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Macroinvertebrate Distribution in Relation to Land Use and Water Chemistry in New York City Drinking-Water-Supply Watersheds
J. N. Am. Benthol. Soc., 2006, 25(4):954–976 Ó 2006 by The North American Benthological Society Macroinvertebrate distribution in relation to land use and water chemistry in New York City drinking-water-supply watersheds Erika B. Kratzer1, John K. Jackson2, David B. Arscott3, Anthony K. Aufdenkampe4, Charles L. Dow5, L. A. Kaplan6, 7 6 J. D. Newbold , AND Bernard W. Sweeney Stroud Water Research Center, 970 Spencer Road, Avondale, Pennsylvania 19311 USA Abstract. Macroinvertebrate communities were examined in conjunction with landuse and water- chemistry variables at 60 sites in the NYC drinking-water-supply watersheds over a 3-y period. The watersheds are in 2 adjacent regions of New York State (east of Hudson River [EOH] and west of Hudson River [WOH]) that are geographically distinct and have unique macroinvertebrate communities. Nonforested land use at EOH sites was mostly urban (4–57%), whereas land use at sites in the rural WOH region was more agricultural (up to 26%) and forested (60–97%). Land use accounted for 47% of among-site variability in macroinvertebrate communities in the EOH region and was largely independent of geological effects. Land use accounted for 40% of among-site variability in macroinvertebrate communities in the WOH region but was correlated with underlying geology. Comparisons among 3 landuse scales emphasized the importance of watershed- and riparian-scale land use to macroinvertebrate communities in both regions. Multivariate and bivariate taxa–environment relationships in the EOH and WOH regions identified specific landuse and water-chemistry gradients and, in general, showed a continuum in conditions across the watersheds. -
This Article Was Originally Published in a Journal Published by Elsevier
This article was originally published in a journal published by Elsevier, and the attached copy is provided by Elsevier for the author’s benefit and for the benefit of the author’s institution, for non-commercial research and educational use including without limitation use in instruction at your institution, sending it to specific colleagues that you know, and providing a copy to your institution’s administrator. All other uses, reproduction and distribution, including without limitation commercial reprints, selling or licensing copies or access, or posting on open internet sites, your personal or institution’s website or repository, are prohibited. For exceptions, permission may be sought for such use through Elsevier’s permissions site at: http://www.elsevier.com/locate/permissionusematerial Estuarine, Coastal and Shelf Science 71 (2007) 259e277 www.elsevier.com/locate/ecss Regional patterns and local variations of sediment distribution in the Hudson River Estuary F.O. Nitsche a,*, W.B.F. Ryan a, S.M. Carbotte a, R.E. Bell a, A. Slagle a, C. Bertinado a, R. Flood c, T. Kenna a, C. McHugh a,b a Lamont-Doherty Earth Observatory of Columbia Univeristy, Palisades, NY 10964, USA b Queens College, City University New York, Flushing, NY, USA c Stony Brook University, Stony Brook, USA Received 3 November 2005; accepted 27 July 2006 Available online 2 October 2006 Abstract The Hudson River Benthic Mapping Project, funded by the New York State Department of Environmental Conservation, resulted in a com- prehensive data set consisting of high-resolution multibeam bathymetry, sidescan sonar, and sub-bottom data, as well as over 400 sediment cores and 600 grab samples. -
Croton-To-Highlands Biodiversity Plan
