Results 251 to 260 of about 3,473 (303)

Spatial and Temporal Patterns of Alkalinity in an Alpine Headwater Stream Network: Linking Catchment Heterogeneity to Carbon Dynamics

open access: yesJournal of Geophysical Research: Biogeosciences, Volume 131, Issue 6, June 2026.
Abstract Alkalinity is a key regulator of carbon dioxide (CO2 ${\text{CO}}_{2}$) dynamics in freshwater systems, influencing both dissolved inorganic carbon speciation and the buffering capacity of water. Despite its importance, alkalinity in freshwater environments remains comparatively underexplored relative to ocean systems.
Francesco Presotto   +4 more
wiley   +1 more source

The diversity and abundance of chytrids on the Greenland Ice Sheet. [PDF]

open access: yesSci Rep
Perini L   +6 more
europepmc   +1 more source

History Matching of Soil Moisture and Evapotranspiration Over Europe Using Iterative Ensemble Smoothers

open access: yesJournal of Advances in Modeling Earth Systems, Volume 18, Issue 6, June 2026.
Abstract Land surface models are crucial components within earth system models, simulating the exchanges of water, energy, carbon, and nitrogen between the land surface, atmosphere, and subsurface. One challenge is the large number of uncertain parameters in these models.
Mikael L. A. Kaandorp   +5 more
wiley   +1 more source

Observed positive feedback between surface ablation and crevasse formation drives glacier acceleration and potential surge. [PDF]

open access: yesNat Commun
Nanni U   +11 more
europepmc   +1 more source

Irreversible glacier change and trough water for centuries after overshooting 1.5 °C. [PDF]

open access: yesNat Clim Chang
Schuster L   +7 more
europepmc   +1 more source

Outburst of a subglacial flood from the surface of the Greenland Ice Sheet. [PDF]

open access: yesNat Geosci
Bowling JS   +19 more
europepmc   +1 more source

Progress in glacier hydrology: a Canadian perspective

Hydrological Processes, 2000
Glacier variations are signals of global change. Current estimates are that ice is being lost from small glaciers of the world at the rate of approximately 130 mm year -1 and that the impact of this alone would be to change sea level upward, by 0.25 mm year -1 .
D Scott Munro
exaly   +2 more sources

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