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

Understanding Greenland ice sheet (GrIS) hydrology is essential for evaluating response of
ice dynamics to a warming climate and future contributions to global sea level rise. Recently …

The hydrology of many important river systems in the world is influenced by the presence of
glaciers in their upper reaches. We assess the global‐scale response of glacier runoff to …

The micronutrient iron is thought to limit primary productivity in large regions of the global
ocean. Ice sheets and glaciers have been shown to deliver bioavailable iron to the coastal …

The influence of meltwater on the dynamics and geomorphic impact of the Greenland Ice
Sheet is strongly controlled by the morphology of the ice sheet's drainage system. However …

Glacial meltwater exports a unique type of organic carbon to marine systems, distinct from
non-glacially derived riverine export, potentially capable of stimulating downstream marine …

In Greenland, tidewater glaciers discharge turbid subglacial freshwater into fjords, forming a
plume near the calving front. To elucidate the effects of this discharge on nutrient and …

Coupling between runoff, hydrology, basal motion, and mass loss (“hydrology-dynamics”) is
a critical component of the Greenland Ice Sheet system. Despite considerable research …

To effectively restore the groundwater environment of the Shiping Mine (SPM) area, which is
contaminated by acid mine drainage (AMD), a hydrogeochemical conceptual model was …

Soil water is an important driving force of the ecosystems, especially in the semiarid hill and
gully region of the northwestern Loess Plateau in China. The mechanism of soil water …