Why Heat is Accelerating the California Drought

Although record low precipitation has been the main driver of one of the worst droughts in California history, abnormally high temperatures have also played an important role in amplifying its adverse effects, according to a recent study by the U.S. Geological Survey and university partners.
Experiments with a hydrologic model for the period Oct. 2013-Sept. 2014 showed that if the air temperatures had been cooler, similar to the 1916-2012 average, there would have been an 86% chance that the winter snowpack would have been greater, the spring-summer runoff higher, and the spring-summer soil moisture deficits smaller.

To gauge the effect of high temperatures on drought, lead author Shraddhanand Shukla (University of California – Santa Barbara, UCSB) devised two sets of modeling experiments that compared climate data from water year 2014 (Oct. 2013-Sept. 2014) to similar intervals during 1916-2012.
In the first simulation set, Shukla substituted 2014 temperature values with the historical temperatures for each of the study’s 97 years, while keeping the 2014 precipitation values. In the second simulation set, he combined the observed 2014 temperatures with historical precipitation values for each of the preceding years, 1916-2012.
“This experimental approach allows us to model past situations and tease out the influence of temperature in preceding drought conditions,” said Chris Funk, a USGS scientist and a co-author of the investigation. “By crunching enough data over many, many simulations, the effect of temperature becomes more detectable.  We can’t do the same in reality, the here and now, because then we only have a single sample.” Funk, an adjunct professor at UCSB, helps coordinate research at the university that supports USGS programs.
High heat has multiple damaging effects during drought, according to the study, increasing the vulnerability of California’s water resources and agricultural industry. Not only does high heat intensify evaporative stress on soil, it has a powerful effect in reducing snowpack, a key to reliable water supply for the state. In addition to decreased snowpack, higher temperatures can cause the snowpack to melt earlier, dramatically decreasing the amount of water available for agriculture in summer when it is most needed.