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New York Water Science Center

The New York Water Science Center will provide the hydrologic observations, research, and modeling needed for full integration of hydrogeologic, physiochemical, biological, and landscape processes across the freshwater to marine continuum. 

News

USGS Satellites and Test Tubes Meet to Ensure Safe Drinking Water

USGS Satellites and Test Tubes Meet to Ensure Safe Drinking Water

Advanced Quantitative Precipitation Information System Enhances Flood Prediction in San Francisco Bay Area

Advanced Quantitative Precipitation Information System Enhances Flood Prediction in San Francisco Bay Area

Native American Research Assistantship Student Learns USGS Water Science

Native American Research Assistantship Student Learns USGS Water Science

Publications

Analysis of aquifer framework and properties, Alvahs Lane well field, Cutchogue, New York

The U.S. Geological Survey, in cooperation with the Suffolk County Water Authority, evaluated the aquifer transmissivity and storage properties at the Alvahs Lane well field north of the village of Cutchogue, New York. This analysis of aquifer properties provides the Suffolk County Water Authority with hydrogeologic information needed to develop water supplies to meet the increasing...
Authors
Paul E. Misut

Evaluating drought risk of the Red River of the North Basin using historical and stochastic streamflow upstream from Emerson, Manitoba

Drought and its effect on streamflow are important to understand because of the potential to adversely affect water supply, agricultural production, and ecological conditions. The Red River of the North Basin in north-central United States and central Canada is susceptible to dry conditions. During an extended drought, streamflow conditions in the Red River of the North may become...
Authors
Fleford S. Redoloza, Robin L. Glas, Rochelle A. Nustad, Karen R. Ryberg

Characterization of stream water quality and groundwater levels in the Central Pine Barrens region, Suffolk County, New York, 2017–23

The area locally known as the “Central Pine Barrens” region, located in Suffolk County, New York, contains most of Long Island’s preserved and undeveloped land. This region overlays an aquifer system that provides potable groundwater for residents of Suffolk County. Between 2017 and 2023, the U.S. Geological Survey, in cooperation with the Central Pine Barrens Joint Planning & Policy...
Authors
Amanda M. Dondero, Irene J. Fisher, Amy E. Simonson, Banu N. Bayraktar

Science

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A National Predictive Model for PFAS Occurrence in Groundwater

In October of 2024, USGS Scientist’s published a study where they created a model to predict PFAS occurrence in groundwater at the depths of drinking water supplies. This model can help guide our partners to sample areas where PFAS in drinking water could be an issue for the public.
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Groundwater Flow Modeling - Long Island, New York

Numerical models provide a means to synthesize existing hydrogeologic information into an internally consistent mathematical representation of a real system or process, and thus are useful tools for testing and improving conceptual models or hypotheses of groundwater flow systems. The goal of this effort is to develop a regional model for the Long Island aquifer system to simulate changes in water...
link

Groundwater Flow Modeling - Long Island, New York

Numerical models provide a means to synthesize existing hydrogeologic information into an internally consistent mathematical representation of a real system or process, and thus are useful tools for testing and improving conceptual models or hypotheses of groundwater flow systems. The goal of this effort is to develop a regional model for the Long Island aquifer system to simulate changes in water...
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Saltwater-Interface Mapping - Long Island, New York

Saltwater intrusion is the most common type of water-quality degradation in coastal-plain aquifers. In coastal areas, the hydraulic head under predevelopment (nonpumping) conditions is higher on land than in the surrounding saltwater embayments; thus, fresh groundwater flows seaward (from areas of high potential to areas of lower potential) and meets saltwater at an equilibrium point (interface)...
link

Saltwater-Interface Mapping - Long Island, New York

Saltwater intrusion is the most common type of water-quality degradation in coastal-plain aquifers. In coastal areas, the hydraulic head under predevelopment (nonpumping) conditions is higher on land than in the surrounding saltwater embayments; thus, fresh groundwater flows seaward (from areas of high potential to areas of lower potential) and meets saltwater at an equilibrium point (interface)...
Learn More
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