Climate of Los Angeles

Temperatures and Seasons

Downtown is a hot-summer mediterranean climate (Köppen Csa) but only narrowly above the semi-arid climate (BSh) with precipitation being limited even during winter.

Summer

Summers are warm to hot, and nearly completely dry. The summer temperature pattern usually begins in late June or early July, and lasts through October or November, although it may start as early as May. In August, the average high/low at the University of Southern California downtown campus are 84.8 °F (29.3 °C) and 65.6 °F (18.7 °C). The same figures at the LAX airport, approximately 12 miles (19 km) to the southwest and near the ocean, are 76.6 °F (24.8 °C) and 64.2 °F (17.9 °C). However, temperatures across the region sometimes exceed 90 °F (32 °C) during the summer. This happens when an atmospheric high-pressure area becomes dominant over the Great Basin of Nevada and Utah (a frequent occurrence), and the resulting offshore flow of the atmospheric air mass shuts off the normal coastal sea breeze in Los Angeles. July, August and September are the hottest months, with September holding the all-time record of 113 °F (45 °C). Skies are nearly constantly sunny, unless interrupted in late spring and early summer by the June Gloom pattern, which is unpredictable year-to-year.

Winter

Winters are mildly cool to warm, with average high temperatures at the Downtown/USC weather station of 68 °F (20 °C) and lows of 48 °F (9 °C), with occasional rain. Temperatures across the coastal basin rarely drop below 45 °F (7 °C), although light frost does occasionally form during cooler nights, at least in areas removed from the direct influence of the coastal air (approximately 5 miles (8 km) inland from the beach). However, high pressure systems over the deserts often bring the Santa Ana winds, resulting in hot, dry, and dusty days. Temperatures reach into the 80 to 90 °F (27 to 32 °C) range routinely during Santa Ana Winds even in December and January. Almost every winter season, temperatures reach above 90 °F (32 °C) at least once during a Santa Ana-type event. Sunny skies characteristically dominate the weather pattern even in the winter season.

Spring and Autumn

Spring and autumn hardly exist as such in this climate. Summer temperature patterns of 75 to 90 °F (24 to 32 °C) highs and 60 to 70 °F (16 to 21 °C) lows usually persist until mid-November. Likewise, the "winter-season" temperature pattern of 65 to 75 °F (18 to 24 °C) highs and 45 to 60 °F (7 to 16 °C) lows may last through April or May, periodically interrupted by hot Santa Ana wind events for up to a week at a time. The rainy season almost always ends by mid-May. June is normally a transitional month of less-volatile temperatures between 60 and 80 °F (16 and 27 °C), with increased cloudy days and the disappearance of the Santa Ana winds.

Rainfall

Rainfall, on average, is quite low. Most rain occurs during winter and early spring, typical of a Mediterranean climate. However, the amount received is usually lower than in other Mediterranean climates. The first sporadic rainfall of the rainy season usually occurs in October or November, with rain becoming more common December through February. February, on average, is the wettest month. The rains then taper off in March, and April and May usually see only one or two light rains. However, the timing and volume of rains in the winter is far from predictable. After a significant rain, the region's air is cleared of the usual atmospheric haze as well as man-made smog, giving exceptionally clear views across the giant metropolis.

Most cold fronts and depressions spun off by the polar low, the strong winter seasonal low-pressure area in the Gulf of Alaska, fail to carry significant precipitable moisture as far south as Los Angeles, resulting in the region's relatively low average rainfall amount of 12–15 inches (300–380 mm) even in normal years. However, a "normal" year rarely occurs, since rainfall in Los Angeles is subject to the position and strength of the jet stream, and the strength of the Gulf of Alaska low. Some years, a well-developed series of cold fronts moves into the area with relatively short separation between each, bringing intermittently rainy periods to Los Angeles for several weeks at a time. If this pattern persists in a rainy season, significantly above-average precipitation will be received. Other years, especially in the drought years of 2012–2015, a blocking region of atmospheric high pressure over the eastern Pacific Ocean, between Alaska and the Pacific Northwest, diverts the jet stream and its flow of cold fronts far to the north through Canada and down into the U.S. Midwest, leaving the U.S. west coast and especially Los Angeles under warm and dry conditions for weeks to months at a time.

Because the rainy season begins in late fall and ends in early spring, precipitation is measured using the water year instead of the calendar year, to give an accurate picture of each rainy season's precipitation amounts. Each water year begins October 1 and ends the following September 30, during the driest part of the year.

