Arctic permafrost stores nearly 1,700 billion metric tons of frozen and thawing carbon.
Anthropogenic warming threatens to release an unknown quantity of this carbon to the …

Driven by the need for integrated management of groundwater (GW) and surface water
(SW), quantification of GW–SW interactions and associated contaminant transport has …

The cryosphere (including, snow, glaciers, permafrost, lake and river ice) is an integral
element of high mountain regions, which are home to roughly 10% of the global population …

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 …

Coastal groundwater (CGW) is a critical water resource for many communities and can be a
key part of coastal ecosystems. Owing to its location, CGW faces both terrestrial and marine …

Despite the increasing Siberian river discharge, the sensitivity of streamflow to climate
forcing/permafrost thawing is poorly quantified. Based on the Budyko framework and …

Observations indicate that groundwater-laden sedimentary aquifers are extensive beneath
large portions of the Greenland and Antarctic ice sheets. A reduction in the mechanical …

Under a warming climate, permafrost degradation has resulted in profound hydrogeological
consequences. Here, we mainly review 240 recent relevant papers. Permafrost degradation …

Under the background of global warming, permafrost on the Qinghai-Tibet Plateau has been
experienced a significant degradation, which may have effects on regional climate …

Global climate warming disproportionately affects high-latitude and mountainous terrestrial
ecosystems. Warming is accompanied by permafrost thaw, shorter winters, earlier snowmelt …