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Person

Michael R McHale

Integrated Ecosystem Studies, Lead (Supv Hydrologist)

New York Water Science Center

Email: mmchale@usgs.gov
Office Phone: 518-285-5675
Fax: 518-285-5601
ORCID: 0000-0003-3780-1816

Location
NYWSC - Troy District Office
District Office - Troy
425 Jordan Road
Troy , NY 12180
US

Supervisor: Jennifer L Graham
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The New York Water Science Center of the U.S. Geological Survey (USGS) in Troy, N.Y., operates a state-of-the-science laboratory for the chemical analysis of soil and water. For over 20 years, the laboratory has specialized in analyses used in acid rain research and other environmental studies such as soil effects on forest health and logging effects on water quality. Laboratory Information: Contact the Lab for customized schedules and fees. phone: (518) 285-5681 Water Soils Ammonium ...
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Background Streams and rivers are an important environmental resource and provide water for many human needs. Streamflow is a measure of the volume of water carried by rivers and streams. Changes in streamflow can directly influence the supply of water available for human consumption, irrigation, generating electricity, and other needs. In addition, many plants and animals depend on streamflow for habitat and survival. Streamflow naturally varies over the course of a year. For example, rivers and streams in many parts of the country have their highest (peak) flow when snow melts in the spring. The amount of streamflow is important because high flows can cause erosion and damaging floods, while very low flows...
Click Here for an interactive network map with links to site water quality data The Adirondack Long-Term Lakes Monitoring Lakes (ALTM) project began in 1982 with the objective of tracking changes in the water chemistry of selected Adirondack lakes that are representative of lake types present throughout the Adirondacks. The network began by measuring the water chemistry at 17 lakes in the Adirondack Mountains. In 1992, the project was expanded to include 52 lakes sampled monthly with a goal of assessing the effectiveness of Title IV of the Clean Air Act Amendments of 1990 to reduce acidic deposition through the regulation of sulfur and nitrogen emissions from fossil fuel burning power plants. From 1992 to 2016...
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Problem Sediment transport is a serious concern in the upper Esopus Creek watershed. The creek is a well-documented source of sediment and turbidity to the Ashokan Reservoir, which is part of the New York City water supply system. During the last 2 decades there has been a series of stream stabilization and sediment reduction projects completed in the upper Esopus Creek watershed intended to reduce the suspended sediment load and turbidity levels delivered to the reservoir. During the last 7 years there has been a concerted effort to measure the effect of these projects on turbidity and suspended sediment. There is currently a large, long-term turbidity and suspended sediment study underway within the upper Esopus...
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Introduction The upper Esopus Creek watershed is located in the eastern Catskill Mountains of New York State and covers 497 km2 from Slide Mountain, the highest peak in the Catskills at 1,274 m, to the Ashokan Reservoir at 193 m elevation (fig. 1). Suspended sediment and turbidity are primary water quality concerns in the Ashokan Reservoir watershed, part of the New York City Catskill-Delaware water supply system that supplies more than 10 million people a day with clean drinking water. Stream corridor assessments of tributaries to the Upper Esopus Creek by Ulster County Soil and Water Conservation District, New York City Department of Environmental Protection, and State University of New York at New Paltz summer...
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