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Volcanic Eruptions Emerge as Lead Cause for Little Ice Age

The Little Ice Age began in the late 13th century, scientists now posit, and lasted about 400 years. Some regions cooled significantly. A series of volcanic eruptions has become a leading culprit.

Sequences of explosive volcanic eruptions in the tropics were the likely trigger for the Little Ice Age, according to a new study.  The research attempts to answer two longstanding questions swirling around the roughly 400-year span of slightly cooler-than normal temperatures: Exactly when did it begin? And what was its initial trigger? Previous estimates for the onset of the Little Ice Age range from as early as the late 1200s to as late as the 1500s, the research team notes. Globally, temperatures averaged a modest 0.6 degrees Celsius, or about 1 degree Fahrenheit cooler than usual.

Researchers have proposed a range of possible causes for the Little Ice Age – from decline in the sun’s output, volcanic activity, some combination of the two, or some form of natural variability within the climate system.

The problem either with a decline in the sun’s output, which happened during this period, or volcanism is that neither was powerful enough on its own to account for the cooling, says Gifford Miller, a climate scientist at the University of Colorado’s Institute of Arctic and Alpine.

Recent research on solar activity has indicated the sun didn’t dim as deeply as earlier research suggested. And volcanic activity typically affects climate only for a few years after an explosive eruption. It does this by hurling vast amounts of sulfur dioxide into the stratosphere, where the SO2 particles reflect sunlight back into space. Those particles eventually drift back into the lower atmosphere, where they get washed out of the sky during storms.

Instead, Dr. Miller’s team proposed that the initial trigger involved several major volcano eruptions occurring within about a decade of one another, followed by another set roughly 150 years later, which intensified the cooling.

The cooling effect of those eruptions, the team posits, probably triggered the growth of Arctic summer sea-ice cover and changes in North Atlantic ocean circulation. These changes reinforced the cooling trend, turning what might have been relatively short cool periods into a centuries-long chill.



January 31, 2012 - Posted by | Climate, Volcanic | , , ,

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