 millimetres of rain instead of its normal average of 132 mm. [40] In Prince George, British Columbia, the confluence of the Fraser and Nechako Rivers had nearly run ...
Canada's annual average temperature over land warmed by 1.7 °C (3.1 °F) between 1948 and 2016. The rate of warming is highest in Canada's north, the Prairies, and northern British Columbia. The country's precipitation has increased in recent years and wildfires expanded from seasonal events to year-round threats.
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The 2021 Pacific Northwest floods were a series of floods that affected British Columbia, Canada, and parts of neighboring Washington state in the United States. The flooding and numerous mass wasting events were caused by a Pineapple Express, a type of atmospheric river, which brought heavy rain to parts of southern British Columbia and northwestern United States.