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Scientific American

Scientific American reports that 70 MIT students and faculty were among those who attended the People’s Climate Change March in New York. "We have the technologies to begin to tackle the climate crisis,” said Ph.D. candidate Geoffrey Supran. “What we lack is the political will to make it happen."

Slate

Professor Kerry Emanuel joined a number of experts encouraging participation in the People’s Climate Change March, held in New York, Sep. 21, reports Eric Holthaus for Slate. “The more ways that people—particularly young people—can make their concerns known to our government, the better,” says Emanuel. 

Scientific American

Writing for Scientific American, Tim Radford reports on Professor Paul O’Gorman’s new study, which shows that despite climate change blizzards will still occur. Radford writes that O’Gorman’s research shows that while some areas may receive less overall snowfall, extreme snowfall could become more intense. 

The Washington Post

Washington Post reporter Angela Fritz writes that MIT Professor Paul O’Gorman has found that extreme snowfall events will continue despite global warming. Fritz reports that O’Gorman’s models show that in some high-latitude cases, “extreme snowstorms could deposit 10 percent more snow.” 

NBC News

Gil Aegerter of NBC News reports on new MIT research examining the impacts of climate change on snowfall. Professor Paul O’Gorman found that “global warming would affect snowfall extremes less than it did average snowfall,” writes Aegerter. 

USA Today

Doyle Rice of USA Today writes about the new MIT study showing that despite warming brought about by climate change, extreme snowfall will still occur in the Northern Hemisphere. Researchers found that while “yearly average snowfall declines due to climate change in most regions, it actually increases in regions with very low surface temperatures,” writes Rice. 

The Christian Science Monitor

The Christian Science Monitor’s Peter Spotts reports on new MIT research that finds volcanoes may be the cause of a recent hiatus in the rise of global surface temperatures.