Los Angeles Times

Warming, drought link uncertain

Analysis underscore­s difficulty of gauging influence of humancause­d climate change on rain patterns.

- By Bettina Boxall bettina. boxall @ latimes. com

Global warming contribute­d to extreme heat waves in many parts of the world last year but cannot be definitive­ly linked to the California drought, according to a newreport.

The third annual analysis of extreme weather events underscore­d the continuing difficulty of teasing out the influence of human- caused climate change on precipitat­ion patterns.

One of three studies examining the California drought in 2013 found that the kind of high- pressure systems that blocked winter storms last year have increased with global warming.

But another study concluded that a long- term rise in sea surface temperatur­es in the western Pacific did not contribute substantia­lly to the drought. And researcher­s noted that California precipitat­ion since 1895 has “exhibited no appreciabl­e downward trend.”

Overall, the report’s editors concluded that the papers didn’t demonstrat­e that global warming clearly influenced the drought, which is one of the worst in the state record.

In the report, published in the Bulletin of the American Meteorolog­ical Society and released lastweek, 20 research teams explored the causes of 16 extreme weather events recorded in 2013, including torrential downpours in Colorado, heat waves in Korea and Australia and a blizzard in South Dakota.

The studies overwhelmi­ngly showed that humancause­d climate change played a role in the heat waves, in some cases making them10 times more likely.

But the report editors wrote that “natural variabilit­y likely played a much larger role in the extreme precipitat­ion events,” whether it was flooding in India, deep snow in the Spanish Pyrenees or the California drought.

Last year’s exceedingl­y dry winter in California was largely the result of a stubborn high- pressure system parked over the northeaste­rn Pacific Ocean. Nicknamed the Ridiculous­ly Resilient Ridge by Stanford University researcher Daniel Swain, the system shunted winter storms far to the north, off their normal path to California.

Those sorts of high- pres- sure systems “are considerab­ly more likely to occur” with global warming, said Swain, lead author of one of the three California papers. “It suggests an increased likelihood of the kinds of large- scale atmospheri­c conditions that are conducive to drought in California,” he added.

But Marty Hoerling, coeditor of the climate report and a research meteorolog­ist with the National Oceanic and Atmospheri­c Administra­tion, noted that high- pressure systems have increased everywhere. What drives storms is the difference in atmospheri­c pressure over the north and south Pacific, he said, and that was not examined in the Swain paper.

Researcher­s concluded in a third paper that although long- term warming contribute­s to storm- diverting high- pressure systems over the northeast Pacific, that is countered by an increase in atmospheri­c humidity that can promote wetter weather in California.

Comparing the periods of 1871 to 1970 with 1980 to 2013, the authors wrote that there was “no appreciabl­e longterm change in the risk for dry climate extremes over California since the late 19th century.”

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