– Scientific coordinator : Florent Gimbert (IGE, UGA)
Introduction
Glacier dynamics regulates the advection of ice towards lower elevations with higher temperature and melt rates, and thus controls the supply of fresh water to populations for mountain glaciers (Huss et al., 2014) and to oceans for ice sheets (Ritz et al., 2015). Compared to viscous flow, glacier fracturing, basal sliding and subglacial hydrology are processes that remain poorly known since they remain challenging to (…)
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