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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.
Temperatures at sea level generally range from highs of 84–88 °F (29–31 °C) during the summer months to 79–83 °F (26–28 °C) during the winter months.
It is common practice to follow the section sign with a non-breaking space so that the symbol is kept with the section number being cited. [ 1 ] [ 7 ] : 212, 233 The section sign is itself sometimes a symbol of the justice system, [ a ] [ citation needed ] in much the same way as the Rod of Asclepius is used to represent medicine.
In July 2009 Seattle's all-time high temperature was broken by a margin of 4 degrees Fahrenheit (2.2 Celsius), [14] then broken again by a margin of 5 F (2.8 C) in June 2021. The single-day precipitation record set in October 2003 saw higher precipitation by nearly 2 inches (50mm) than any other day on record.
Cyprus from Space Solar Map of the Island Mountainous Geography on the northern coast Seacoast from Southern Side Sunsets on the island Seacoast from Eastern side. Cyprus has a subtropical climate, Mediterranean and semi-arid type (Csa and BSh) according to Köppen climate classification, [1] [2] with very mild winters on sea level and warm to hot summers.
Canada's annual average temperature over land warmed by 1.7 degrees Celsius 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.
Monsoons are large-scale sea breezes which occur when the temperature on land is significantly warmer or cooler than the temperature of the ocean. Most summer monsoons or southwest monsoons (Filipino: Habagat) have a dominant westerly component and a strong tendency to ascend and produce copious amounts of rain (because of the condensation of water vapor in the rising air).
The United Kingdom straddles the higher mid-latitudes between 49° and 61°N on the western seaboard of Europe.Since the UK is always in or close to the path of the polar front jet stream, frequent changes in pressure and unsettled weather are typical.
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