Meltwater and cold pump effects override climate control of grain size in polythermal glacier ice. [PDF]
Li Y, Fu C.
europepmc +1 more source
Systematic Review of Metallic, Industrial, and Pharmaceutical Emerging Contaminants in Snow and Ice: A Global Perspective from Polar and High-Mountain Regions. [PDF]
Spagnesi A +4 more
europepmc +1 more source
Automated satellite-based glacial lake inventory and change detection in High Mountain Asia. [PDF]
Kumar R, Vijay S.
europepmc +1 more source
Meeting Review of the Cryospheric Ecosystems Conference, 1-4 September 2025, Poznań, Poland. [PDF]
Skoczeń K +6 more
europepmc +1 more source
Future projections of glacier mass change in High Mountain Asia using GRACE and climatemodel data. [PDF]
Dharpure JK, Howat IM, Patel A.
europepmc +1 more source
The Earth's Greatest Porous Media
Abstract How deeply does modern meteoric water circulate into the continental crust? How deep is the Earth's Critical Zone (CZ), the top layer of the continental lithosphere that co‐evolves with the atmosphere, hydrosphere, and biosphere, extending from vegetation canopy down to fresh bedrock and the base of active groundwater circulation?
Ying Fan +3 more
wiley +1 more source
Preparing for cascading hazards in High Mountain Asia. [PDF]
Wang X, Fan X, Bhuyan K.
europepmc +1 more source
Increasing Respiration Weakens the Carbon Sink Over Two Decades in a Temperate Deciduous Forest
Using a 20‐year eddy covariance record from a temperate deciduous forest, we show that net carbon uptake declined over two decades. Both the trend and interannual variability in net carbon exchange were respiration driven, with warming winters and increasing late‐summer diffuse light driving the trend in respiration.
Darby D. Bergl +8 more
wiley +1 more source
Spatial and temporal variability of supraglacial algae on an Alpine glacier (Forni Glacier, Italy). [PDF]
Dory F +21 more
europepmc +1 more source
Composition and Provenance of Victoria Group Sandstones in Southern North Victoria Land, Antarctica
Three distinct source areas contributed to sandstones of the Victoria Group within the Transantarctic Basin in southern North Victoria Land. During the Permian, quartzose sandstones were derived from erosion of the local Ross Orogen, likely from an uplifted swell in the area of today's Ross Sea, the Ross High.
Martin Elsner +6 more
wiley +1 more source

