Low surface water storage (3.6 ± 0.9 cm), negligible impoundment
by supraglacial lakes or topographic depressions, and high discharge to moulins (2.54 — 2.81 cm ⋅ d − 1) indicate that the surface drainage system conveyed its own storage volume every < 2 d to the bed.
The role of supraglacial lakes in this has been a point of emphasis; Luthje et al, (2006) noted that the area covered
by supraglacial lakes was independent of the summer melt rate, but controlled by topography.
Not exact matches
Breakup of the Larsen B Ice Shelf triggered
by chain reaction drainage of
supraglacial lakes (pages 5872 — 5876) Alison F. Banwell, Douglas R. MacAyeal and Olga V. Sergienko Article first published online: 27 NOV 2013 DOI: 10.1002 / 2013GL057694 Key Points Larsen B Ice Shelf rapidly broke ‐ up
by chain ‐ reaction drainage of surface
lakes Lake ‐ induced stress set fracture spacing small enough for capsize ‐ driven breakup
Lake interaction
by flexural stress defines an ice ‐ shelf stability tipping point (http://onlinelibrary.wiley.com/doi/10.1002/2013GL057694/abstract)
Ryder Glacier is much different: Howat and others (2008) note that Ryder Glacier, North Greenland, accelerated
by 300 % over a 7 week period following drainage of a
supraglacial lake in 1995.