Summer swelter trend: West gets hotter days, East hot nights
As outlandish as the killer heat wave that struck the Pacific Northwest was, it fits into a decades-long pattern of uneven summer warming across the United States.
The West is getting roasted by hotter summer days while the East Coast is getting swamped by hotter and stickier summer nights, an analysis of decades of U.S. summer weather data by The Associated Press shows.
State-by-state average temperature trends from 1990 to 2020 show America’s summer swelter is increasing more in some of the places that just got baked with extreme heat over the past week: California, Nevada, New Mexico, Arizona, Utah, Oregon and Colorado.
The West is the fastestwarming region in the country during June, July and August, up 3 degrees on average since 1990. The Northwest has warmed nearly twice as much in the past 30 years as it has in the Southeast.
That includes Portland, Oregon which set a record 116-degree high that was 3 degrees warmer than temperatures ever recorded in Oklahoma City or DallasFort Worth.
Although much of the primary cause of the past week’s extreme heat was an unusual but natural weather condition, scientists see the fingerprint of human-caused climate change, citing altered weather patterns that park
heat in different places for longer periods.
“The ridiculous temperatures in the Pacific Northwest may on one hand be considered a black swan (ultra-rare) event, but on the other hand are totally consistent” with long-term trends, said meteorologist Judah Cohen of the private firm Atmospheric and Environmental Research. “So I am not going to predict when is the next time Portland will hit 116 but I believe hotter summers for the broader region are here to stay.”
Climate change is altering and weakening the jet stream, narrow bands of wind that circle the Earth flowing west to east. Those changes allow key weatherproducing patterns of high and low pressure to stall in
place. High pressure is stalling more often in the West in summer, said Pennsylvania State University climate scientist Michael Mann. High pressure brings hot and dry weather that, when stalled, can create what are known as heat domes. Low pressure brings wet weather.
Another factor is higher water temperatures in the Pacific Ocean that also generate more so-called high-pressure ridges the West, said Gerald Meehl, a National Center for Atmospheric Research scientist who studies heat waves.
These patterns are showing up so often that their effects can be seen in longterm data. The U.S. Northwest, western Canada and Siberia, which also just saw a stunning heat wave, are
among Earth’s fastest warming land areas during summer since 1990, Cohen said.
The Midwest is warming slower during the summer than either coast. That’s because stalled low pressure areas often drive cooler air into the Great Lakes region, said North Illinois University climate scientist Victor Gensini.
Water explains the big difference between western and eastern heat trends, scientists said.
“In western states where drought has been expanding and intensifying during the past decade, soil moisture has been declining. Dry soil heats up faster than moist soil during the day because all the solar energy goes into heating rather than into evaporating moisture,” said Jennifer Francis, a climate scientist at the Woodwell Climate Research Center. “Dry soil also cools off faster at night.”
That’s partly why the West, which is getting drier by the decade and is mired in a 20-year megadrought, is seeing those crazy triple digit daytime temperatures.
The East is getting wetter by the decade, NOAA records show, and the East Coast is seeing its biggest warming increase at night. The overnight lows in New Jersey and Delaware have warmed 3 degrees since 1990, the biggest increases in the nation.
Water vapor is a greenhouse gas, Francis explained, “So at night it traps more of the heat.”
Kathie Dello, North Carolina’s state climatologist, attributes the trends to human-caused warming. “There’s no other explanation,” she said.