A new study says that global warming has measurably worsened the
ongoing1 California drought. While scientists largely agree that natural weather variations have caused a lack of rain, an emerging
consensus2 says that rising temperatures may be making things worse by driving moisture from plants and soil into the air. The new study is the first to estimate how much worse: as much as a quarter. The findings suggest that within a few decades, continually increasing temperatures and resulting moisture losses will push California into even more
persistent3 aridity4. The study appears this week in the journal Geophysical Research Letters. "A lot of people think that the amount of rain that falls out the sky is the only thing that matters," said lead author A. Park Williams, a bioclimatologist at Columbia University's Lamont-Doherty Earth
Observatory5. "But warming changes the baseline amount of water that's available to us, because it sends water back into the sky."
The study adds to growing evidence that climate change is already bringing extreme weather to some regions. California is the world's eighth-largest economy, ahead of most countries, but many scientists think that the nice weather it is famous for may now be in the process of going away. The record-breaking drought is now in its fourth year; it is drying up wells, affecting major produce growers and feeding wildfires now
sweeping6 over vast areas.
The researchers
analyzed7 multiple sets of month-by-month data from 1901 to 2014. They looked at precipitation, temperature, humidity, wind and other factors. They could find no long-term rainfall trend. But average temperatures have been creeping up--about 2.5 degrees
Fahrenheit8 over the 114-year period, in step with building fossil-fuel
emissions9. Natural weather variations have made California unusually hot over the last several years; added to this was the background trend. Thus, when rainfall declined in 2012, the air sucked already
scant10 moisture from soil, trees and crops harder than ever. The study did not look directly at snow, but in the past, gradual melting of the high-mountain winter snowpack has helped water the lowlands in warm months. Now, melting has accelerated, or the snowpack has not formed at all,
helping11 make warm months even
dryer12 according to other researchers.