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Spatially variable response of Himalayan glaciers to climate change affected by debris cover
The present state and future evolution of Himalayan glaciers has been controversial. An analysis of remotely sensed frontal changes and surface velocities from glaciers in the greater HimalayaExpand
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Glacier-surface velocities in alpine terrain from optical satellite imagery—Accuracy improvement and quality assessment
The worldwide retreat of mountain glaciers has important consequences for the water, food, and power supply of large and densely populated areas in South and Central Asia. Successful mitigation ofExpand
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Short Communication: TopoToolbox 2 – MATLAB-based software for topographic analysis and modeling in Earth surface sciences
TLDR
TopoToolbox has become a more memory-efficient and faster tool for basic and advanced digital terrain analysis that can be used as a framework for building hydrological and geomorphological models in MATLAB. Expand
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Multiple fluvial processes detected by riverside seismic and infrasound monitoring of a controlled flood in the Grand Canyon
As rivers transport water and sediment across Earth's surface, they radiate elastic and acoustic waves. We use seismic and infrasound observations during a controlled flood experiment (CFE) in theExpand
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Tectonic control of Yarlung Tsangpo Gorge revealed by a buried canyon in Southern Tibet
The Himalayan mountains are dissected by some of the deepest and most impressive gorges on Earth. Constraining the interplay between river incision and rock uplift is important for understandingExpand
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Seasonal precipitation gradients and their impact on fluvial sediment flux in the Northwest Himalaya
Abstract Precipitation in the form of rain and snowfall throughout the Himalaya controls river discharge and erosional processes and, thus, has a first-order control on the fluvial sediment flux.Expand
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Hillslope‐glacier coupling: The interplay of topography and glacial dynamics in High Asia
[1] High Asian glacial landscapes have large variations in topographic relief and the size and steepness of snow accumulation areas. Associated differences in glacial cover and dynamics allow aExpand
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Global Assessment of Supraglacial Debris‐Cover Extents
Rocky debris on glacier surfaces influences ice melt rates and the response of glaciers to climate change. However, scarce data on the extent and evolution of supraglacial debris cover have so farExpand
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Timing and extent of late Quaternary glaciation in the western Himalaya constrained by 10Be moraine dating in Garhwal, India
Glacial chronologies from the Himalayan region indicate various degrees of asynchronous glacial behavior. Part of this has been related to different sensitivities of glaciers situated in contrastingExpand
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