More than 80% of California is in one of the two most severe categories of drought, as shown by the darker colors on the above map. No region has escaped the drought.
California is preparing for a third straight year of drought, and officials are tightening limits on water use to levels never seen so early in the water year.
Most of the state’s water reservoirs are well below average, with several at less than a third of their capacity.
The outlook for rain and snow this winter, when most of the state’s yearly precipitation arrives, isn’t promising.
Especially worrying is the outlook for the Sierra Nevada, the long mountain chain that runs through the eastern part of the state. California’s cities and its farms—which grow over a third of the nation’s vegetables and two-thirds of its fruit and nuts—rely on runoff from the mountains’ snowpack for water.
A closer look at California’s water resources shows the challenge ahead and how hot/dry cycles is putting the state’s water supply and agriculture at greater risk.
Where California gets its water?
Statewide, California averages about 2 feet of precipitation a year, about two-thirds of the global average, giving the state as a whole a semiarid climate.
The majority of California’s rain and snow falls in the mountains, primarily in winter and spring. But agriculture and coastal cities need that water to get through the dry summers.
To get water to dry Southern California and help with flood control in the north, California over the past century developed a statewide system of reservoirs, tunnels and canals that brings water from the mountains.
The largest of those projects, the State Water Project, delivers water from the higher-precipitation northern Sierra to the southern half of the state.
To track where the water goes, it’s useful to look at the volume in acre-feet. California is about 100 million acres in area, so at 2 feet a year, its annual precipitation averages about 200 million acre-feet.
Of that 200, an average of only about 80 million acre-feet heads downstream. Much of the water returns to the atmosphere through evapotranspiration by plants and trees in the Sierra Nevada or North Coast forests.
Of the 80 million acre-feet that does run off, about half remains in the aquatic environment, such as rivers flowing to the ocean.
That leaves about 41 million acre-feet for downstream use. About 80% of that goes for agriculture and 20% for urban uses.
In wet years, there may be much more than 80 million acre-feet of water available, but in dry years, it can be much less.
In 2020, for example, California’s precipitation was less than two-thirds of average, and the State Water Project delivered only 5% of the contracted amounts. The state’s other main aqueduct systems that move water around the state also severely reduced their supplies.
2021 water year one of the three driest on record
The 2021 water year, which ended Sept. 30, was one of the three driest on record for the Sierra Nevada. Precipitation was about 44% of average.
With limited precipitation as of December 2021 and the state in extreme drought, the State Water Project cut its preliminary allocations for water agencies to 0% for 2022, with small amounts still flowing for health and safety needs.
Updated Drought Monitor released Dec 2nd. pic.twitter.com/9KoAPZy5rf— NWS Bay Area (@NWSBayArea) December 3, 2021
While conditions could improve if more storms come in the next three months, the official National Oceanic and Atmospheric Administration outlook points to below-normal precipitation being more likely than above normal.
Drought and a warming climate
Multiyear dry periods, when annual precipitation is below average, are a feature of California’s climate, but rising global temperatures are also having an impact.
Over the past 1,100 years, there has been at least one dry period lasting four years or longer each century. There have been two in the past 35 years—1987-92 and 2012-15. A warmer climate intensifies the effect of these dry periods, as drier soil and drier air stress both natural vegetation and crops.
Rising global temperatures affect runoff from the Sierra Nevada, which provides over 60% of California’s developed water supply.
Over 80% of the runoff in the central and southern Sierra Nevada comes from the snow zone. In the wetter but lower-elevation northern Sierra, rainfall contributes over one-third of the annual runoff.
The average snowline, the elevation above which most precipitation is snow, goes from about 5,000 feet elevation in the north to 7,000 feet in the south. On average, each 1.8 degrees Fahrenheit (1 Celsius) of warming could push the snowline another 500 feet higher, reducing the snow total.
Shifts from snow to rain and earlier runoff also mean that more of the capacity behind existing dams will be allocated to flood control, further reducing their capacity for seasonal water-supply storage.
A wealth of research has established that the Sierra Nevada could see low- to no-snow winters for years at a time by the late 2040s if the climate cycles continue warming.
Warming will also increase water demand from forests as growing seasons lengthen and drive both drought stress leading to tree mortality and increased risk of high-severity wildfires.
Sustainability in a warming climate
Water storage is central to California’s water security.
Communities and farms can pump more groundwater when supplies are low, but the state has been pumping out more water than is replenished in wet years.
Parts of the state rely on water from the Colorado River, whose dams provide for several years of water storage, but the basin lacks the runoff to fill the dams.
Public opposition has made it difficult to build new dams, so better use of groundwater for both seasonal and multiyear storage is crucial.
A great documentary about the coming WATER WARS!