Lake Carmel Harmful Algal Bloom Action Plan
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2014 Aquatic Invasive Species Surveys of New York City Water Supply Reservoirs Within the Catskill/Delaware and Croton Watersheds
2014 aquatic invasive species surveys of New York City water supply reservoirs within the Catskill/Delaware and Croton Watersheds Megan Wilckens1, Holly Waterfield2 and Willard N. Harman3 INTRODUCTION The New York City Department of Environmental Protection (DEP) oversees the management and protection of the New York City water supply reservoirs, which are split between two major watershed systems, referred to as East of Hudson Watersheds (Figure 1) and Catskill/Delaware Watershed (Figure 2). The DEP is concerned about the presence of aquatic invasive species (AIS) in reservoirs because they can threaten water quality and water supply operations (intake pipes and filtration systems), degrade the aquatic ecosystem found there as well as reduce recreational opportunities for the community. Across the United States, AIS cause around $120 billion per year in environmental damages and other losses (Pimentel et al. 2005). The SUNY Oneonta Biological Field Station was contracted by DEP to conduct AIS surveys on five reservoirs; the Ashokan, Rondout, West Branch, New Croton and Kensico reservoirs. Three of these reservoirs, as well as major tributary streams to all five reservoirs, were surveyed for AIS in 2014. This report details the survey results for the Ashokan, Rondout, and West Branch reservoirs, and Esopus Creek, Rondout Creek, West Branch Croton River, East Branch Croton River and Bear Gutter Creek. The intent of each survey was to determine the presence or absence of the twenty- three AIS on the NYC DEP’s AIS priority list (Table 1). This list was created by a subcommittee of the Invasive Species Working Group based on a water supply risk assessment. -
Watershed Agricultural Program 2019 Annual Report and 2020 Workload
Watershed Agricultural Program 2019 Annual Report and 2020 Workload TABLE OF CONTENTS Planning For Increased BMP Implementation Page WAP Managers Report 2 The Watershed Agricultural Program (WAP) commenced a 6 year contract with 2019 Planning Goals 3 the New York City Department of Environmental Protection (DEP), on April 1, 2019 Accomplishments-Funding 3 2019 to accelerate the implementation of BMPs with over $4 million in annual 2019 Accomplishments-BMPs 4 funding. The increase in BMP implementation funds are targeted for the 2019 Planning Goals 22 implementation of BMPs that have been on our backlog list prior to 2017. To 22020 Projected Workload 22 accomplish the increase in workload the WAP has added two assistant Whole 2020 Projected Workload-BMPs 23 Farm Planner positions and has also increased the number of engineering Staff Listing 24 department staff. Program summaries: Conservation Reserve The conservation planners focused on 92 revisions that placed identified Enhancement Program (CREP) 5 resource concerns in the prioritization process, and Whole Farm Plans were Nutrient Management 6 revised accordingly. Precision Feed Management 7-8 Farmer Education 9 In 2019 the WAP implemented 487 BMPs on all active farms at a total cost $4.6 Economic Viability 10 million. These figures include 453 BMPs on West of Hudson farms ($4.2m) and 34 2019 WAP Farm Tour 11 BMPs on East of Hudson farms ($400,000). Projects 12-17 WIRC Team 18 The Precision Feed Management (PFM) Program is a science based program that East of Hudson 19-21 develops feed management plans to deal with the large quantity of feed nutrients managed annually on participant farms. -
Aquatic Microbial Ecology 67:251
Vol. 67: 251–263, 2012 AQUATIC MICROBIAL ECOLOGY Published online November 6 doi: 10.3354/ame01596 Aquat Microb Ecol Rapid regulation of phosphate uptake in freshwater cyanobacterial blooms Luis Aubriot*, Sylvia Bonilla Phytoplankton Ecology and Physiology Group, Sección Limnología, Facultad de Ciencias, Universidad de la República, Iguá 4225, Montevideo 11400, Uruguay ABSTRACT: Cyanobacterial blooms are generally explained by nutrient uptake kinetic constants that may confer competitive capabilities, like high nutrient-uptake rate, affinity, and storage capacity. However, cyanobacteria are capable of flexible physiological responses to environmen- tal nutrient