Results 251 to 260 of about 86,378 (349)

Drilling Within the Critical Zone

open access: yesHydrological Processes, Volume 40, Issue 3, March 2026.
This review synthesises 30 years of critical zone drilling methodologies for studying subsurface weathering, water storage, and biogeochemical processes. We evaluate drilling techniques, sampling strategies, downhole logging, and long‐term monitoring approaches while addressing contamination control and core preservation challenges.
Amanda Donaldson   +14 more
wiley   +1 more source

Water Oxygen Isotope Thermometer in Headwaters: Indicating Groundwater Recharge and Peatland Water Dependence on Air Temperature

open access: yesHydrological Processes, Volume 40, Issue 3, March 2026.
Stable isotopes in water act as natural tracers of precipitation temperature. In mountainous environments, the oxygen isotopic signature measured in stream water reflects air temperature during precipitation events. Oxygen‐isotope‐derived temperatures are closely linked to recharge processes, particularly in peatlands, as well as in groundwater systems.
Stéphane Binet   +9 more
wiley   +1 more source

Climate Change in the Upper Tagus River Basin: Impacts on Climate Variables and Hydrological Processes

open access: yesHydrological Processes, Volume 40, Issue 3, March 2026.
Climate change impacts on hydrological processes were evaluated in the most populated basin in the Iberian Peninsula. Temperature increase, together with precipitation reduction, will raise evapotranspiration rate, reducing water availability for hydrological processes.
Alejandro Sánchez‐Gómez   +1 more
wiley   +1 more source

A non-optically active lake salinity dataset by satellite remote sensing. [PDF]

open access: yesSci Data
Deng M   +7 more
europepmc   +1 more source

Distributed Sediment Delivery at Masse Experimental Basin (Central Italy)

open access: yesHydrological Processes, Volume 40, Issue 3, March 2026.
The SEDD model is applied in an equipped basin of 231 ha. Sediment delivery processes are governed by a single parameter, βe, which scales with runoff coefficient, QR. For high‐intensity events (QR > 0.15), the functional component of connectivity becomes invariant, suggesting that sediment transport is driven solely by the basin's structural ...
Vincenzo Palmeri   +6 more
wiley   +1 more source

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