![]() ![]() The summer dry season normally runs from May through October, when clear skies, hot temperatures, and very little change in sensible weather occur from day to day. While the typical dry-summer and wet-winter pattern typical of most Mediterranean climates is part of the climate of Los Angeles, precipitation annually is lower than in many typical Mediterranean climates, giving it semi-arid characteristics. ![]() Los Angeles has a hot-summer Mediterranean climate ( Köppen Csa), with hot, dry summers, and mild-to-warm winters, with increased precipitation. The primary weather station for Los Angeles is located near downtown at the University of Southern California campus, and this article refers primarily to climate data generated by this station as representative of the Los Angeles metropolitan area as a whole. The two northernmost cities in Los Angeles County, Palmdale and Lancaster, frequently receive snow in the winter due to their altitude of approximately 2,500 feet (760 m), while their summers are hotter than the rest of the county.Ĭlassifications Los Angeles Climate according to major climate systems The Los Angeles area contains microclimates, where daytime temperatures can vary as much as 36 ☏ (20 ☌) between inland areas such as the San Fernando Valley or San Gabriel Valley, and the coastal Los Angeles Basin. Under the modified Köppen climate classification, the coastal areas are classified as Csb, and the inland areas as Csa. It is characterized by seasonal changes in rainfall-with a dry summer and a winter rainy season. It is classified as a Mediterranean climate, which is a type of dry subtropical climate. The climate of Los Angeles is mild to hot year-round, and mostly dry. Downtown Los Angeles on a typically sunny day, but with unusual atmospheric clarity. ![]()
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