Results 121 to 130 of about 4,218 (261)

Potential of Sentinel-3 snow cover fraction data for improving hydrological simulations at the regional scale. [PDF]

Sci Rep
Tanhapour M, Parajka J, Schwaizer G, Vreugdenhil M, Kohnová S, Hlavčová K, Výleta R, Szolgay J.   +7 more
europepmc   +1 more source

When Snowpacks Shrink: Declining Weathering and Export Rates but Rising Stream Solute Concentrations in Warming Mountains

Hydrological Processes, Volume 40, Issue 5, May 2026.
In a snow‐dominated headwater catchment, snow‐dependent water storage controls silicate weathering and solute export. In the driest year with the least snow water equivalent (SWE), rates of silicate weathering and export rates of weathering products were about half and a third of those in the wettest year with the highest SWE.
Abigail S. Knapp, Bryn Stewart, Devon Kerins, Pamela L. Sullivan, Holly R. Barnard, Li Li   +5 more
wiley   +1 more source

Erratum: Host-virome associations in the weathering crust of a rapidly retreating temperate Alpine glacier. [PDF]

Microb Genom
Varliero G, Bauder A, Stierli B, Qi W, Frey B.   +4 more
europepmc   +1 more source

Land Cover Change Drives River Flow Modifications in Central Chile

Hydrological Processes, Volume 40, Issue 5, May 2026.
This study examines the combined effects of land cover change and ENSO on streamflow dynamics in four coastal catchments of central Chile, using a 45‐year (1979–2023) dataset of remote sensing and hydroclimatic data. Conclusions Native forest loss reduced summer flows and PP–Q relationship; preserved forests enhanced resilience.
Rossana Escanilla‐Minchel, Joseph Holden, Mark Smith   +2 more
wiley   +1 more source

Wetlands set the pace of annual runoff in the northern Great Plains. [PDF]

Commun Earth Environ
Rahmani J, Creed IF, Badiou P, Ameli AA.
europepmc   +1 more source

Spatial Layout of Trees on Farms Influences Magnitude and Timing of River Flow Peak

Hydrological Processes, Volume 40, Issue 5, May 2026.
Effectiveness of agroforestry as a lowland NFM strategy is spatially modelled for a range of planting layouts. Peak flow for a 10‐year storm was attenuated by 2.6% and delayed by 19 min with just 0.6% catchment tree coverage under riparian planting alone. Increasing coverage provided a strongly diminishing return in flood peak attenuation.
Josiah B. Judson, Pippa J. Chapman, Marcelo V. Galdos, Joseph Holden   +3 more
wiley   +1 more source

Two-year daily precipitation stable isotope dataset (δ¹⁸O and δ²H) from a continental station in NW Croatia. [PDF]

Data Brief
Briški M, Palatinuš I, Bajo P, Brčić V.   +3 more
europepmc   +1 more source

Stemflows and Preferential Flows: A Historical Review and Challenges for the Future

Hydrological Processes, Volume 40, Issue 5, May 2026.
Possible implementation of stemflow in the MIPS model where all water in the system is represented as particles in pathways of specified velocity. Stemflow (green particles) can be treated as a localised input with probabilities of entering higher velocity pathways than throughfall, depending on the input rates.
Keith Beven, John T. Van Stan
wiley   +1 more source

Hybrid physical-statistical framework for seasonal streamflow forecasting in the Upper Feather River Basin, California. [PDF]

Sci Rep
Ozcan Z, Iseri Y, Ulloa F, Imbulana N, Snider E, Mure-Ravaud M, Anderson ML, Kavvas ML.   +7 more
europepmc   +1 more source

Persistent Evapotranspiration in a Shallow Boreal Shield Peatland Despite Summer Drought: Implications for Ecohydrological Resilience

Hydrological Processes, Volume 40, Issue 5, May 2026.
We examine energy balance and evapotranspiration dynamics in a shallow peatland as an analogue for projected climate change impacts in deeper peatlands. Across nine growing seasons, we document similar total evapotranspiration between dry and wet years, leading to net moisture deficit in some dry years.
K. L. Simone, P. A. Moore, B. Van Huizen, J. M. Waddington   +3 more
wiley   +1 more source