Statewide trends

Changing weather patterns due to climate change are at least partly responsible for the dramatic decline in precipitation during the two back-to-back winters in California—the winters of 2012-2013 and 2013-2014—that contributed to the severity of the California drought.

Researchers have linked climate change to the circulation patterns that produced the unprecedented high-pressure weather pattern known as the “ridiculously resilient ridge” that blocked storms from the state.[1][2]

Regional trends

A study looking at data from 1979 to 2014 finds up to a 25 percent decrease in precipitation in the US Southwest related to an increase in high pressure, anticyclonic conditions during this time in the North East Pacific.[3]

Globally, models show that many mid-latitude and subtropical dry regions will see a decrease in precipitation by 2100 should global emissions continue to increase.[4]