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Hydrologiska Byråns Vattenbalansavdelning (HBV)
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Description
High-resolution integrated hydrological modeling using coupled PRMS-MODFLOW system to simulate surface water and groundwater interactions extending 400 m into subsurface. Model accounts for complex terrain, vegetation dynamics, and groundwater-surface water exchange processes.
Typical Equipment
- GSFLOW
- PRMS
- MODFLOW
- Seequent's three-dimensional Leapfrog geological modelling software
Output Measurements
- streamflow
- groundwater levels
- water table depth
- groundwater storage
- evapotranspiration
- recharge rates
Papers Using This Protocol (15)
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Controls from above and below: Snow, soil, and steepness drive diverging trends of subsurface water and streamflow dynamics
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Declining groundwater storage expected to amplify mountain streamflow reductions in a warmer world
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Dwindling Groundwater Reserves Will Threaten Mountain Streamflow in a Warmer World
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On the similarity of hillslope hydrologic function: a clustering approach based on groundwater changes
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Quantifying Subsurface Flow and Solute Transport in a Snowmelt-Recharged Hillslope With Multiyear Water Balance
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Understanding the Hydrogeochemical Response of a Mountainous Watershed Using Integrated Surface-Subsurface Flow and Reactive Transport Modeling
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The effects of spatial and temporal resolution of gridded meteorological forcing on watershed hydrological responses
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Direct Observation of the Depth of Active Groundwater Circulation in an Alpine Watershed
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Modeling geogenic and atmospheric nitrogen through the East River Watershed, Colorado Rocky Mountains
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Resolution matters when modeling climate change in headwaters of the Colorado River
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Baseflow Age Distributions and Depth of Active Groundwater Flow in a Snow Dominated Mountain Headwater Basin
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The importance of interflow to groundwater recharge in a snowmelt-dominated headwater basin
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Exploring source water mixing and transient residence time distributions of outflow and evapotranspiration with an integrated hydrologic model and Lagrangian particle tracking approach
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Depth- and time-resolved distributions of snowmelt-driven hillslope subsurface flow and transport and their contributions to surface waters.
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