Vast regions of the northern hemisphere are exposed to snowfall and seasonal frost. This
has large effects on spatiotemporal distribution of infiltration and groundwater recharge …

The amount and patterning of precipitation beneath vegetation is determined by throughfall
and stemflow. Throughfall is the portion of precipitation that falls through, or drips from, the …

Thirty‐three snowpack models of varying complexity and purpose were evaluated across a
wide range of hydrometeorological and forest canopy conditions at five Northern …

A series of process‐based algorithms has been developed to describe the accumulation,
unloading and sublimation of intercepted snow in forest canopies. These algorithms are …

The results of a 3 year field study to observe the processes controlling snow interception by
forest canopies and under canopy snow accumulation and ablation in mountain maritime …

Accumulation of snow under forest canopies is known to decline with increasing canopy
density and leaf area because of snow interception and sublimation in the canopy. Seasonal …

A comprehensive, physically based model of snow accumulation, redistribution, sublimation,
and melt for open and forested catchments was assembled, based on algorithms derived …

Feedbacks, or internal interactions, play a crucial role in the climate system. Negative
feedback will reduce the impact of an external perturbation, a positive feedback will amplify …

Western US forest ecosystems and downstream water supplies are reliant on seasonal
snowmelt. Complex feedbacks govern forest–snow interactions in which forests influence …

Hydrology and Global Environmental Change presents the hydrological contribution to, and
consequences of, global environmental change. Assuming little or no prior knowledge on …