12 At its height from 1906 to 1910, estimated warming from soot on Arctic snow was eight times that of the pre-industrial era, the researchers said.
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11. Soot, mostly from burning coal, reduces the reflectivity of snow and ice, letting Earth\'s surface absorb more solar energy and possibly resulting in earlier snow melts and exposure of much darker underlying soil, rock and sea ice. This in turn led to warming across much of the Arctic region. 20\'
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