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Heat spikes over Tibet may help explain severe Californian flooding

Unusually high temperatures over the mountainous region can kick-start a chain of events that ultimately leads to a severe deluge on the US West Coast, scientists say 
severe flooding in California in March 2023
Severe flooding in California in March 2023
US Army Photo/Alamy

In 2017, California experienced its wettest winter on record. Record-breaking rain in January of that year caused major flooding, inundating hundreds of homes, blocking roads and causing power blackouts for more than half a million people.

But the torrential rain puzzled researchers because it occurred during a weak La Niña phase, where sea-surface temperatures in the Pacific Ocean are generally below normal. This would usually increase the risk of a dry winter for California, not a very wet one.

Six years later, the same thing happened again. The Pacific Ocean was in a La Niña but, contrary to expectations, torrential rain poured over California between December 2022 and March 2023.

For years, this strange inversion of winter weather baffled scientists. Now, an international team of researchers thinks the answer may lie in unusually warm weather on the Tibetan plateau, a vast mountain plateau in Asia with an average elevation greater than 4500 metres above sea level.

Weather in high-elevation regions like this can have an effect on weather “comparable to sea-surface temperatures”, says at the University of California, Los Angeles, who led the study.

The team used climate models to simulate the effect of record warm weather over the Tibetan plateau in December 2016 and the wet weather that arrived in California in January 2017. They repeated the same modelling for February 2023 over the Tibetan plateau and March 2023 in California.

Xue says in both cases, the warm temperatures over the plateau led to meteorological effects well known to drive extreme rainfall. They caused a perturbation in the westerly jet, a fast-flowing atmospheric river, which, in turn, affected other atmospheric rivers and triggered the breaking of Rossby waves – large meanders in high-altitude winds – near the Californian coast.

According to the paper, the modelling suggests heat over the Tibetan plateau can explain 56 per cent of the extreme rainfall anomaly over California in January 2017, and 30 per cent of the rainfall anomaly in March 2023.

The connection between the high mountains and California emerges in the data only after 1980, adds Xue, a sign that rapidly rising temperatures in mountainous regions are causing unexpected effects. “Certainly this is something related to climate change,” he says.

The conclusions form part of to identify the role high-elevation land temperatures might play in driving extreme or unusual weather events around the world.

“The study seems to nicely demonstrate how anomalous surface heating over the Tibetan plateau during early winter can affect the winter hydroclimate and its extremes on the other side of the Pacific Ocean basin, across the US south-west coast,” says at the University of Lausanne in Switzerland. However, he says the exact causal mechanisms linking the Tibetan plateau to California require further study.

, formerly of the US National Oceanic and Atmospheric Administration, agrees. He says that, while the findings are “intriguing”, more work is needed to confirm the connection using fresh data before it can prove useful for forecasting.

Journal Reference:

Science Advances

Topics: Environment / floods