Runoff estimates from the Greenland ice sheet carry uncertainty because the fate of surface melt in permanently snow-covered regions is unconstrained. In situ and airborne observations reveal large-scale liquid water storage in buried layers of aged and compacted snow.
References
Forster, R. R. et al. Nature Geosci. 7, 95–98 (2013).
Wouters, B., Bamber, J. L., van den Broeke, M. R., Lenaerts, J. T. M. & Sasgen, I. Nat. Geosci. 6, 613–616 (2013).
Fettweis, X., Tedesco, M., van den Broeke, M. & Ettema, J. Cryosphere 5, 359–375 (2011).
Humphrey, N. F., Harper, J. T. & Pfeffer, W. T. J. Geophys. Res. 117, F01010 (2012).
Benson, C. S. Research Report 120 (US Army Corps of Engineers, 1962).
Müller, F. J. Glaciol. 16, 119–133 (1976).
Braithwaite, R. J., Laternser, M. & Pfeffer, W. T. J. Glaciol. 40, 477–485 (1994).
Marsh, P. & Woo, M-K. Wat. Resour. Res. 20, 1853–1864 (1984).
Pfeffer, W. T., Illangasekare, T. H. & Meier, M. F. J. Glaciol. 36, 238–246 (1990).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Harper, J. Greenland's lurking aquifer. Nature Geosci 7, 86–87 (2014). https://doi.org/10.1038/ngeo2061
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo2061
- Springer Nature Limited