Locating a complex subglacial drainage network using seismic arrays on Glacier d’Otemma, Switzerland
Journal of Glaciology, vol. 72
Abstract
Abstract Glaciers actively store and release meltwater with significant impacts on glacier flow velocity and downstream environments. The evolution of this drainage system is a key component in understanding glacier dynamics. In temperate alpine glaciers, the change of the subglacial drainage network from distributed to channelised is theoretically known, but lacks empirical documentation. As subglacial channels are extremely difficult to access, it is important to test innovative methods for locating them. Here, we use surface seismic monitoring, which enables us to identify the location of multiple subglacial channels below Glacier d’Otemma, Valais, Switzerland. We calculate time delays between pairs of seismic sensors and backtrack source locations. Using matched field processing and beamforming analysis, we obtain spatial and temporal patterns of seismic noise produced by the glacier. This allows us to interpret a possible evolution of the subglacial drainage network from a distributed to an efficient one and locate three distinct subglacial channels in close proximity.
Authors 8
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Eva Wolf corresponding
Affiliation as printed
Université de Lausanne
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Institut de physique du globe de Paris
Affiliation as printed
Institut de Physique du Globe de Paris
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Institut de physique du globe de Paris
Affiliation as printed
Institut de Physique du Globe de Paris
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Affiliation as printed
University of Oslo Faculty of Mathematics and Natural Sciences
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Affiliation as printed
Université de Lausanne
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Affiliation as printed
Université de Lausanne
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Michael Dietze Aachen
Affiliation as printed
RWTH Aachen University
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Affiliation as printed
Université de Lausanne
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