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Chapin, F. S; Sturm, M; Serreze, M. C; McFadden, J. P; Key, J. R; Lloyd, A. H; McGuire, A. D; Rupp, T. S; Lynch, A. H; Schimel, J. P; Beringer, J; Chapman, W. L; Epstein, H. E; Euskirchen, E. S; Hinzman, L. D; Jia, G; Ping, C.-L; Tape, K. D; Thompson, C. D. C; Walker, D. A; Welker, J. M
Science, 10/2005, Letnik: 310, Številka: 5748Journal Article
A major challenge in predicting Earth's future climate state is to understand feedbacks that alter greenhouse-gas forcing. Here we synthesize field data from arctic Alaska, showing that terrestrial changes in summer albedo contribute substantially to recent high-latitude warming trends. Pronounced terrestrial summer warming in arctic Alaska correlates with a lengthening of the snow-free season that has increased atmospheric heating locally by about 3 watts per square meter per decade (similar in magnitude to the regional heating expected over multiple decades from a doubling of atmospheric CO₂). The continuation of current trends in shrub and tree expansion could further amplify this atmospheric heating by two to seven times.
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JCR | SNIP | JCR | SNIP | JCR | SNIP | JCR | SNIP |
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in: SICRIS
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