fluctuations through adaptation of their phosphate uptake properties. Growth opti- mization is possible if the physiological reaction time of cyanobacteria (tR) matches the duration of nutrient availability. Here, we investigate the tR of this complex physiological process. We per- formed [32P] uptake experiments with filamentous cyanobacterial blooms. The phytoplankton were subjected to different nutrient exposure times (tE) by varying patterns of phosphate addi- tions. After 15 to 25 min of phosphate tE, the cyanobacteria-dominated phytoplankton began their adaptive response by reducing and finally ceasing uptake activity before exhausting their nutrient uptake capacity. The time of onset of phosphate uptake regulation (in min) is an indicator of tR. Rapid adaptive behaviour may be the initial phase of longer-term nutrient acclimation (hours to days), which results in a higher growth rate. The growth response of bloom-forming cyanobacteria may be more dependent on the ability to optimize the uptake of phosphate during the time span of nutrient fluctuation than on the amount of nutrient taken up per se. Freshwater cyanobacterial blooms may therefore be promoted by their short tR during phosphate fluctuations. -
Harmful Algal Bloom Action Plan Lake George
HARMFUL ALGAL BLOOM ACTION PLAN LAKE GEORGE www.dec.ny.gov EXECUTIVE SUMMARY SAFEGUARDING NEW YORK’S WATER Protecting water quality is essential to healthy, vibrant communities, clean drinking water, and an array of recreational uses that benefit our local and regional economies. 200 NY Waterbodies with HABs Governor Cuomo recognizes that investments in water quality 175 protection are critical to the future of our communities and the state. 150 Under his direction, New York has launched an aggressive effort to protect state waters, including the landmark $2.5 billion Clean 125 Water Infrastructure Act of 2017, and a first-of-its-kind, comprehensive 100 initiative to reduce the frequency of harmful algal blooms (HABs). 75 New York recognizes the threat HABs pose to our drinking water, 50 outdoor recreation, fish and animals, and human health. In 2017, more 25 than 100 beaches were closed for at least part of the summer due to 0 HABs, and some lakes that serve as the primary drinking water source for their communities were threatened by HABs for the first time. 2012 2013 2014 2015 2016 2017 GOVERNOR CUOMO’S FOUR-POINT HARMFUL ALGAL BLOOM INITIATIVE In his 2018 State of the State address, Governor Cuomo announced FOUR-POINT INITIATIVE a $65 million, four-point initiative to aggressively combat HABs in Upstate New York, with the goal to identify contributing factors fueling PRIORITY LAKE IDENTIFICATION Identify 12 priority waterbodies that HABs, and implement innovative strategies to address their causes 1 represent a wide range of conditions and protect water quality. and vulnerabilities—the lessons learned will be applied to other impacted Under this initiative, the Governor’s Water Quality Rapid Response waterbodies in the future. -
Multi-Gear, Multi-Site Fish Survey in New
SUBMERSED AQUATIC VEGETATION IN A HUDSON RIVER WATERSHED: THE GREAT SWAMP OF NEW YORK A Final Report of the Tibor T. Polgar Fellowship Program Chris Cotroneo Polgar Fellow Biology Department Queens College 65-30 Kissena Boulevard Flushing, NY 11367 Project Advisor: John Waldman, Ph.D. Biology Department Queens College 65-30 Kissena Boulevard Flushing, NY 11367 Cotroneo, C., and J. Waldman. 2019. Submersed Aquatic Vegetation in a Hudson River Watershed: The Great Swamp of New York. Section III: 1-44 pp. In S.H. Fernald, D.J. Yozzo and H. Andreyko (eds.), Final Reports of the Tibor T. Polgar Fellowship Program, 2016. Hudson River Foundation. III-1 ABSTRACT Baseline information about submersed aquatic vegetation (SAV) communities and their associated fish assemblages represents a valuable information resource for use by the scientific community for comparison to other studies, documenting changes over time, and to assist with actions such as fish passage. In order to collect data throughout the entire growing season, a comprehensive six-month, submersed aquatic vegetation (SAV) study was conducted in New York’s Great Swamp. Sampling sites were selected based upon the presence of SAV representative of the surrounding area and were sampled bi- weekly. Aerial percent cover was estimated for each SAV species identified within the sampling site. A total of 12 SAV stands were sampled throughout the course of the study. A total of 58 SAV samples were taken, revealing five dominant SAV species: Potamogeton crispus, P. pusillus, P. illinoensis, Ceratophyllum demersum, and Elodea canadensis. Every fourth week the same sites were sampled for nekton to determine if habitat use changed with any changes in dominant SAV species. -
