Articles | Volume 7, issue 5
The Cryosphere, 7, 1433–1445, 2013
The Cryosphere, 7, 1433–1445, 2013

Research article 23 Sep 2013

Research article | 23 Sep 2013

Evidence of meltwater retention within the Greenland ice sheet

A. K. Rennermalm1, L. C. Smith2, V. W. Chu2, J. E. Box3, R. R. Forster4, M. R. Van den Broeke5, D. Van As3, and S. E. Moustafa1 A. K. Rennermalm et al.
  • 1Department of Geography, Rutgers, The State University of New Jersey, New Brunswick, NJ, USA
  • 2Department of Geography, University of California Los Angeles, Los Angeles, CA, USA
  • 3Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark
  • 4Department of Geography, University of Utah, Salt Lake City, UT, USA
  • 5Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands

Abstract. Greenland ice sheet mass losses have increased in recent decades with more than half of these attributed to surface meltwater runoff. However, the magnitudes of englacial storage, firn retention, internal refreezing and other hydrologic processes that delay or reduce true water export to the global ocean remain less understood, partly due to a scarcity of in situ measurements. Here, ice sheet surface meltwater runoff and proglacial river discharge between 2008 and 2010 near Kangerlussuaq, southwestern Greenland were used to establish sub- and englacial meltwater storage for a small ice sheet watershed (36–64 km2). This watershed lacks significant potential meltwater storage in firn, surface lakes on the ice sheet and in the proglacial area, and receives limited proglacial precipitation. Thus, ice sheet surface runoff not accounted for by river discharge can reasonably be attributed to retention in sub- and englacial storage. Evidence for meltwater storage within the ice sheet includes (1) characteristic dampened daily river discharge amplitudes relative to ice sheet runoff; (2) three cold-season river discharge anomalies at times with limited ice sheet surface melt, demonstrating that meltwater may be retained up to 1–6 months; (3) annual ice sheet watershed runoff is not balanced by river discharge, and while near water budget closure is possible as much as 54% of melting season ice sheet runoff may not escape to downstream rivers; (4) even the large meltwater retention estimate (54%) is equivalent to less than 1% of the ice sheet volume, which suggests that storage in en- and subglacial cavities and till is plausible. While this study is the first to provide evidence for meltwater retention and delayed release within the Greenland ice sheet, more information is needed to establish how widespread this is along the Greenland ice sheet perimeter.