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 …

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 …

Abstract 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 …

Groundwater interactions with mountain streams are often simplified in model projections,
potentially leading to inaccurate estimates of streamflow response to climate change. Here …

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

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

Baseflow, the groundwater contribution to streamflow, sustains surface water between
precipitation events and is an important indicator of groundwater availability. Although many …

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 …

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 …