Nutrient Loads from the Catchment
Chapter 7 Assessing and controlling the risk of cyanobacterial blooms Nutrient loads from the catchment Ingrid Chorus and Matthias Zessner CONTENTS Introduction and general considerations 434 7.1 Determining targets for nutrient concentrations in the waterbody 437 7.2 Determining critical nutrient loads to the waterbody 440 7.3 Identifying key nutrient sources and pathways causing loads 443 7.3.1 Background information 443 7.3.2 Identifying nutrient sources and pathways 446 7.3.3 Nutrient loads from wastewater, stormwater and commercial wastewater 451 7.3.3.1 Sources 452 7.3.3.2 Pathways 453 7.3.3.3 What to look for when compiling an inventory of loads from sewage, stormwater and commercial wastewater sources 454 7.3.4 Nutrient loads from agriculture and other fertilised areas 456 7.3.4.1 Sources 456 7.3.4.2 Pathways 457 7.3.4.3 What to look for when compiling an inventory of loads from agricultural activities 459 7.3.5 Nutrient loads from aquaculture and fisheries 463 7.3.5.1 What to look for when including aquaculture and fisheries in the inventory of activities causing nutrient loads 463 7.4 Approaches to quantifying the relevance of sources and pathways 465 7.4.1 Tier 1: Assessment using emission factors 468 7.4.1.1 Municipalities 468 7.4.1.2 Agriculture 470 7.4.2 Tier 2: Assessment using the Riverine Load Approach 472 7.4.2.1 Flow normalisation to avoid misinterpretation of causalities 474 7.4.2.2 Estimation of diffuse loads 474 7.4.3 Tier 3: Pathway-Oriented Approach 476 433 434 Toxic Cyanobacteria in Water 7.4.4 Tier 4: The Source-Oriented -
Infrastructure and Tectonics of the Hudson Highlands, New York Nicholas M
NYSGA 2009 Trip 9 - Ratcliffe and Aleinikoff Trip 9 - Ratcliffe and Aleinikoff Pre-Ottawan (1.09 Ga) Infrastructure and Tectonics of the Hudson Highlands, New York Nicholas M. Ratcliffe1 and John N. Aleinikoff2 1U.S. Geological Survey, Reston VA 20192, [email protected] 2U.S. Geological Survey, Denver, CO 80225, [email protected] INTRODUCTION This trip focuses on some of the oldest Mesoproterozic rocks in the Appalachians and the nature of the pre-Ottawan (pre-1.09 Ga) infrastructure of the Hudson Highlands and Manhattan Prong. Zircon geochronology by Aleinikoff (Table 1) is revised from that given in Table 1 of Ratcliffe and Aleinikoff (2008) and is still preliminary. Ongoing geologic mapping east of the Hudson River in the Peekskill, West Point, Lake Carmel, Mohegan Lake, Brewster and Peach Lake quadrangles continues to lead to a reinterpretation and clarification of our former views (Ratcliffe and Aleinikoff, 2001, 2008) as well a new synthesis for the Hudson Highlands east of the Hudson River. After publish- ing the detailed geology of the Poughquag quadrangle (Ratcliffe and Burton, 1990) and the Oscawana Lake quad- rangle (Ratcliffe, 1992), investigations were resumed in 2000 to prepare the previously mapped but unpublished quadrangles for publication. This trip presents, in preliminary form, much of the recent, (post-2000) information, which helps clarify the age and distribution of Mesoproterozoic basement rocks of the Hudson Highlands and Manhattan Prong and is an abbrevi- ated version of our 2008 NEIGC trip. Please note that stops have been changed and that the route is different. A remarkable newly recognized aspect of Hudson Highlands geology covered in this trip is the widespread presence of orthogneisses and metavolcanic rocks belonging to the time period between 1400 Ma and 1200 Ma, or during Geochrons 14 and 13 of Rivers (1997). -
Longevity and Effectiveness of Aluminum Addition to Reduce Sediment Phosphorus Release and Restore Lake Water Quality
