Short-lived greenhouse gases cause centuries of sea-level rise
http://news.mit.edu/2017/short-lived-greenhouse-gases-cause-centuries-sea-level-rise-0109[font face=Serif][font size=5]Short-lived greenhouse gases cause centuries of sea-level rise[/font]
[font size=4]Through warming effects, methane and other gases impact rising seas long after leaving the atmosphere.[/font]
Jennifer Chu | MIT News Office
January 9, 2017
[font size=3]Even if there comes a day when the world completely stops emitting greenhouse gases into the atmosphere, coastal regions and island nations will continue to experience rising sea levels for centuries afterward, according to a new study by researchers at MIT and Simon Fraser University.
In a paper published this week in the Proceedings of the National Academy of Sciences, the researchers report that warming from short-lived compounds greenhouse gases such as methane, chlorofluorocarbons, or hydrofluorocarbons, that linger in the atmosphere for just a year to a few decades can cause sea levels to rise for hundreds of years after the pollutants have been cleared from the atmosphere.
If you think of countries like Tuvalu, which are barely above sea level, the question that is looming is how much we can emit before they are doomed. Are they already slated to go under, even if we stopped emitting everything tomorrow? says co-author Susan Solomon, the Ellen Swallow Richards Professor of Atmospheric Chemistry and Climate Science at MIT. Its all the more reason why its important to understand how long climate changes will last, and how much more sea-level rise is already locked in.
Encouragingly, the researchers found that the Montreal Protocol, while designed to protect the ozone layer by phasing out pollutants such as chlorofluorocarbons has also helped stem rising seas. If the Montreal Protocol had not been ratified, and countries had continued to emit chlorofluorocarbons to the atmosphere, the researchers found that by 2050, the world would have experienced up to an additional 6 inches of sea-level rise.
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http://dx.doi.org/10.1073/pnas.1612066114