Given the known influence of temperature on drought, the fact that the 2012 — 2014 record drought severity has co-occurred with record statewide warmth (7) raises the question of whether long - term warming has altered the probability that
precipitation deficits yield extreme drought in California.
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.
Taken together, the observed record from California suggests that (i)
precipitation deficits are more likely to
yield 1 - SD PMDI droughts if they occur when conditions are warm and (ii) the occurrence of 1 - SD PMDI droughts, the probability of
precipitation deficits producing 1 - SD PMDI droughts, and the probability of
precipitation deficits co-occurring with warm conditions have all been greater in the past two decades than in the preceding century.