Central Valley Agriculture
USGS tools are being used by water managers during California's severe drought
Where Did the Water Go?
USGS California Water Science Center Drought web site answers all your questions about drought in California
Is Climate Change Affecting Water Supply?
USGS scientists at the California Water Science Center are studying how climate change may impact water resources
Is the Central Valley Sinking?
As groundwater is withdrawn at greater rates, land subsidence becomes a bigger issue
Competition for water resources is growing throughout California, particularly in the Central Valley. Statewide population growth, anticipated reductions in Colorado River water deliveries, drought, and the ecological crisis in the Sacramento-San Joaquin Delta have created an intense demand for water. USGS Tools and information can be used to help manage the Central Valley aquifer system, an important State and national resource.
The Central Valley of California, which stretches from Redding to below Bakersfield, is predominantly used for agriculture, providing one quarter of the Nation's food as well as accounting for 20% of the Nation's groundwater demand. Fifty percent of the water used in the Central Valley comes from groundwater. As California enters it's 5th straight year of sever drought, groundwater resources throughout the Central Valley are being withdrawn faster than they are being replenished. When groundwater levels continue to drop, land surface can begin to subside, or sink.
The CAWSC is studying both water use and availability as well as land subsidence throughout the Central Valley. An over view of the Valley and CAWSC research is available on the CAWSC Central Valley web site.
Central Valley Hydrologic Model
One key tool being used to assist water managers in the Central Valley is the Central Valley Hydrologic Model (CVHM). The CVHM is an extensive, detailed three-dimensional (3D) computer model of the hydrologic system of the Central Valley. The Central Valley Hydrologic Model (CVHM) simultaneously accounts for changing water supply and demand across the landscape, and simulates surface water and groundwater flow across the entire Central Valley.
A complete description of the model and datasets used in the model are available on the CAWSC CVHM web site.
Land Subsidence
Over time, overpumping in the San Joaquin Valley has caused groundwater-level declines and associated aquifer-system compaction and land subsidence that has resulted in permanent aquifer-system storage loss. By 1970, significant land subsidence (more than one foot) had occurred in about half of the San Joaquin Valley and locally, some areas had subsided by as much as 28 feet. Reduced surface-water availability during 1976-77, 1986-92, 2007-09, and 2012-2015 caused groundwater-pumping increases in the San Joaquin Valley, declines in water-levels to near or beyond historic lows, and renewed aquifer compaction. The resulting land subsidence has reduced the freeboard and flow capacity of the Delta-Mendota Canal—as well as the California Aqueduct and other canals that transport floodwater and deliver irrigation water—requiring expensive repairs.
The USGS CAWSC is monitoring land subsidence in the Central Valley and throughout California through an extensive land subsidence monitoring network.
Drought
The CAWSC has produced an interactive map combining water levels, CVHM regions, and subsidence data. The map is a great visualization of the effects of the ongoing severe drought in California. CAWSC also has a complete web site dedicated to information and data about the severe drought in California including the CAWSC role in science-based decision making.
Below are publications associated with this project.
Water availability and land subsidence in the Central Valley, California, USA
Water availability and subsidence in California's Central Valley
Land subsidence along the Delta-Mendota Canal in the northern part of the San Joaquin Valley, California, 2003-10
California's Central Valley Groundwater Study: A Powerful New Tool to Assess Water Resources in California's Central Valley
Land subsidence in the San Joaquin Valley, California, as of 1980
Land subsidence in the San Joaquin Valley, California, as of 1972
Competition for water resources is growing throughout California, particularly in the Central Valley. Statewide population growth, anticipated reductions in Colorado River water deliveries, drought, and the ecological crisis in the Sacramento-San Joaquin Delta have created an intense demand for water. USGS Tools and information can be used to help manage the Central Valley aquifer system, an important State and national resource.
The Central Valley of California, which stretches from Redding to below Bakersfield, is predominantly used for agriculture, providing one quarter of the Nation's food as well as accounting for 20% of the Nation's groundwater demand. Fifty percent of the water used in the Central Valley comes from groundwater. As California enters it's 5th straight year of sever drought, groundwater resources throughout the Central Valley are being withdrawn faster than they are being replenished. When groundwater levels continue to drop, land surface can begin to subside, or sink.
The CAWSC is studying both water use and availability as well as land subsidence throughout the Central Valley. An over view of the Valley and CAWSC research is available on the CAWSC Central Valley web site.
Central Valley Hydrologic Model
One key tool being used to assist water managers in the Central Valley is the Central Valley Hydrologic Model (CVHM). The CVHM is an extensive, detailed three-dimensional (3D) computer model of the hydrologic system of the Central Valley. The Central Valley Hydrologic Model (CVHM) simultaneously accounts for changing water supply and demand across the landscape, and simulates surface water and groundwater flow across the entire Central Valley.
A complete description of the model and datasets used in the model are available on the CAWSC CVHM web site.
Land Subsidence
Over time, overpumping in the San Joaquin Valley has caused groundwater-level declines and associated aquifer-system compaction and land subsidence that has resulted in permanent aquifer-system storage loss. By 1970, significant land subsidence (more than one foot) had occurred in about half of the San Joaquin Valley and locally, some areas had subsided by as much as 28 feet. Reduced surface-water availability during 1976-77, 1986-92, 2007-09, and 2012-2015 caused groundwater-pumping increases in the San Joaquin Valley, declines in water-levels to near or beyond historic lows, and renewed aquifer compaction. The resulting land subsidence has reduced the freeboard and flow capacity of the Delta-Mendota Canal—as well as the California Aqueduct and other canals that transport floodwater and deliver irrigation water—requiring expensive repairs.
The USGS CAWSC is monitoring land subsidence in the Central Valley and throughout California through an extensive land subsidence monitoring network.
Drought
The CAWSC has produced an interactive map combining water levels, CVHM regions, and subsidence data. The map is a great visualization of the effects of the ongoing severe drought in California. CAWSC also has a complete web site dedicated to information and data about the severe drought in California including the CAWSC role in science-based decision making.
Below are publications associated with this project.