Anthropogenic warming has increased drought risk in California

Noah S. Diffenbaugh1,2, Daniel L. Swain3, Danielle Touma3
1Department of Environmental Earth System Science and; Woods Institute for the Environment, Stanford University, Stanford, CA 94305
2Woods Institute for the Environment, Stanford University, Stanford, CA 94305;
3Department of Environmental Earth System Science and

Tóm tắt

Significance California ranks first in the United States in population, economic activity, and agricultural value. The state is currently experiencing a record-setting drought, which has led to acute water shortages, groundwater overdraft, critically low streamflow, and enhanced wildfire risk. Our analyses show that California has historically been more likely to experience drought if precipitation deficits co-occur with warm conditions and that such confluences have increased in recent decades, leading to increases in the fraction of low-precipitation years that yield drought. In addition, we find that human emissions have increased the probability that low-precipitation years are also warm, suggesting that anthropogenic warming is increasing the probability of the co-occurring warm–dry conditions that have created the current California drought.

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