Articles | Volume 12, issue 10
https://doi.org/10.5194/tc-12-3383-2018
https://doi.org/10.5194/tc-12-3383-2018
Research article
 | 
29 Oct 2018
Research article |  | 29 Oct 2018

Basal control of supraglacial meltwater catchments on the Greenland Ice Sheet

Josh Crozier, Leif Karlstrom, and Kang Yang

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Cited articles

Ahlstrøm, A. P., Petersen, D., Langen, P. L., Citterio, M., and Box, J. E.: Abrupt shift in the observed runoff from the southwestern Greenland ice sheet, Sci. Adv., 3, 12, https://doi.org/10.1126/sciadv.1701169, 2017. a
Andersen, M. L., Stenseng, L., Skourup, H., Colgan, W., Khan, S. A., Kristensen, S. S., Andersen, S. B., Box, J. E., Ahlstrøm, A. P., Fettweis, X., and Forsbergb, R.: Basin-scale partitioning of Greenland ice sheet mass balance components (2007–2011), Earth Planet. Sc. Lett., 409, 89–95, https://doi.org/10.1016/j.epsl.2014.10.015, 2015. a, b
Andrews, L. C., Catania, G. A., Hoffman, M. J., Gulley, J. D., Lüthi, M. P., Ryser, C., Hawley, R. L., and Neumann, T. A.: Direct observations of evolving subglacial drainage beneath the Greenland Ice Sheet, Nature, 514, 80–83, https://doi.org/10.1038/nature13796, 2014. a
ArcticDEM: DEMs provided by the Polar Geospatial Center under NSF OPP awards 1043681, 1559691 and 1542736, The University of Minnesota, available at: https://www.pgc.umn.edu/data/arcticdem/ (last access: 7 January 2018), 2017. a, b, c
Banwell, A. F., Arnold, N. S., Willis, I. C., Tedesco, M., and Ahlstrøm, A. P.: Modeling supraglacial water routing and lake filling on the Greenland Ice Sheet, J. Geophys. Res.-Earth, 117, F04012, https://doi.org/10.1029/2012JF002393, 2012. a
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Short summary
Understanding ice sheet surface meltwater routing is important for modeling and predicting ice sheet evolution. We determined that bed topography underlying the Greenland Ice Sheet is the primary influence on 1–10 km scale ice surface topography, and on drainage-basin-scale surface meltwater routing. We provide a simple means of predicting the response of surface meltwater routing to changing ice flow conditions and explore the implications of this for subglacial hydrology.