Meryl Storb is hydrologist with the USGS WY-MT Water Science Center.
Meryl is also a PhD candidate in the Payn Watershed Hydrology Lab at Montana State University. She has a B.S. in Environmental Geology from the University of Montana and experience as an environmental consultant. Her past work focused on groundwater studies and Environmental Impact Assessments related to mining, and oil and gas development for a range of clients in the United States, Canada, and West Africa. Meryl's current projects are focused on water quality and building understanding of biogeochemical processes and mechanisms surrounding fate and transport for solutes in both surface water and groundwater.
Professional Experience
2016 – present Hydrologist, U.S. Geological Survey Wyoming-Montana Water Science Center
2014 – present Ph.D. student, Montana Sate University in the Payn Watershed Hydrology Lab
2008-2014 Hydrogeologist/Environmental Consultant, Geomatrix/AMEC/Newfields, Missoula, MT
2005-2008 Research Assistant/Environmental Health Technician, Missoula City County Health Department – Milltown Dam Removal Project, Missoula, MT.
Education and Certifications
Ph.D. Candidate, Ecology and Environmental Science (Watershed Hydrology), Montana State University, 2014- Present. Anticipated Graduation 2024
B.S. in Environmental Geology from the University of Montana, 2008
Science and Products
Growth of coal mining operations in the Elk River Valley linked to increasing transport of selenium, nitrate, and sulfate into Koocanusa Reservoir
Flaxville Aquifer
Input Files and WRTDS Model Output for the two major tributaries of Lake Koocanusa
Growth of coal mining operations in the Elk River Valley (Canada) linked to increasing solute transport of Se, NO3-, and SO42- into the transboundary Koocanusa Reservoir (USA-Canada)
Science and Products
- Science
Growth of coal mining operations in the Elk River Valley linked to increasing transport of selenium, nitrate, and sulfate into Koocanusa Reservoir
The Koocanusa Reservoir (also called Lake Koocanusa) is a transboundary reservoir that's located in northwestern Montana and southwestern British Columbia, Canada (BC) and encompasses the headwaters of the Kootenai watershed, eventually flowing into the Columbia River. Coal mining has occurred in the Elk River watershed in British Columbia, Canada for more than 100 years. Concentrations of...Flaxville Aquifer
The Flaxville aquifer is present in the northern and central parts of the Fort Peck Indian Reservation and consists of sand and gravel that forms extensive plateaus and topographic benches used for dryland farming. Because many residents rely on groundwater as their primary water supply on the Reservation, the Flaxville and underlying aquifers are important sources of groundwater. The goal of this... - Data
Input Files and WRTDS Model Output for the two major tributaries of Lake Koocanusa
Canadian discrete water quality data and daily streamflow records were evaluated using the Weighted Regression on Time, Discharge, and Seasons (WRTDS) model implemented with the EGRET R package (Hirsch et al. 2010, Hirsch and De Cicco 2015). Models were used to estimate loads of solutes and evaluate trends for three constituents of interest (selenium, nitrogen, and sulfate). Six models were genera - Multimedia
- Publications
Growth of coal mining operations in the Elk River Valley (Canada) linked to increasing solute transport of Se, NO3-, and SO42- into the transboundary Koocanusa Reservoir (USA-Canada)
Koocanusa Reservoir (KOC) is a waterbody that spans the United States (U.S.) and Canadian border. Increasing concentrations of total selenium (Se), nitrate + nitrite (NO3–, nitrite is insignificant or not present), and sulfate (SO42–) in KOC and downstream in the Kootenai River (Kootenay River in Canada) are tied to expanding coal mining operations in the Elk River Watershed, Canada. Using a paireAuthorsMeryl Biesiot Storb, Ashley Morgan Bussell, Sara L. Caldwell Eldridge, Robert M. Hirsch, Travis S. Schmidt