Geography of southern California

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The San Gabriel Mountains, part of the Angeles National Forest in Los Angeles County, California

The geography of southern California refers to the geography of southern California in the United States.

Climate

Köppen climate types of southern California

Despite the popular image of California as a place of sunshine and perfect weather, the local climate can be very diverse, with some areas experiencing more extreme conditions. However, the weather in the region is usually mild, especially in the winter, and dry, with rainfall ranging from moderate in the coastal regions to almost none at all in the desert.[1]

Around the coastal areas, the weather does not vary as dramatically as it does inland. Climate is affected by factors such as latitude, topography, and proximity to water masses - primarily the Pacific Ocean, and southern California's mountain ranges. The Transverse Ranges and the Peninsular Ranges are key players in the region's climate.

Essentially, the mountain ranges separate southern California into two distinct climatic regions: The heavy-populated coastal area west of these mountains is the one most associated with the term "southern California" and is characterized by pleasant weather all-year round, without frequent heat spells in the summer and without low temperatures in winter. By comparison, the area east of the ranges, between the mountains and the borders with Nevada and Arizona, is dominated by the Sonoran Desert and the Mojave Desert and tends to be more arid and register more extreme temperatures in both summer and winter.[2]

Low clouds and fog

This is a common weather prediction for southern California. Due to the topographic features and proximity to the Pacific, southern California has its share of both low clouds and fog.[3]

Coastal fogs are frequently generated by interaction between seasonal inversion layers and the coastal marine layer, and may reach as far inland as 20 miles, butting up against inland mountains or coastal mountain ranges. While

ground fogs' to a dense almost "Tule fog
" (pronounced ˈtuːliː fog) in the Winter and Spring, depending on the interaction of cold air brought down from the local mountains and the warmer ocean air masses.

However, over the last few decades, clouds have become less prevalent on the coast, due to urban heat and climate change.[4] When compared with data from the 1970s, scientists discovered that the stratus cloud cover has decreased between 25% and 50%.[5]

"May Gray" and "June Gloom"

In contrast with the sunny summer, late spring in southern California is often overcast. This period, known to the locals as "May Gray" and "

La Niña pattern, usually foretell more gray days in the season.[7]

Santa Ana winds in California expand fires and spreads smoke over hundreds of miles, as in this October 2007 satellite image.

Wildfires

Because of the hot, dry and windy nature of southern California,

American West, increasing in temperature as they approach the ocean.[11][12]

Because natural wildfires are more likely to appear towards the end of long, dry summers, they have become a more serious problem in recent years because of climate change, which makes wildfires increasingly larger and more frequent.[13] Climate change has also widened the wildfire "season" from a few summer months to virtually the entire year.[14] At the same time, climate scientists are expecting that climate change will diminish the strength of the Santa Ana winds, potentially limiting its role in spreading wildfires.[15]

Physical geography

Other than the Pacific Coast, the Transverse Ranges and the Peninsular Ranges are the two most important physical landscapes in the region. Both ranges have their particular characteristics, from the trend of the mountains, to the different climates within each range.

The ellipse outlines the region of the California Transverse Ranges.

Transverse Ranges

The

San Bernardino County. They derive the name Transverse Ranges due to their east-west orientation, making them transverse to the general north-south orientation of most of California's coastal mountain ranges.[17]

Climate

The Transverse Ranges experience temperature differences from winter to summer of about 36 °F (20 °C). One factor contributing to this variability is the distance from the ocean: the eastern part of the Transverse Ranges is furthest from the coast and has the most drastic temperature variation, whereas the western part is closest to the ocean and therefore has less variance.[18]

The amount of precipitation of any area is affected by elevation, and topography influences temperature within elevation ranges. The higher the elevation, the lower the temperatures, and with lower temperatures come increased precipitation. The highest point of the Ranges is

rain shadow effect, when air flow inland from the ocean and it rises, it begins to cool and after it reaches the other side of the mountain it becomes warm and evaporates.[20] This is one of the reasons for the dry conditions in the Transverse Ranges that are furthest from the coast.[21] The Ranges are also affected by the Santa Ana winds, a regional wind system created when air is forced from a high pressure to a low pressure, causing air to move from inland towards the ocean. These dry winds usually originate at the eastern end of the Ranges.[9]

Geology

The

Sierra Nevada can be found.[23][24]

Composite ranges

These east-to-west running ranges include a variety of different mountains. Some mountains are steep like the San Gabriel Mountains. Other areas of the Transverse Ranges have a very low elevation like the Mojave Desert. The mountains ranges comprising the Transverse ranges include:[25]

Transverse Ranges

Urban interaction

The Peninsular Ranges are the southernmost mountains in the California Coast Ranges

People have taken full advantage of the Transverse Ranges. The Ranges create a number of coastal plains and valleys which have become densely populated because of their prime living conditions. These valleys include

Inland Valley
. The mountain ranges create recreation and living areas and have several ski resorts and provide several hiking and off-road vehicle use areas. Many people reside in the hills of the Transverse Ranges, where they may work locally or commute to work in more populated areas 'down the hill.' Such communities provide an alternative to city and suburban living in southern California.

Peninsular Ranges

The

Coast Ranges that run along the Pacific coast from Alaska to Mexico.[27] Elevations range from 500 ft to 11,500 ft (150 m to 3,500 m) and vegetation in these ranges varies from coastal sage scrub to chaparral, and from oak woodland to conifer forest
.

