Abstract Groundwater 18O/16O, 2H/1H, 13C/12C, 3H, and 14C data can help quantify
molecular movements and chemical reactions governing groundwater recharge, quality …

Inland water carbon (C) sequestration rates play a potentially important role in the balance
between C supplies from the atmosphere and associated watersheds and the net demand of …

Hydraulic conductivity function for frozen soils (HCFF) is crucial for accurately simulating the
water transfer process in cold regions, impacting hydrological states and frost heave …

Through taliks—thawed zones extending through the entire permafrost layer—represent a
critical type of heterogeneity that affects water redistribution and heat transport, especially in …

The fate of the vast stocks of organic carbon stored in permafrost of the Western Siberian
Lowland, the world's largest peatland, is uncertain. Specifically, the amount of greenhouse …

Accelerating multiphase water transformation affects runoff processes and components
greatly and have changed the spatiotemporal patterns of water resources in the Third Polar …

Both gradual and abrupt changes in lake surface area in permafrost regions are crucial for
understanding the water cycles in cold regions under climate change. However, seasonal …

Riverine export fluxes of organic carbon (OC), major and trace elements remain at the
forefront of environmental research in Arctic and subarctic regions, due mostly to high …

The hydrogen and oxygen isotope composition of precipitation and water vapor are useful
tracers in the water cycle. The water balance of inland river basins located in the monsoon …

Climatic warming has resulted in permafrost degradation and it is expected to alter the
hydrological processes and hydraulic connectivity on the Qinghai-Tibet Plateau (QTP) …