Abstract
Replying to Peel and McMahon
Peel and McMahon1 argue that limitations of the continental runoff data set2 we use in our study3 call our main conclusion into question — that is, that changes in twentieth-century continental-scale runoff are partly attributable to the suppression of CO2-induced stomatal closure. We support Peel and McMahon's pleas for better and more complete runoff data, but we remain confident in our conclusions, as explained here.
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References
Peel, M. C. & McMahon, T. A. Nature 444, doi: 10.1038/nature05480 (2006).
Labat, D., Goddéris, Y., Probst, J. L. & Guyot, J. L. Adv. Water Resour. 27, 631–642 (2004).
Gedney, N. et al. Nature 439, 835–838 (2006).
Legates, D. R., Lins, H. F. & McCabe, G. J. Adv. Water Resour. 28, 1310–1315 (2005).
Shiklomanov, I. A. Water Int. 25, 11–31 (2000).
Gornitz, V., Rosenzweig, C. & Hillel, D. Global Planet. Change 14, 147–161 (1997).
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Gedney, N., Cox, P., Betts, R. et al. A quality-controlled global runoff data set (Reply). Nature 444, E14–E15 (2006). https://doi.org/10.1038/nature05481
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DOI: https://doi.org/10.1038/nature05481
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