Sometimes rainfall can occur in the summer from westward-straying monsoon thunderstorms, but this is unusual. Even less common is rain from remnants of dissipating eastern Pacific hurricanes. Los Angeles averages only 15.1 inches (384 mm) of precipitation per year, and this is lower at the coast and higher in the mountains and foothill cities. Snow is extremely rare in the Los Angeles basin, but the nearby San Gabriel Mountains and San Bernardino Mountains typically receive snow every winter season. The greatest snowfall recorded in downtown Los Angeles was 2 inches (5 cm) on January 15, 1932.

El Niño–Southern Oscillation

Historically-speaking, the warm-phase of an El Niño–Southern Oscillation (ENSO) regime typically coincides with above average precipitation across Southern California. The above average sea-surface temperatures in the equatorial Pacific Ocean are largely responsible for this as the ocean acts as a rich moisture source for tropical moisture to advect towards the North American continent in atmospheric river events. Prior to the strong El Nino of 2015-2016, the previous two strong El Niño events in 1982-83 and 1997-98 coincided with well-above average precipitation across Southern California. While some measurements suggest the 2015-2016 El Niño was the strongest on record since 1950, Southern California received below average precipitation contrary to what the Climate Prediction Center predicted leading up to the winter months. While scientists have long agreed the intensity and timing of the winter precipitation pattern in Los Angeles is more complex than just analyzing the warm/cool phase of ENSO, the fact that Los Angeles received below average precipitation during the strong El Niño event of 2015-2016 will be the subject of numerous research studies among climate scientists.

Coastal Basin

The Los Angeles Basin, composed of the coastal plain surrounded by mountains, is generally the coolest in summer and mildest in winter. Overall, it receives less rainfall than the surrounding valleys and mountains.

LAX

LAX airport and its surroundings (Westchester and El Segundo, as well as Santa Monica, Venice, and the immediately surrounding neighborhoods) are generally the coolest part of the region in the summer, as they receive a near-constant sea breeze. Santa Monica and its environs may be 10 to 15 °F (6 to 8 °C) cooler than areas only 5 miles (8.0 km) further inland. Under the Köppen climate classification LAX has a semi-arid climate due to its modest winter rainfall and mild mean temperatures.

Santa Monica

Santa Monica has mean temperatures low enough for its precipitation numbers to still retain a cool-summer mediterranean climate (csb).

Culver City and Palms Area

Culver City, Palms, and surrounding areas are only a few miles inland from Santa Monica and the beach, but reach temperatures up to 10 degrees (F) warmer on average in the summer. Culver City has a semi-arid climate that is still significantly moderated by the Pacific trade winds keeping averages mild compared to areas farther inland.

Long Beach

Long Beach, located in the coastal basin about 20 miles (32 km) to the south of downtown Los Angeles, has a coastally-influenced climate, but is not as cool as Santa Monica, or the Westside, or the South Bay during the summer. Long Beach sits on a south-facing section of coast, and does not receive as much sea breeze cooling from the prevailing westerly/south-westerly winds (as these winds may pass over the Palos Verdes Peninsula, San Pedro, and the twin ports first). Long Beach's high temperature can compete with those of downtown Los Angeles. Locations further north in Long Beach, which stretches over 8.5 miles (13.7 km) northward from the water, can be considerably warmer than Long Beach's coast and airport weather station.

San Fernando Valley

The San Fernando Valley is known for significantly higher temperatures than the coastal basin. Canoga Park and Woodland Hills, in the south-west end of the valley, typically record the highest temperatures. The all-time high of 116 °F (47 °C) nearly rivals the record high temperatures of Phoenix, Arizona (122 °F (50 °C)) and Palm Springs (123 °F (51 °C)). The city of Burbank, at the eastern end of the Valley, is also known for being significantly hotter than downtown Los Angeles, which is only 9 miles (14 km) to the south. During winter both the Canoga Park and Burbank weather stations are significantly wetter than some coastal stations and thus retain hot-summer mediterranean climates (csa). By comparison, Canoga Park has quite cool summer nights, in contrast to many other interior Southern California areas.

North/Central Orange County

The climate of Santa Ana, the county seat of Orange County, as well as Anaheim, both in north-central Orange County, are quite similar, and typical of locations on the coastal plain 10 to 15 miles (16 to 24 km) inland from the beach. Whilst Santa Ana sits firmly on the border between the semi-arid and the hot-summer mediterranean climate, Anaheim is firmly a semi-arid climate with very low precipitation for the Los Angeles metropolitan area.

