Elevation-dependent warming in mountain regions of the world

Schoner, W; Pepin, N; Bradley, R. S.; Diaz, H. F.; Baraer, M.; Caceres, E. B.; Forsythe, N.; Fowler, H.; Greenwood, G; Hashmi, M. Z.; Liu, X D; Miller, J. R.; Ning, L; Ohmura, A; Palazzi, E; Rangwala, I.; Severskiy, I.; Shahgedanova, M.; Wang, M B; Williamson, S. N.; Yang, D Q

doi:10.1038/nclimate2563

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Elevation-dependent warming in mountain regions of the world

Author(s): N. Pepin , R. S. Bradley , H. F. Diaz , M. Baraer , E. B. Caceres , N. Forsythe , H. Fowler , G. Greenwood , M. Z. Hashmi , X. D. Liu , J. R. Miller , L. Ning , A. Ohmura , E. Palazzi , I. Rangwala , W. Schöner , I. Severskiy , M. Shahgedanova , M. B. Wang , S. N. Williamson , D. Q. Yang

Publication date Created: April 23 2015

Publication date (Print): April 23 2015

Journal: Nature Climate Change

Publisher: Springer Nature

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Global and regional climate changes due to black carbon

Lalgudi V. Ramanathan, Mark Carmichael (2008)

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Role of land-surface changes in arctic summer warming.

F Chapin, M. Sturm, M Serreze … (2005)

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.