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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.
San Diego on average has 146 sunny days and 117 partly cloudy days a year. The average annual precipitation is less than 12 inches (30 cm), resulting in a borderline arid climate. Rainfall is strongly concentrated in the cooler half of the year, particularly the months December through March, although precipitation is lower than any other part ...
Average high temperatures are in the lower 80's F (26-28 C) with overnight lows in the lower 60's F (15-17 C). During this season, there is essentially no rainfall, and both July and August average less than 0.05 of an inch (1.27 mm) of monthly precipitation. The winter wet season normally runs from November through April.
National Weather Service Forecast Office, Kansas City/Pleasant Hill. Retrieved 29 August 2016. ^ "NOWData: Las Vegas Area monthly summarized data, 1981–2010, mean of monthly average temperatures". National Weather Service Forecast Office, Las Vegas, NV.
And while Downtown Los Angeles records slightly warmer average highs in August than in September , its warmest average September day (mean maximum) is 99.4 F, the highest of the calendar year.
The man-made lake created by Hoover Dam reached extremely low levels in July of 2022 at 1,041 feet. Levels as of Friday, April 12, 2024, were 33 feet higher, near 1,074 feet, and were 28 feet ...
While reaching just above average was good news, the current snowpack pales in comparison to April 2023, when the Sierra snow water content stood at 237% of average after a barrage of atmospheric ...
Droughts in California. The historical and ongoing droughts in California result from various complex meteorological phenomena, some of which are not fully understood by scientists. Drought is generally defined as "a deficiency of precipitation over an extended period of time (usually a season or more), resulting in a water shortage." [1]