The Peninsular Ranges of

Sierra San Pedro Martir, Sierra de la Giganta, and Sierra de la Laguna. These ranges run from north to south.[29]

The Santa Ana Mountains are the largest natural landscape along the coast of southern California. These mountains peak at about 5,689 feet, on Santiago Peak.[30] This range starts in the north, in the Corona area heading southeast of the Puente Hills region.

Peaks of the Peninsular Ranges

The San Jacinto Mountains are located in the desert areas in the north and east side of southern California. They peak at about 10,833 feet.[31] They run from the San Bernardino Mountains southeast to the Santa Rosa Mountains. This mountain range is the northernmost part of the Peninsular Range.

The

Anza-Borrego portion of the Colorado Desert. The highest peak in the range is Toro Peak (8,717 feet).[32]

The

Sonora Desert
lies to the east and the Santa Rosa Mountains are to the northwest.

Climate

As with the Transverse Ranges, areas along the coast tend to have less temperature variation than do inland areas. The Peninsular Ranges also form a

rain shadow on the Colorado Desert region of California and on much of the larger Sonora Desert.[34] The ranges are affected by the marine layer
that provides cooling temperatures and fog, and rainfall varies seasonally with tropical storm activity.

References

  1. ^ "Average Yearly Precipitation for California Cities - Current Results". www.currentresults.com. Retrieved 2019-02-08.
  2. ^ "Southern California Climate". DigiMarCon - Digital Marketing Conferences. Retrieved 2019-02-08.
  3. ^ Schwartz, Rachel E. (2015). California Coastal Low Clouds : Variability and Influences across Climate to Weather and Continental to Local Scales (Thesis). UC San Diego.
  4. ^ Kaufman, Mark (31 May 2018). "Clouds are disappearing in Southern California, and we're not totally sure why". Mashable. Retrieved 2019-02-08.
  5. ^ Kahn, Brian (31 May 2018). "Southern California Is Losing Its Clouds and That's Bad News For Fire Season". Earther. Retrieved 2019-02-08.
  6. ^ Robbins, Gary (30 May 2017). "Yeah, 'May Gray' is a thing. So is 'June gloom." Statistics prove it". sandiegouniontribune.com. Retrieved 2019-02-08.
  7. ^ Aron, Hillel (2017-05-31). "In Praise of June Gloom, L.A.'s Most Underappreciated Weather Event". L.A. Weekly. Retrieved 2019-02-08.
  8. ^ "Most destructive wildfires in California history". ABC7 San Francisco. 2017-10-10. Retrieved 2019-02-08.
  9. ^
    ISSN 0458-3035
    . Retrieved 2019-02-08.
  10. ^ Meyer, Robinson (2017-10-17). "Will Northern California Soon Have Southern California's Climate?". The Atlantic. Retrieved 2019-02-08.
  11. ^ Mastars, Nathan (25 October 2012). "The Devil Wind: A Brief History of the Santa Anas". KCET. Retrieved 8 February 2019.
  12. ISSN 0458-3035
    . Retrieved 2019-02-08.
  13. ^ Barron, Laignee; Gajanan, Mahita (17 October 2017). "Why California's Fires are Bigger, Deadlier, and More Costly". Time. Retrieved 2019-02-08.
  14. ^ Sullivan, Brian K. (17 January 2019). "Climate Changed: Now California Wildfires Burn All Year". Bloomberg. Retrieved 2019-02-08.
  15. ^ Smith, Joshua Emerson (31 January 2019). "Climate change should tamp down California's wildfire-fanning Santa Ana winds, study finds". Los Angeles Times. Retrieved 2019-02-08.
  16. S2CID 31687132
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  17. .
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  19. . Retrieved 2019-02-08.
  20. ^ "Rainshadow Desert". digital-desert.com. Retrieved 2019-02-08.
  21. ^ Clarke, Chris (2012-11-30). "Rain Shadow Desert: Why the Rain Often Skips The Desert". KCET. Retrieved 2019-02-08.
  22. ISSN 2156-2202
    .
  23. .
  24. ^ "Southern California Areal Mapping Project home". geomaps.wr.usgs.gov. Retrieved 2019-02-08.
  25. .
  26. .
  27. ^ "California Coast Ranges Mountains North Coast and South Coast Ranges". www.seecalifornia.com. Retrieved 2019-02-08.
  28. ^ Interior, Department of (March 2003). "3 - Affected Environment". Santa Rosa and San Jacinto Mountains National Monument (N.M.) Management Plan: Environmental Impact Statement. Palm Springs, CA. p. 42.{{cite book}}: CS1 maint: location missing publisher (link)
  29. ^ Minch, John; Minch, Edwin; Minch, Jason. "Geology of Baja California". math.ucr.edu. Retrieved 2019-02-08.
  30. ^ "The tallest peaks in Southern California". Orange County Register. 2012-09-08. Retrieved 2019-02-08.
  31. ^ Snibbe, Kurt (3 January 2015). "BACK IN THE DAY: San Jacinto Peak and Mountains named for saint". The Press-Enterprise. Retrieved 8 February 2019.
  32. ^ Interior, Department of (June 2002). "3 - Visual and Scenic Resources". California Desert Conservation Area Plan Amendment for the Coachella Valley, Santa Rosa and San Jacinto Mountains Trails Management Plan, Riverside County: Environmental Impact Statement. Riverside County, CA. p. 56.{{cite book}}: CS1 maint: location missing publisher (link)
  33. ^ "Cuyapaipe Mountain : Climbing, Hiking & Mountaineering : SummitPost". www.summitpost.org. Retrieved 2019-02-08.
  34. . Peninsular Ranges rain shadow.