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Full-Text Articles in Physical Sciences and Mathematics
Quantifying Evapotranspiration And Water Table Interactions In Regions Of Shallow Groundwater: Sensitivity To Soil Properties, Vegetation, And Climate Variability, Mehmet E. Soylu
School of Natural Resources: Dissertations, Theses, and Student Research
Evapotranspiration (ET) is an important component of the water and energy balance, yet it is also one of the most challenging components to estimate. There has been great effort to understand the nature of controlling mechanisms and interactions between ET and other earth system processes. The controlling factors of ET can be grouped into two broad categories – namely moisture availability and energy availability (e.g., solar radiation). Soil moisture is a key factor that most of the land surface hydrologic processes are dependent on. While plant water use is mainly controlled by radiation, temperature is another key factor for ET …
Numerical Validation Of A Diurnal Streamflow-Pattern-Based Evapotranspiration Estimation Method, Zoltan Gribovszki, Peter Kalicz, Jozsef Szilagyi
Numerical Validation Of A Diurnal Streamflow-Pattern-Based Evapotranspiration Estimation Method, Zoltan Gribovszki, Peter Kalicz, Jozsef Szilagyi
School of Natural Resources: Faculty Publications
No abstract provided.
Landscape Structure, Groundwater Dynamics, And Soil Water Content Influence Soil Respiration Across Riparian–Hillslope Transitions In The Tenderfoot Creek Experimental Forest, Montana, Vincent J. Pacific, Diego Andrés Riveros-Iregui, Daniel L. Welsch, Howard E. Epstein
Landscape Structure, Groundwater Dynamics, And Soil Water Content Influence Soil Respiration Across Riparian–Hillslope Transitions In The Tenderfoot Creek Experimental Forest, Montana, Vincent J. Pacific, Diego Andrés Riveros-Iregui, Daniel L. Welsch, Howard E. Epstein
School of Natural Resources: Faculty Publications
Variability in soil respiration at various spatial and temporal scales has been the focus of much research over the last decade aimed to improve our understanding and parameterization of physical and environmental controls on this flux. However, few studies have assessed the control of landscape position and groundwater table dynamics on the spatiotemporal variability of soil respiration. We investigated growing season soil respiration in a ~393 ha subalpine watershed in Montana across eight riparian–hillslope transitions that differed in slope, upslope accumulated area (UAA), aspect, and groundwater table dynamics. We collected daily-to-weekly measurements of soil water content (SWC), soil temperature, soil …
Comment On ‘‘An Unconfined Groundwater Model Of The Death Valley Regional Flow System And A Comparison To Its Confined Predecessor’’ By R.W.H. Carroll, G.M. Pohll And R.L. Hershey [Journal Of Hydrology 373/3–4, Pp. 316–328], Claudia C. Faunt, Alden M. Provost, Mary C. Hill, Wayne R. Belcher
Comment On ‘‘An Unconfined Groundwater Model Of The Death Valley Regional Flow System And A Comparison To Its Confined Predecessor’’ By R.W.H. Carroll, G.M. Pohll And R.L. Hershey [Journal Of Hydrology 373/3–4, Pp. 316–328], Claudia C. Faunt, Alden M. Provost, Mary C. Hill, Wayne R. Belcher
United States Geological Survey: Staff Publications
Carroll et al. (2009) state that the United States Geological Survey (USGS) Death Valley Regional Flow System (DVRFS) model, which is based on MODFLOW, is ‘‘conceptually inaccurate in that it models an unconfined aquifer as a confined system and does not simulate unconfined drawdown in transient pumping simulations.’’ Carroll et al. (2009) claim that ‘‘more realistic estimates of water availability’’ can be produced by a SURFACT-based model of the DVRFS that simulates unconfined groundwater flow and limits withdrawals from wells to avoid excessive drawdown. Differences in results from the original MODFLOW- based model and the SURFACT-based model stem primarily from …