Susan Wherry
Susan Wherry is a hydrologist at the USGS Oregon Water Science Center.
Science and Products
Predicting redox conditions in groundwater at a national scale using random forest classification
Examining the effect of physicochemical and meteorological variables on water quality indicators of harmful algal blooms in a shallow hypereutrophic lake using machine learning techniques
Future climate-induced changes in mixing and deep oxygen content of a caldera lake with hydrothermal heat and salt inputs
Modeling flow and water quality in reservoir and river reaches of the Mahoning River Basin, Ohio
Summary of extreme water-quality conditions in Upper Klamath Lake, Oregon, 2005–19
Factors affecting nitrate concentrations in stream base flow
Assessment of Columbia and Willamette River flood stage on the Columbia Corridor Levee System at Portland, Oregon, in a future climate
A metabolism-based whole lake eutrophication model to estimate the magnitude and time scales of the effects of restoration in Upper Klamath Lake, south-central Oregon
Comparison of mercury mass loading in streams to atmospheric deposition in watersheds of Western North America: Evidence for non-atmospheric mercury sources
Simulation of deep ventilation in Crater Lake, Oregon, 1951–2099
The frequency of deep ventilation events in Crater Lake, a caldera lake in the Oregon Cascade Mountains, was simulated in six future climate scenarios, using a 1-dimensional deep ventilation model (1DDV) that was developed to simulate the ventilation of deep water initiated by reverse stratification and subsequent thermobaric instability. The model was calibrated and validated with lake temperatur
Revision and proposed modification for a total maximum daily load model for Upper Klamath Lake, Oregon
Future Climate Effects on Columbia and Willamette River Levees
Input and results from a random forest classification (RFC) model that predicts redox conditions in groundwater in the contiguous United States
Input and results from boosted regression tree and artificial neural network models that predict daily maximum pH and daily minimum dissolved oxygen in Upper Klamath Lake, 2005-2019
1-D Deep Ventilation (1DDV) model for Crater Lake, Oregon, 1950-2100
Water quality measurements in off-channel water bodies of the Willamette River near Albany and Keizer, OR (2017 and 2019)
Hydrodynamic model of the lower Columbia River, Washington and Oregon, 2017-2020
Input and results from a boosted regression tree (BRT) model relating base flow nitrate concentrations in the Chesapeake Bay watershed to catchment characteristics (1970-2013)
Science and Products
Predicting redox conditions in groundwater at a national scale using random forest classification
Examining the effect of physicochemical and meteorological variables on water quality indicators of harmful algal blooms in a shallow hypereutrophic lake using machine learning techniques
Future climate-induced changes in mixing and deep oxygen content of a caldera lake with hydrothermal heat and salt inputs
Modeling flow and water quality in reservoir and river reaches of the Mahoning River Basin, Ohio
Summary of extreme water-quality conditions in Upper Klamath Lake, Oregon, 2005–19
Factors affecting nitrate concentrations in stream base flow
Assessment of Columbia and Willamette River flood stage on the Columbia Corridor Levee System at Portland, Oregon, in a future climate
A metabolism-based whole lake eutrophication model to estimate the magnitude and time scales of the effects of restoration in Upper Klamath Lake, south-central Oregon
Comparison of mercury mass loading in streams to atmospheric deposition in watersheds of Western North America: Evidence for non-atmospheric mercury sources
Simulation of deep ventilation in Crater Lake, Oregon, 1951–2099
The frequency of deep ventilation events in Crater Lake, a caldera lake in the Oregon Cascade Mountains, was simulated in six future climate scenarios, using a 1-dimensional deep ventilation model (1DDV) that was developed to simulate the ventilation of deep water initiated by reverse stratification and subsequent thermobaric instability. The model was calibrated and validated with lake temperatur