The mechanism driving the catastrophic weather phenomenon that gripped western North America in 2021 has been revealed by researchers at the Department of Environmental Systems Science, Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland.
The experts used the atmospheric Community Earth System Model to determine the causes of the heatwave, which affected the US states of Oregon and Washington, as well as the Canadian province of British Columbia, causing temperature to rise to 40-50 degrees Celsius in June-July 2021.
At the time, the extreme temperatures normally typical for desert regions resulted in a death toll of 1,400 people and triggered deadly wild fires.
The heatwave originated in the North Pacific Ocean, where high humidity over the open sea led to the emergence of air masses carrying potential energy. These masses traveled thousands of kilometers through atmospheric currents known as "ocean conveyor belts" and reached western North America, the research, published in the journal Earth's Future, states.
The masses then spiraled down to the surface, and the potential energy turned into heat. The vertical expansion of the air masses brought in additional heat from the higher layers of the atmosphere, while the horizontal expansion brought dangerously soaring temperatures to a wide geographical area. Extremely low soil moisture also contributed to the heatwave, the authors say.
Fountain at Georgetown Waterfront Park during a heatwave on August 13, 2021, in Washington, DC.
© AFP 2023 / BRENDAN SMIALOWSKI
The heatwave, which brought some of the highest temperatures ever recorded in the region, on some days exceeded average temperatures by 10 degrees Celsius (or 18 degrees Fahrenheit). The maximum surpassed on some days was by 30 degrees Celsius (54 degrees Fahrenheit). At the time, it was said that a disruption of the jet stream carrying air across the Northern Hemisphere along a circular path was at fault.