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The coldest month on record at Vancouver International Airport was January 1950 when an Arctic air inflow moved in from the Fraser Valley and remained locked over the city, with an average low of −9.7 °C (14.5 °F) and an average high of only −2.9 °C (26.8 °F), making for a daily average of −6.3 °C (20.7 °F), 10 °C (18 °F) colder ...
This is a list of cities by average temperature (monthly and yearly). The temperatures listed are averages of the daily highs and lows. Thus, the actual daytime temperature in a given month may be considerably higher than the temperature listed here, depending on how large the difference between daily highs and lows is.
The island of Taiwan lies across the Tropic of Cancer, and its climate is influenced by the East Asian Monsoon. Northern Taiwan has a humid subtropical climate , with substantial seasonal variation of temperatures, while parts of central and most of southern Taiwan have a tropical monsoon climate where seasonal temperature variations are less ...
Coastal British Columbia has a more temperate climate, with a mild and rainy, cloudy winter. On the east and west coasts, average high temperatures are generally in the low 20s °C, while between the coasts, the average summer high temperature ranges from 25 to 30 °C (77 to 86 °F), with temperatures in some interior locations occasionally ...
Snowfall and frigid weather stranded thousands of people across four countries. At least 85 people in Taiwan died from hypothermia and cardiac arrest following a sudden drop in temperature during the weekend of January 22–24. The cold claimed a further fourteen lives in Thailand, and snowstorms resulted in six deaths across Japan.
Weather events in Taiwan (1 C, 1 P) Pages in category "Climate of Taiwan" The following 3 pages are in this category, out of 3 total.
Climate data for Richmond (Vancouver International Airport) Climate ID: 1108447; coordinates ; elevation: 4.3 m (14 ft); 1991–2020 normals, extremes 1898–present [a] Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
The climate of Asia is dry across its southwestern region. Some of the largest daily temperature ranges on Earth occur in the western part of Asia . The monsoon circulation dominates across the southern and eastern regions, due to the Himalayas forcing the formation of a thermal low which draws in moisture during the summer.