What Climate Zone Am I In California – California’s climate varies greatly from hot desert to alpine tundra, depending on latitude, elevation, and proximity to the Pacific coast. The coastal regions of California, the Sierra Nevada mountains, and much of the Central Valley have a Mediterranean climate, with hot, dry summers and cool, cold winters. The influence of the ocean generally moderates extreme temperatures, creating warm winters and cooler summers in coastal areas.
The cold coast of California Currt, affected by the upwelling of cold water from the low land, often creates summer fog around the coast, creating a warm summer Mediterranean climate (Csb Köpp climate). Inland, the climate becomes more continental, and in some areas semi-arid (Köpp BSk), with cold winters and very hot summers. The lower inland valleys, especially the Ctral valley, have a subtropical Mediterranean climate (Köpp Csa), with low temperatures but well-defined summers and a rainy and foggy winter season.
What Climate Zone Am I In California
The temperature between the near coast and the lower valleys in the south is about 7 °F (4 °C) in winter, and the coast gets warmer, and in summer about 25 °F (14 °C), with a warm interior. . . For example, the average daily high in San Francisco in July and August is between 17 and 20 °C (62 °F and 68 °F).
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And Walnut Creek, about 20 miles (32 km) inland, average daily highs in July and August are 90°F (32°C)—a temperature increase of more than one degree (Fahrenheit) per mile.
In Southern California, the temperature range is 4°F in winter and 23°F (2°C and 13°C) in summer. In Santa Monica Beach, the average high in August is 75°F (24°C), while in Burbank, about 10 miles (16 km) inland, the average high in August is 95°F (35°C): Rising temperatures to two degrees Fahrheit per mile.
During the coldest winter months (October-March), the Coachella Valley consistently has the warmest winter temperatures anywhere west of the Rocky Mountains. East of Los Angeles, the Gateway Cities, and parts of the San Gabriel Valley average the warmest winter temperatures (72°F, 22°C) in the entire western United States. 11°C) across West Palm Springs, a city in the Coachella Valley, with an average high/low temperature of 75°F/50°F/63°F (24°C/10°C/17). °C) respectively during the winter season from November to April.
The southwest end, around San Diego, has a sub-arid or semi-arid climate (Kopp BS) since the winters are dry there.
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The southeastern regions have a hot and dry climate (Kopp BWh), similar to that of the desert. On the north side of the Mojave Desert in the eastern part of the state is Death Valley, which has recorded some of the hottest temperatures in the world. It is common in summer for temperatures in the valley to exceed 49 °C (120 °F). The highest temperature reliably recorded in the world,
134°F (56.7°C), was recorded in Death Valley on July 10, 1913. A temperature of 130°F (54°C) or higher was recorded as recently as 2005. The average July 24-hour temperature is 101.8°F (38.8°C) (1981-2010 NCDC standard).
The highest temperature ever recorded in California was 134°F (57°C) in Death Valley on July 10, 1913. This is also the highest temperature ever recorded on Earth. The minimum was -43 °C (-45 °F) in Boca on January 20, 1937.
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Strong winds from the oceans also bring moisture, and the northern parts of the region generally receive more annual rainfall than the southern parts. California’s mountain range also affects the climate: moist air from the west cools as it rises over the mountains, shedding moisture; some of the wettest parts of the region are on the west-facing mountain slopes. Northwest California has a temperate climate with annual precipitation ranging from 15 inches (380 mm) to 50 inches (1,300 mm). Some areas of the Coast Redwood forest receive more than 100 inches (2,500 mm) of precipitation annually.
The Ctral Valley has a wide range of rainfall. The northern parts of the Ctral basin receive a lot of rain from winter storms that flow in from the Pacific Northwest, while the southern regions of the Ctral basin are almost desert-like due to the lack of rain. Some parts of the valley are occasionally filled with thick fog (locally known as “tule far”).
The high mountains, including the Sierra Nevada, Cascade Range, and Klamath Mountains, have a mountainous climate with snow in the winter and mild to moderate heat in the summer. Lake Tahoe, Mammoth Lakes, and Mount Shasta resorts regularly receive more than 10 feet (3.0 m) of snow in a season, and in some years significantly, leading to, for example, the race the annual Fourth of July snow.
On the eastern side of the mountains there is a dry rain shadow. California’s desert climate is located east of the high Sierra Nevada and the Transverse and Peninsular Ranges of southern California. The low desert east of the mountains of southern California, including the Imperial and Coachella Valleys and the bottom of the Colorado River, is part of the Sonoran Desert, with the least winter frost; The high desert of eastern California, including the Mojave Desert, the Ows Valley, and the Modoc Plateau, is part of the Great Basin region, which has a more continental climate. During the summer months, especially from July to early September, the region is affected by the Mexican Monsoon (also known as the “Southwest Monsoon”), which brings moisture from the tropical Pacific, the Gulf of California, and/or the Gulf of Mexico. towards the desert sea, causing brief thunderstorms but often thunderstorms, especially in mountainous areas.
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Despite its long coastline, California is not prone to tropical storms. Due to the cold California Currt from the North Pacific Ocean and the fact that hurricanes must “move” westward, California has experienced two tropical storms in recorded history, a storm that made landfall in 1939 and dumped heavy rain over the Los Angeles area. and inland deserts and tropical storms Nora, Hurricane Dolores, and Hurricane Linda (2015) The remnants of tropical systems will hit California repeatedly, every few years.
The SO cycle has a significant effect on the age of precipitation and snow patterns in California, especially during the winter and spring seasons. During the El Niño phase, the jet stream moves across southern California, allowing for hot temperatures and heavy rain, especially in the southern parts of the state. During the La Niña phase, the jet stream is farther north, so the northern parts of California are wet, while the southern part is cold and dry.
Summers in California can have daytime temperatures above 100 °F (38 °C) and less than 0.3 inches (7.6 mm) of monthly precipitation, especially in southern areas. This makes them vulnerable to forest fires. These can be life-threatening and prompt evacuation. Wildfires are rare on the coast because of cooler, wet summers, but they can occur in the fall when the marine layer thins, causing temperatures to warm and humidity to drop significantly. High school students across the United States have free digital access to The New. York Times through September 1, 2021.
These maps show growth zones (also known as resistance zones) in two time periods: historical and projected. The zones are based on the coldest annual temperature for each location averaged over a 30-year period. Gardeners and home gardeners use the zones on these maps to tell them which plants will be successful in their area.
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Globally, 2020 tied 2016 as the hottest year on record. These temperature changes can affect which plants can grow successfully in the area. Some plants will now be able to grow in regions further north because it is now warmer, and some will not be able to grow in their normal regions because it is too hot. This is also true for plant pests that can now find new habitats further north during the winter and attack plants there.