Records

In downtown Los Angeles, weather records began on July 1, 1877. The highest temperature recorded in downtown Los Angeles was 113 °F (45 °C) on September 27, 2010. The lowest temperature was 28 °F (−2 °C) on January 7, 1913 and on January 4, 1949. The wettest “rain year” from July to the following June was 1883/1884 with 38.18 inches (969.8 mm), and the driest 2006/2007 with 3.21 inches (81.5 mm). The greatest rainfall in one month was 15.80 inches (401.3 mm) in December 1889, which also had the most days – twenty – receiving at least 0.01 inches (0.3 mm) of rain. The greatest rainfall in 24 hours was 5.68 inches (144.3 mm) on March 2, 1938.

At the Los Angeles International Airport, the highest recorded temperature was 110 °F (43 °C) on September 26, 1963. The lowest temperature was 27 °F (−3 °C) on January 4, 1949. The wettest year was 1983 with 29.46 inches (748 mm) and the driest year was 1947 with 2.95 inches (74.9 mm). The greatest rainfall in one month was 13.79 inches (350 mm) in February 1998. The greatest rainfall in 24 hours was 5.60 inches (142.2 mm) on November 21, 1967.

In Long Beach, the highest recorded temperature was 111 °F (44 °C) on October 16, 1958, and October 15, 1961, and again on September 27, 2010. The lowest temperature was 21 °F (−6 °C) on January 20, 1922. The wettest year was 1978 with 27.67 inches (703 mm). The driest year was 2002 with 2.63 inches (66.8 mm). The greatest rainfall in one month was 14.50 inches (368 mm) in January 1969, including a record 24-hour rainfall of 6.71 inches (170.4 mm) on January 20 that month. The record snowfall was 1.5 inches (3.8 cm) in January 1949.

Santa Ana Winds

The Santa Ana winds are strong, extremely dry offshore winds that characteristically sweep across Southern California and northern Baja California during late fall into winter season. They range from hot to cold, depending on the prevailing temperatures in the source region, the Great Basin and upper Mojave Desert. Nevertheless, the winds are notorious for causing hot, dry weather due to compressional heating of the lower atmosphere.

Notable Santa Ana windstorms happen several times a year between fall and spring. Once every several years a strong windstorm causes significant damage, toppling or uprooting large old trees and damaging structures across the region.

Heavy Rains, Landslides, and Debris Flows

While overall precipitation is low, the rain that does fall sometimes comes in brief heavy storms. Combined with steep mountain slopes and recent burn areas from wildfires, these heavy rains often cause landslides and debris flows in foothill areas, damaging structures and blocking roads.

Thunderstorms, Lightning, and Tornadoes

Textbook cumulonimbus-formed summer thunderstorms are extremely rare in Los Angeles, because the atmosphere over the coastal basin is generally too stable and dry, especially during summer, to allow the strong vertical development necessary for mature cumulonimbus clouds. Full, mature thunderstorms can develop in the surrounding deserts and mountains during the summer North American Monsoon, but very rarely over the Los Angeles metropolitan region and coastal basin. This atmospheric stability is largely due to the cool and persistent marine layer, which is fueled by the constant influx of cold Pacific water via the California Current. Summer thunderstorms that do manage to form on the coastal basin are typically associated with tropical cyclones, which can bring enough tropical heat and moisture to overcome the cool marine layer, destabilizing the atmosphere.

Though still relatively rare, thunderstorms most often occur during warm southerly-flow winter rain storms. These warm storms are different from the typical northwesterly cold fronts that bring most of the region's winter precipitation. Atmospheric instability caused by these warm winter storm systems allows the formation of small, weak, isolated thunderstorms, which tend to move across the area quickly, producing a few rumbles of thunder, and soon dissipate back into the larger rain storm system. Occasionally, these bring impressive displays of lightning, hail, and damaging winds to small localities within the region. Small, weak, isolated tornadoes can occur during these events, but are exceedingly rare. Likewise, weak-to-moderate-strength waterspouts may form over the ocean (typically off the stretch of coast between Long Beach and Huntington Beach) during warm winter storms, but again, this is very rare.

Sea temperatures

The average annual temperature of the sea is 63 °F (17 °C), from 58 °F (14 °C) in January to 68 °F (20 °C) in August.