Anthropogenic climate change is decreasing seasonal snowpacks globally, with potentially
catastrophic consequences on water resources, given the long-held reliance on snowpack …

Groundwater is by far the largest unfrozen freshwater resource on the planet. It plays a
critical role as the bottom of the hydrologic cycle, redistributing water in the subsurface and …

A decade-long (2010–2020) period with precipitation deficits in central–south Chile (30–
41∘ S), the so-called megadrought (MD), has led to streamflow depletions of larger …

Headwater catchments are the fundamental units that connect the land to the ocean.
Hydrological flow and biogeochemical processes are intricately coupled, yet their respective …

Mountain‐block recharge (MBR) is the subsurface inflow of groundwater to lowland aquifers
from adjacent mountains. MBR can be a major component of recharge but remains difficult …

The mountain cryosphere and groundwater play pivotal roles in sha** the hydrological
cycle, yet their connectivity remains incompletely understood. Current knowledge on …

The western US is experiencing increasing rain to snow ratios due to climate change, and
scientists are uncertain how changing recharge patterns will affect future groundwater …

Bedrock property quantification is critical for predicting the hydrological response of
watersheds to climate disturbances. Estimating bedrock hydraulic properties over watershed …

Isotopic information from 81 snowpits was collected over a 5‐year period in a large,
Colorado watershed. Data spans gradients in elevation, aspect, vegetation, and seasonal …

The streamflow seasonality in mountain catchments is often influenced by snow. However, a
shift from snowfall to rain is expected in the future. Consequently, a decrease in snow …