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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 University of Victoria. [32] The Victoria Airport, 25 km (16 mi) north of the city, receives about 45% more precipitation than the city proper.
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. [9]
Rainfall in Victoria increases from south to the northeast, with higher averages in areas of high altitude. Mean annual rainfall exceeds 1,800 millimetres (71 inches) in some parts of the northeast but is less than 280 mm (11 in) in the Mallee. Rain is heaviest in the Otway Ranges and Gippsland in southern Victoria and in the mountainous ...
The blue numbers are the amount of precipitation in either millimeters (liters per square meter) or inches. The red numbers are the average daily high and low temperatures for each month, and the red bars represent the average daily temperature span for each month. The thin gray line is 0 °C or 32 °F, the point of freezing, for orientation.
[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 ...
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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.