Journal of Glaciology · 1983 · 11 citations · 8 references
Natural SciencesEarth SciencesGlaciologySediment TransportSedimentologyGlacial HydrologyGlacial SedimentationGlacial SedimentologyGlacier Mass BalanceSediment DynamicsWater FlowGlacial Sediment DischargeGlacial Sediment TransportSediment ConcentrationSediment Load In Glacial SystemsSuspended Sediment BudgetSuspended Sediment ConcentrationSuspended Sediment DynamicsSuspended Sediment Removal
Abstract Between 16 and 19 June 1981 a large water pocket of volume 183 000 m 3 burst from glacier de Tsidjiore Nouve. From hourly stream discharge and suspended sediment concentration observations a suspended sediment output of 1 674 × 10 3 kg was calculated. The transport of bed-load was estimated at 3 840 × 10 3 kg, hence a total quantity of around 5 500 × 10 3 kg of sediment were removed from the catchment, including the pro-glacial field, in the four days of the outburst.
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