Unraveling driving forces explaining significant reduction in satellite-inferred Arctic surface albedo since the 1980s.

1 A shows a decreasing trend in both satellite-inferred and modeled multimonth mean Arctic surface albedo from 1982 to 2014.

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A recent observational study ( 19 ) shows a positive trend in the annual-mean solar radiation absorbed over the Arctic ocean that is about twice the trend over the Arctic land during 1982 to 2015, presumably, due to differences in albedo reduction over land and ocean.

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The CAM5 precipitation rate shows an increasing trend (6.93 mm decade −1 ) as the Arctic warms (0.43 K decade −1 for SAT).

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