Mountain glaciers are rapidly retreating with consequences for
downstream hydrology, including changes in annual discharge, increased
seasonality, disappearance of melt-water fed springs and alterations to
ecology and water quality. The influence of glaciers on watershed
hydrology is complex temporally (from daily to seasonal to
inter-decadal timescales) and spatially (from the immediate proglacial
environment to regional scales). We invite contributions that study
these systems and the impacts of changes to them through, but not
limited to, field observations, glacier and water resources monitoring,
processes analysis, modeling, and/or remote sensing. This session is
not restricted to any specific region of the world.
We look forward to seeing you in San Francisco!