Ozone depletion trumps greenhouse gas increase in jet-stream shift

Credit: NASA Earth Observatory 							 Watching the Ozone Hole Before and After
Credit: NASA Earth Observatory Watching the Ozone Hole Before and After the Montreal Protocol
UNIVERSITY PARK, Pa. Depletion of Antarctic ozone is a more important factor than increasing greenhouse gases in shifting the Southern Hemisphere jet stream in a southward direction, according to researchers at Penn State. "Previous research suggests that this southward shift in the jet stream has contributed to changes in ocean circulation patterns and precipitation patterns in the Southern Hemisphere, both of which can have important impacts on people's livelihoods," said Sukyoung Lee, professor of meteorology. According to Lee, based on modeling studies, both ozone depletion and greenhouse gas increase are thought to have contributed to the southward shift of the Southern Hemisphere jet stream, with the former having a greater impact. But until now, no one has been able to determine the extent to which each of these two forcings has contributed to the shift using observational data. "Understanding the differences between these two forcings is important in predicting what will happen as the ozone hole recovers," she said. "The jet stream is expected to shift back toward the north as ozone is replenished, yet the greenhouse-gas effect could negate this." Lee and her colleague, Steven Feldstein, professor of meteorology, developed a new method to distinguish between the effects of the two forcings.
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