Claire R Tiedeman
Claire Tiedeman is an Emeritus Research Hydrologist in the USGS Water Resources Mission Area, Earth System Processes Division, Water Cycle Branch.
Claire Tiedeman is an Emeritus Research Hydrologist in the USGS Water Resources Mission Area, Earth System Processes Division, Water Cycle Branch. She has used field methods and modeling tools to conduct research on groundwater flow and solute transport in a wide range of complex geologic settings, including basin-scale flow systems and site-scale fractured-rock aquifers. Her research also involves development and application of methods for assessing model uncertainty.
Science and Products
Filter Total Items: 40
Characterizing a ground water basin in a New England mountain and valley terrain
A ground water basin is defined as the volume of subsurface through which ground water flows from the water table to a specified discharge location. Delineating the topographically defined surface water basin and extending it vertically downward does not always define the ground water basin. Instead, a ground water basin is more appropriately delineated by tracking ground water flowpaths with a ca
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Application of nonlinear-regression methods to a ground-water flow model of the Albuquerque Basin, New Mexico
This report documents the application of nonlinear-regression methods
to a numerical model of ground-water flow in the Albuquerque Basin,
New Mexico. In the Albuquerque Basin, ground water is the primary source
for most water uses. Ground-water withdrawal has steadily increased
since the 1940's, resulting in large declines in water levels in the
Albuquerque area. A ground-water flow mode
Authors
C. R. Tiedeman, J. M. Kernodle, D. P. McAda
Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire
This report documents the development of a computer model to simulate steady-state (long-term average) flow of ground water in the vicinity of Mirror Lake, which lies at the eastern end of the Hubbard Brook valley in central New Hampshire. The 10-km2 study area includes Mirror Lake, the three streams that flow into Mirror Lake, Leeman's Brook, Paradise Brook, and parts of Hubbard Brook and the Pem
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Characterization of a high-transmissivity zone by well test analysis: Steady state case
A method is developed to analyze steady horizontal flow to a well pumped from a confined aquifer composed of two homogeneous zones with contrasting transmissivities. Zone 1 is laterally unbounded and encloses zone 2, which is elliptical in shape and is several orders of magnitude more transmissive than zone 1. The solution for head is obtained by the boundary integral equation method. Nonlinear le
Authors
Claire R. Tiedeman, Paul A. Hsieh, Sarah B. Christian
Science and Products
Filter Total Items: 40
Characterizing a ground water basin in a New England mountain and valley terrain
A ground water basin is defined as the volume of subsurface through which ground water flows from the water table to a specified discharge location. Delineating the topographically defined surface water basin and extending it vertically downward does not always define the ground water basin. Instead, a ground water basin is more appropriately delineated by tracking ground water flowpaths with a ca
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Application of nonlinear-regression methods to a ground-water flow model of the Albuquerque Basin, New Mexico
This report documents the application of nonlinear-regression methods
to a numerical model of ground-water flow in the Albuquerque Basin,
New Mexico. In the Albuquerque Basin, ground water is the primary source
for most water uses. Ground-water withdrawal has steadily increased
since the 1940's, resulting in large declines in water levels in the
Albuquerque area. A ground-water flow mode
Authors
C. R. Tiedeman, J. M. Kernodle, D. P. McAda
Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire
This report documents the development of a computer model to simulate steady-state (long-term average) flow of ground water in the vicinity of Mirror Lake, which lies at the eastern end of the Hubbard Brook valley in central New Hampshire. The 10-km2 study area includes Mirror Lake, the three streams that flow into Mirror Lake, Leeman's Brook, Paradise Brook, and parts of Hubbard Brook and the Pem
Authors
Claire R. Tiedeman, Daniel J. Goode, Paul A. Hsieh
Characterization of a high-transmissivity zone by well test analysis: Steady state case
A method is developed to analyze steady horizontal flow to a well pumped from a confined aquifer composed of two homogeneous zones with contrasting transmissivities. Zone 1 is laterally unbounded and encloses zone 2, which is elliptical in shape and is several orders of magnitude more transmissive than zone 1. The solution for head is obtained by the boundary integral equation method. Nonlinear le
Authors
Claire R. Tiedeman, Paul A. Hsieh, Sarah B. Christian