© International Glaciological Society The role of sedirn.ent transport in the rn.echanics of jokulhlaups
ABSTRACT. The classical theory of jokulhlaups used Rothlisberger's earlier theory of ice-channel drainage to describe the development of the Oood hydrograph. This theory has some drawbacks: the mechanism o [ initiation (breaking the seal) is opaque, the l\i[anning roughness coefficient is too l...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.303.3044 http://www.maths.ox.ac.uk/%7Efowler/papers/1996.3.pdf |
| Summary: | ABSTRACT. The classical theory of jokulhlaups used Rothlisberger's earlier theory of ice-channel drainage to describe the development of the Oood hydrograph. This theory has some drawbacks: the mechanism o [ initiation (breaking the seal) is opaque, the l\i[anning roughness coefficient is too large and the hydrographs can reveal a sudden switching from channel opening to channel closure which is not simulated by the model. In this paper, we examine these features by exploring a more detailed model, which takes into account the physics of sediment erosion and its effect on channel morphology. \Ve propose a theory in which channels need not be semicircular, but have shapes determined by a local balance between closure and melting, and in which erosion of the tunnel margins is taken into account; in particular, we deri\'e theoretical predictions for sediment discharge, and we also propose a mechanism whereby the pressure seal over the caldera rim at Grimsvotn in Vatnajokull, Iceland, can be broken when the lake-level water pressure is still some 6 bar below the maximum overburden ice pressure. 1. |
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