On January 17, 2014 California State Governor, Jerry Brown, declared a drought state of emergency.
As of April 1, 2014, the California Department of Water Resources measured the statewide water content of snowpack at only 18% of the historical average. The April 1 snowpack measurement is crucial because this is when the snowpack is normally at its peak and begins to melt into streams and reservoirs. Snowpack, through runoff, provides about one-third of the water used by California's cities and farms. California's 2014 Water Year, which ended September 30, 2014, was the third driest in 119 years of record. It also was the warmest year on record. At the end of Water Year 2014, about half of USGS California streamgages with long-term data records had flows less than 25% of normal, and about a quarter of the gages had stream flows less than 10% normal. Statewide, reservoirs were 57% of average levels.
Since October 1, 2014, the State has had several significant precipitation events. However, mild temperatures accompanying storms in the northern part of the state, and low January precipitation, have resulted in low statewide snow water equivalent in the Sierras, measured on January 29th at 25 percent of normal. The State currently remains in drought conditions and most reservoir levels are still well below historic averages.
The USGS closely monitors the effects of drought through data collection and research, and is studying the current drought in the context of long-term hydrologic, climatic, and environmental changes. These studies support successful planning and science-based decision-making by water managers who must address complex issues and competing interests in times of drought. They also and help decision-makers prepare for climate change and possible future drought.
A drought is a period of drier-than-normal conditions that results in water-related problems. When rainfall is less than normal for several weeks, months, or years, the flow of streams and rivers declines, water levels in lakes and reservoirs fall, and the depth to water in wells increases. If dry weather persists and water-supply problems develop, the dry period can become a drought.
The term "drought" can have different meanings to different people, depending on how a water deficiency affects them. Droughts have been classified into different types such as:
- meteorological drought - lack of precipitation
- agricultural drought - lack of soil moisture, or
- hydrologic drought -reduced streamflow or groundwater levels
It is not unusual for a given period of water deficiency to represent a more severe drought of one type than another type. For example, a prolonged dry period during the summer may substantially lower the yield of crops due to a shortage of soil moisture in the plant root zone but have little effect on groundwater storage replenished the previous spring.