The research team is comprised of Tom Ballinger, Assistant Professor in the Department of Geography at Texas State University, Dagmar Budikova, Department of Geography, Geology and the Environment, Illinois State University, and Trent W. Ford, Department of Geography and Environmental Resources, Southern Illinois University. Their study, "United States Heat Wave Frequency and Arctic Ocean Marginal Sea Ice Variability," is published in the journal JGR Atmospheres at

The study highlights a statistical relationship between Arctic sea ice and extreme weather events in the United States. The research suggests that during warmer years in the Arctic when sea ice is low, heat waves are more frequent to the south across much of the eastern half of the U.S. due to North Atlantic ocean-atmosphere interactions involving jet stream currents in the Northern Hemisphere. The evidence suggests these factors allow specific weather patterns, including heatwaves, to persist for longer periods than the historical norm.  

"With the Arctic warming faster than in the mid-latitudes, you would expect that the temperature and pressure gradient, and therefore Northern Hemisphere atmospheric circulation, to be affected as a physical response," Ballinger said. "We’re seeing evidence of this through more persistent weather systems in the mid-latitudes."

In addition to heatwaves, the researcher suggests Arctic conditions contribute to ongoing dry or rainy weather patterns and harsh winter weather in the U.S. and Siberia. Understanding these connections could help scientists improve their weather and climate projections in different parts of the world.