Streamflow from northern Eurasia into the Arctic Ocean has been increasing since the 1930s. Research shows that increased poleward moisture transport is responsible for additional water in the region.
References
Chapin, F. et al. Science 310, 657 (2005).
Peterson, B. J. et al. Science 298, 2171–2173 (2002).
Zhang, X. et al. Nature Clim. Change 3, 47–51 10.1038/nclimate1631(2013).
Serreze, M. C. et al. Geophys. Res. Lett 30, 1110 (2003).
Adam, J. C. & Lettenmaier, D. P. J. Geophys. Res. 108, 4257 (2003).
Kistler, R. et al. Bull. Am. Meteorol. Soc. 82, 247–268 (2001).
McClelland, J. W., Holmes, R. M., Peterson, B. J. & Stieglitz, M. J. Geophys. Res. 109, D10182 (2004).
Rawlins, M. A., Ye, H., Yang, D., Shiklomanov, A. & Mcdonald, K. C. J. Geophys. Res. 114, D18119 (2009).
Troy, T. J., Sheffield, J. & Wood, E. F. J. Geophys. Res. 117, D05131 (2012).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Troy, T. Wetting the Arctic. Nature Clim Change 3, 17–18 (2013). https://doi.org/10.1038/nclimate1790
Published:
Issue Date:
DOI: https://doi.org/10.1038/nclimate1790
- Springer Nature Limited