Water Research 97 (2016) 122e132 Contents lists available at ScienceDirect Water Research journal homepage: www.elsevier.com/locate/watres Longevity and effectiveness of aluminum addition to reduce sediment phosphorus release and restore lake water quality * Brian J. Huser a, , Sara Egemose b, Harvey Harper c, Michael Hupfer d, Henning Jensen b, Keith M. Pilgrim e, Kasper Reitzel b, Emil Rydin f, Martyn Futter a a Swedish University of Agricultural Sciences, Department of Aquatic Sciences and Assessment, Box 7050, 75007, Uppsala, Sweden b University of Southern Denmark, Department of Biology, Campusvej 55, DK-5230, Odense M, Denmark c ERD Environmental Research & Design, 3419 Trentwood Blvd., Suite 102, Orlando, FL, USA d Leibniz Institute of Freshwater Ecology and Inland Fisheries, Berlin, Germany e Barr Engineering, 4077 77th Street, Minneapolis, MN, 55304, USA f Erken Laboratory, Dep. of Ecology and Genetics, Uppsala University, Norra Malmavagen€ 45, SE 761 73, Norrtalje,€ Sweden article info abstract Article history: 114 lakes treated with aluminum (Al) salts to reduce internal phosphorus (P) loading were analyzed to Received 3 May 2015 identify factors driving longevity of post-treatment water quality improvements. Lakes varied greatly in Received in revised form morphology, applied Al dose, and other factors that may have affected overall treatment effectiveness. 25 June 2015 Treatment longevity based on declines in epilimnetic total P (TP) concentration averaged 11 years for all Accepted 30 June 2015 lakes (range of 0e45 years). When longevity estimates were used for lakes with improved conditions Available online 8 July 2015 through the end of measurements, average longevity increased to 15 years. Significant differences in treatment longevity between deeper, stratified lakes (mean 21 years) and shallow, polymictic lakes Keywords: Aluminum (mean 5.7 years) were detected, indicating factors related to lake morphology are important for treat- Water management ment success. -
Total Maximum Daily Load (TMDL) for Phosphorus in Lake Carmel Final
Total Maximum Daily Load (TMDL) for Phosphorus in Lake Carmel Putnam County, New York July 2016 Prepared for: U.S. Environmental Protection Agency Region 2 290 Broadway New York, NY 10007 Prepared by: NYSDEC Division of Water Bureau of Water Resource Management TABLE OF CONTENTS 1.0 INTRODUCTION ...........................................................................................................................4 1.1. Background .....................................................................................................................................4 1.2. Problem Statement ........................................................................................................................4 2.0 WATERSHED AND LAKE CHARACTERIZATION ......................................................................5 2.1. Watershed Characterization .........................................................................................................5 2.2. Lake Morphometry ...................................................................................................................... 10 2.3. Water Quality .............................................................................................................................. 11 3.0 NUMERIC WATER QUALITY TARGET ..................................................................................... 12 4.0 SOURCE ASSESSMENT .............................................................................................................. 12 4.1. Models used to Analyze Phosphorus Contributions -
Lake Carmel TMDL EPA Approval Letter (PDF)
UNITED STATES ENVIRONMENTAL PROTECTION AGENCY REGION 2 290 BROADWAY NEW YORK, NY 10007-1866 SEP 2 0 2016 Mr. Mark Klotz, Director Division of Water, 4th Floor New York State Department of Environmental Conservation 625 Broadway Albany, New York 12233-3500 Dear Mr. Klotz: On September 2, 2016, the U.S. Environmental Protection Agency, Region 2, received for review and approval, the New York State Department of Environmental Conservation's document, dated July 2016: "Total Maximum Daily Load (TMDL) for Phosphorus in Lake Carmel, Putnam County, New York." The EPA approves this TMDL pursuant to Section 303(d)(2) of the Clean Water Act (CWA) and the EPA's implementing regulations at 40 CFR 130.7(d)(2). The rationale for this approval is provided in the enclosure entitled "Review of Total Maximum Daily Load (TMDL) for Total Phosphorus for Lake Carmel, New