Tulare Lake Hydrologic Region

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From the 16.5 MAF of groundwater pumped annually in the state of California, 39% will be used for agriculture, 41% will be used in the urban sector, while 18% will be used to manage the state’s wetlands (DWR 2015). The Central Valley alone uses 74% of all extracted groundwater, where the Tulare Lake Hydrologic Region is the greatest groundwater user (DWR 2015). Since the state’s topography and hydrological conditions vary throughout the state, the amount of precipitation that the state receives will vary. Some areas lack access to enough water to meet water demands, so the state and federal water projects help by importing water. When the amount of surface water from the state and federal water projects does not fully meet local water demands, …show more content…

The lack of groundwater oversight has unfortunately introduced concerns that need to be mitigated and better addressed. Some groundwater basins throughout the state are not sustainable for they have experienced a depletion in groundwater storage, experienced groundwater overdraft, had a reduction in stream flows, the potential to lose ecosystems, had a depletion in groundwater quality, experienced land subsidence, and or faced salt water intrusion.
In a coordinated effort, conjunctive use has been sought as a way of managing both groundwater and surface water simultaneously. According to California’s Water Plan Update 2013, conjunctive use is defined as “a coordinated and planned use and management of both surface water and groundwater resources to maximize the availability and reliability of water supplies in a region to meet various management objectives” (DWR 2013). Through conjunctive use, groundwater is essentially stored and used for future needs mostly during drought periods. Through this management scheme users can rely on stored groundwater during dry periods, and surface water during wet …show more content…

Land subsidence is defined as the gradual sinking of the Earth’s surface (USGS 2016). Areas of concern include the Tulare Lake Basin and the San Juaquin basin, with land subsidence of up to 30ft due to groundwater overdraft (Lund and Harter 2013). Land subsidence can be a threat locally because of the damage it can cause to infrastructure, canals, bridges, and sewers. Figure 3 demonstrates how dire the results may be from land subsidence. Figure 3 is an image demonstrating how much land subsidence has occurred in the Central Valley, near the area of Mendota California. In the image it can be seen how the land has significantly dropped with time as a result of the large amounts of groundwater that have been withdrawn from the

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