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San Joaquin Valley

Area of the Central Valley in California

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Through Holocene and Groundwater

San Joaquin Valley draws from eight counties of Northern and Central California, including all of San Joaquin and Kings counties, most of Stanislaus, Merced, and Fresno counties, and parts of Madera and Tulare counties, along with a majority of Kern County. Although the valley is predominantly rural, it has four densely populated urban centers: Stockton/Modesto, Fresno, Porterville/Visalia, and Bakersfield.

Geography

The San Joaquin Valley is the southern half of California's Central Valley. It extends from the Sacramento–San Joaquin River Delta in the north to the Tehachapi Mountains in the south, and from the California coastal ranges (Diablo and Temblor) in the west to the Sierra Nevada in the east.

The valley contains two large river systems, divided north and south. The northern portion of the San Joaquin Valley is called the San Joaquin Basin: the watershed of the San Joaquin River and its tributaries, including parts of the Kings River, all of which drain northwest into the Sacramento–San Joaquin River Delta and eventually out to the Pacific Ocean. The somewhat larger southern portion is the Tulare Basin, an endorheic basin centered on Tulare Lake. Historically, Tulare Lake was fed by the Tule River, the Kings River, the Kaweah River, the White River and the Kern River, but much of this water has been diverted for agricultural uses and the watershed is mostly dry in its lower reaches.

Geological history

The San Joaquin Valley began to form about 66 million years ago during the early Paleocene era. Broad fluctuations in the sea level caused various areas of the valley to be flooded with ocean water for the next 60 million years. About 5 million years ago, the marine outlets began to close due to uplift of the coastal ranges and the deposition of sediment in the valley. Starting 2 million years ago, a series of glacial episodes periodically caused much of the valley to become a fresh water lake. Lake Corcoran was the last widespread lake to fill the valley about 700,000 years ago. At the beginning of the Holocene there were three major lakes remaining in the southern part of the Valley, Tulare Lake, Buena Vista Lake and Kern Lake. In the late 19th and in the 20th century, agricultural diversion of the Kern River eventually dried out these lakes. Today, only a fragment of Buena Vista Lake remains as two small lakes Lake Webb and Lake Evans in a portion of the former Buena Vista Lakebed.

Climate

The San Joaquin Valley has extremely hot, dry summers and pleasantly mild winters characterized by dense tule fog. Its rainy season normally runs from November through April. The valley has experienced a severe and intensifying megadrought since the early 2010s. This drought is not only affecting humans, with farmland taking much of the impact, but also the wildlife as well.

In August 2015, the Director of the California Department of Water Resources stated, "Because of increased pumping, groundwater levels are reaching record lows—up to 100 feet lower than previous records." Research from NASA shows that parts of the San Joaquin Valley sank as much as 8 inches (0.20 m) in a four-month period, and land near Corcoran sank 13 inches (0.33 m) in 8 months. The sinking has destroyed thousands of groundwater well casings and has the potential to damage aqueducts, roads, bridges, and flood-control structures. In the long term, the subsidence caused by extracting groundwater could irreversibly reduce the underground aquifer's water storage capacity, although immediate and short-term needs are given higher priority and a sense of urgency than long-term sustainability.

The National Weather Service Forecast Office for the San Joaquin Valley is located in Hanford and includes a Doppler weather radar. Weather forecasts and climatological information for the San Joaquin Valley are available from its official website.

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