C
Clifford I. Voss
Researcher at United States Geological Survey
Publications - 106
Citations - 5730
Clifford I. Voss is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Aquifer & Groundwater flow. The author has an hindex of 38, co-authored 101 publications receiving 4891 citations.
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Variable density flow and solute transport simulation of regional aquifers containing a narrow freshwater‐saltwater transition zone
TL;DR: In this paper, the authors proposed a variable density flow and solute transport simulation of aquifer systems containing narrow transition zones between freshwater and saltwater using Galerkin finite element methodology.
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Aquifer Reclamation Design: The Use of Contaminant Transport Simulation Combined With Nonlinear Programing
Steven M. Gorelick,Clifford I. Voss,Philip E. Gill,Walter Murray,Michael A. Saunders,Margaret H. Wright +5 more
TL;DR: In this article, a simulation-management methodology is demonstrated for the rehabilitation of aquifers that have been subjected to chemical contamination, where finite element groundwater flow and contaminant transport simulation are combined with nonlinear optimization.
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Most atolls will be uninhabitable by the mid-21st century because of sea-level rise exacerbating wave-driven flooding.
Curt D. Storlazzi,Stephen B. Gingerich,Ap van Dongeren,Olivia M. Cheriton,Peter W. Swarzenski,Ellen Quataert,Clifford I. Voss,Donald W. Field,H. Annamalai,Greg Piniak,Robert McCall +10 more
TL;DR: It is shown that, on the basis of current greenhouse gas emission rates, the nonlinear interactions between sea-level rise and wave dynamics over reefs will lead to the annual wave-driven overwash of most atoll islands by the mid-21st century.
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Groundwater flow with energy transport and water-ice phase change: Numerical simulations, benchmarks, and application to freezing in peat bogs
TL;DR: In this article, the U.S. Geological Survey's SUTRA computer code was modified to simulate fully saturated, coupled porewater-energy transport, with freezing and melting pore water, and includes proportional heat capacity and thermal conductivity of water and ice, decreasing matrix permeability due to ice formation and latent heat.