Abstract In 2015, the Olympic Mountains contained 255 glaciers and perennial snowfields
totaling 25.34±0.27 km2, half of the area in 1900, and about 0.75±0.19 km3 of ice. Since …

During the past decades, glacier mass loss is becoming increasingly significant worldwide
but knowledge about the acceleration is still limited despite its potentially profound impacts …

Inversion of low‐frequency regional seismic records to solve for a time series of bulk forces
exerted on the earth by a landslide (a force‐time function) is increasingly being used to infer …

Glacier mass balance models are needed at sites with scarce long-term observations to
reconstruct past glacier mass balance and assess its sensitivity to future climate change. In …

Climate change is driving the loss of alpine glaciers globally, yet investigations about the
water quality of rivers stemming from them are few. Here we provide an overview …

Glacier mass loss in Alaska has implications for global sea level rise, fresh water input into
the Gulf of Alaska and terrestrial fresh water resources. We map all glaciers (> 4000 km2) on …

Hydrological systems across the globe are increasingly subjected to pressures from a
warming climate and anthropogenic disturbance. Responses to stress can be nonlinear and …

Finely resolved geodetic data provide an opportunity to assess the extent and morphology of
crevasses and their change over time. Crevasses have the potential to bias geodetic …

Glaciers in western North American outside of Alaska are often overlooked in global studies
because their potential to contribute to changes in sea level is small. Nonetheless, these …

Globally, glaciers are shrinking in response to climate change, with implications for global
sea level rise as well as downstream ecosystems and water resources. Sliding at the ice …