Greater complexity in three-dimensional (3D) model structures yields more plausible
groundwater recharge/discharge patterns, especially in groundwater/surface-water …

Across many river basins in the arid Western United States, upstream surface water
reservoirs store snowmelt runoff to meet downstream water demand. A collaborative …

This research highlights development and application of an integrated hydrologic model
(GSFLOW) to a semiarid, snow‐dominated watershed in the Great Basin to evaluate Pinyon …

Water for the Seasons was a five-year collaborative research project which aimed to assess
the climate resiliency of the Truckee-Carson River System, a snow-fed river system in the …

Groundwater and surface water interaction is an essential component of the hydrological
cycle. The hydraulic connectivity and exchange of water between surface water (eg rivers …

High elevation groundwater basins in the western United States are facing changes in the
amount and timing of snowmelt due to climate change. The objective of this study is to …

A new version of MODFLOW, called MODFLOW–USG (for UnStructured Grid), was
developed to support a wide variety of structured and unstructured grid types, including …

Fractures, a generic term for a discontinuity or mechanical break in rock, are ubiquitous in
the upper crust of the Earth and play a major role in processes governing subsurface fluid …

This study develops a modeling framework to better understand surface and groundwater
interactions in the Martis Valley Basin. Prior to the current study there were no physical or …

Greater complexity in three-dimensional (3D) model structures yields more plausible
groundwater recharge/discharge patterns, especially in groundwater/surface-water …