York." The TMDL addresses the total phosphorus loading and impairment in this waterbody and is established at a level sufficient to attain the NYSDEC's water quality guidance value for total phosphorus for Lake Carmel. The EPA expects this approved TMDL will be incorporated in the New York State Water Quality Management Plan. Sincerely, Q~ C, ~< ~!avier Laureano, Director Clean Water Division Enclosure Internet Address (URL) • http://www.epa.gov Recycled/Recyclable • Printed with Vegetable Oil Based Inks on Recycled Paper (Minimum 50% Postconsumer content) Review of Total Maximum D~ily Load (TMDL) for Total Phosphorus for Lake Carmel, New York This document contains EPA's review of the above-referenced TMDL. This TMDL review document includes TMDL review guidelines that summarize and provide guidance regarding currently effective statutory and regulatory requirements relating to TMDLs. -
Ulster Orange Greene Dutchess Albany Columbia Schoharie
Barriers to Migratory Fish in the Hudson River Estuary Watershed, New York State Minden Glen Hoosick Florida Canajoharie Glenville Halfmoon Pittstown S a r a t o g a Schaghticoke Clifton Park Root Charleston S c h e n e c t a d y Rotterdam Frost Pond Dam Waterford Schenectady Zeno Farm Pond Dam Niskayuna Cherry Valley M o n t g o m e r y Duanesburg Reservoir Dam Princetown Fessenden Pond Dam Long Pond Dam Shaver Pond Dam Mill Pond Dam Petersburgh Duanesburg Hudson Wildlife Marsh DamSecond Pond Dam Cohoes Lake Elizabeth Dam Sharon Quacken Kill Reservoir DamUnnamed Lent Wildlife Pond Dam Delanson Reservoir Dam Masick Dam Grafton Lee Wildlife Marsh Dam Brunswick Martin Dunham Reservoir Dam Collins Pond Dam Troy Lock & Dam #1 Duane Lake Dam Green Island Cranberry Pond Dam Carlisle Esperance Watervliet Middle DamWatervliet Upper Dam Colonie Watervliet Lower Dam Forest Lake Dam Troy Morris Bardack Dam Wager Dam Schuyler Meadows Club Dam Lake Ridge Dam Beresford Pond Dam Watervliet rapids Ida Lake Dam 8-A Dyken Pond Dam Schuyler Meadows Dam Mt Ida Falls Dam Altamont Metal Dam Roseboom Watervliet Reservoir Dam Smarts Pond Dam dam Camp Fire Girls DamUnnamed dam Albia Dam Guilderland Glass Pond Dam spillway Wynants Kill Walter Kersch Dam Seward Rensselaer Lake Dam Harris Dam Albia Ice Pond Dam Altamont Main Reservoir Dam West Albany Storm Retention Dam & Dike 7-E 7-F Altamont Reservoir Dam I-90 Dam Sage Estates Dam Poestenkill Knox Waldens Pond DamBecker Lake Dam Pollard Pond Dam Loudonville Reservoir Dam John Finn Pond Dam Cobleskill Albany Country Club Pond Dam O t s e g o Schoharie Tivoli Lake Dam 7-A . -
Work on Watersheds Report Highlights Stories Coordinate Groups
Work on Watersheds Hu ds on R i v e r UTICA SARATOGA SPRINGS Mo haw k River SCHENECTADY TROY ALBANY y r a u t s E r e v i R n o s d u H KINGSTON POUGHKEEPSIE NEWBURGH Hudson River MIDDLETOWN Watershed Regions PEEKSKILL Upper Hudson River Watershed Mohawk River Watershed YONKERS Hudson River Estuary Watershed NEW YORK Work on Watersheds INTRODUCTION | THE HUDSON RIVER WATERSHED ALLIANCE unites and empowers communities to protect their local water resources. We work throughout the Hudson River watershed to support community-based watershed groups, help municipalities work together on water issues, and serve as a collective voice across the region. We are a collaborative network of community groups, organizations, municipalities, agencies, and individuals. The Hudson River Watershed Alliance hosts educational and capacity-building events, including the Annual Watershed Conference to share key information and promote networking, Watershed Roundtables to bring groups together to share strategies, workshops to provide trainings, and a breakfast lecture series that focuses on technical and scientific innovations. We provide technical and strategic assistance on watershed work, including fostering new initiatives and helping sustain groups as they meet new challenges. What is a watershed group? A watershed is the area of land from which water drains into a river, stream, or other waterbody. Water flows off the land into a waterbody by way of rivers and streams, and underground through groundwater aquifers. The smaller streams that contribute to larger rivers are called tributaries. Watersheds are defined by the lay of the land, with mountains and hills typically forming their borders.