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The climate of California varies widely from hot desert to alpine tundra, depending on latitude, elevation, and proximity to the Pacific Coast. California 's coastal regions, the Sierra Nevada foothills, and much of the Central Valley have a Mediterranean climate, with warmer, drier weather in summer and cooler, wetter weather in winter.
California land area totals 99,813,760 or roughly 100 million acres, so since 2000, the area that burned annually has ranged between 90,000 acres, or 0.09%, and 1,590,000 acres, or 1.59% of the total land of California. [2] During the 2020 wildfire season alone, over 8,100 fires contributed to the burning of nearly 4.5 million acres of land.
Archived from the original on 29 June 2011. Retrieved 22 December 2010. Caçador has the lowest recorded temperature, officially, in Brazil, of −14 °C in 1952. Another record, unofficial, of −17.8 °C in 1996-06-29, at the summit of Morro da Igreja, Urubici, also in Santa Catarina, would give the record to this locality.
Temperature. The average yearly temperature is around 23 °C (73 °F) during the day and 16 °C (61 °F) at night (one of the warmest temperature averages in Europe). In the coldest month – January – the typical maximum temperature ranges from 12 to 20 °C (54 to 68 °F) during the day and the minimum from 6 to 12 °C (43 to 54 °F) at night.
Show comments. (Reuters) -More than 6,000 firefighters in California's Central Valley continued to battle the largest blaze in the U.S. on Saturday, which burned its way into the history books as ...
Throughout recent recorded history, California has experienced periodic droughts, such as 1841, [21] 1864, 1895, 1924, 1928–1935, 1947–1950, 1959–1961, 1976–1977, 1986–1992, 2007–2009, [22][21] and 2011–2017, and 2020–2022. [5] Since 1841, the following dry years have had significantly below-average precipitation.
Cooler climate causes Carboniferous rainforest collapse. 251.9. Permian–Triassic extinction event. 199.6. Triassic–Jurassic extinction event, causes as yet unclear. 66. Perhaps 30,000 years of volcanic activity form the Deccan Traps in India, or a large meteor impact. 66. Cretaceous–Paleogene boundary and Cretaceous–Paleogene extinction ...
Pre-Holocene (1.5 Ma) The time from roughly 15,000 to 5,000 BCE was a time of transition, and swift and extensive environmental change, as the planet was moving from an Ice age, towards an interstadial (warm period). Sea levels rose dramatically (and are continuing to do so), land that was depressed by glaciers began lifting up again, forests ...