$8.00 Croton-to-Highlands Biodiversity Plan Balancing Development and the Environment in the Hudson River Estuary Catchment Metropolitan Conservation Alliance a program of MCA Technical Paper Series: No. 7 Croton-to-Highlands Biodiversity Plan Balancing Development and the Environment in the Hudson River Estuary Catchment by Nicholas A. Miller, M.S. and Michael W. Klemens, Ph.D. Metropolitan Conservation Alliance Wildlife Conservation Society Bronx, NY Cover photograph: Hunter Brook, Yorktown, NY. ©WCS/MCA, Kevin J. Ryan Suggested citation: Miller, N. A. and M. W. Klemens. 2004. Croton-to-Highlands Biodiversity Plan: Balancing development and the environment in the Hudson River Estuary Catchment. MCA Technical Paper No. 7, Metropolitan Conservation Alliance, Wildlife Conservation Society, Bronx, New York. Additional copies of this document can be obtained from: Metropolitan Conservation Alliance Wildlife Conservation Society 68 Purchase Street, 3rd Floor Rye, New York 10580 (914) 925-9175 [email protected] ISBN 0-9724810-2-8 ISSN 1542-8133 Printed on partially recycled paper ACKNOWLEDGEMENTS This project would not have been possible without the enthusiastic collaboration and support of our key partners: the towns of Cortlandt, New Castle, Putnam Valley, and Yorktown. These communities have helped to guide this project and have contributed to its success through active engagement at meetings and planning charettes, on-going outreach to their citizenry, and contribution of seed monies. We extend thanks to all of our partners within these four communities (including many elected and appointed officials, town staff, volunteer board members, and concerned citizens) who have moved this project forward and who continue to make conservation of biodiversity a priority within their towns. -
Volume 26 , Number 2
The hudson RIVeR Valley ReVIew A Journal of Regional Studies HRVR26_2.indd 1 5/4/10 10:45 AM Publisher Thomas s. wermuth, Vice President for academic affairs, Marist College Editors Christopher Pryslopski, Program director, hudson River Valley Institute, Marist College Reed sparling, writer, scenic hudson Editorial Board Art Director Myra young armstead, Professor of history, Richard deon Bard College Business Manager Col. lance Betros, Professor and head, andrew Villani department of history, u.s. Military academy at west Point The Hudson River Valley Review (Issn 1546-3486) is published twice Kim Bridgford, Professor of english, a year by the hudson River Valley Fairfield university Institute at Marist College. Michael Groth, Professor of history, wells College James M. Johnson, Executive Director susan Ingalls lewis, assistant Professor of history, state university of new york at new Paltz Research Assistants sarah olson, superintendent, Roosevelt- Gail Goldsmith Vanderbilt national historic sites elizabeth Vickind Roger Panetta, Professor of history, Hudson River Valley Institute Fordham university Advisory Board h. daniel Peck, Professor of english, Todd Brinckerhoff, Chair Vassar College Peter Bienstock, Vice Chair Robyn l. Rosen, Professor of history, dr. Frank Bumpus Marist College Frank J. doherty david schuyler, Professor of american studies, shirley handel Franklin & Marshall College Marjorie hart Maureen Kangas Thomas s. wermuth, Vice President of academic Barnabas Mchenry affairs, Marist College, Chair alex Reese david woolner, -
New York City, the Lower Hudson River, and Jamaica Bay
3.4 New York City, the Lower Hudson River, and Jamaica Bay Author: Elizabeth M. Strange, Stratus Consulting Inc. Species and habitats in the region encompassing such as beach nourishment, dune construction, New York City, the lower Hudson River, the and vegetation wherever possible. Planners East River, and Jamaica Bay are potentially at expect that the only sizeable areas in the New risk because of sea level rise. Although the York City metropolitan area that are unlikely to region is one of the most heavily urbanized areas be protected are portions of the three Special along the U.S. Atlantic Coast, there are Natural Waterfront Areas (SNWAs) designated nonetheless regionally significant habitats for by the city: Northwest Staten Island/Harbor fish, shellfish, and birds in the area, and a great Heron SNWA; East River–Long Island Sound deal is known about the ecology and habitat SNWA; and Jamaica Bay SNWA. needs of these species. TIDAL WETLANDS Based on existing literature and the knowledge of local scientists, this brief literature review Staten Island. Hoffman Island and Swinburne discusses those species that could be at risk Island are National Park Service properties lying because of further habitat loss resulting from sea off the southeast shore of Staten Island; the level rise and shoreline protection (see Map 3.2). former has important nest habitat for herons, and 252 Although it is possible to make qualitative the latter is heavily nested by cormorants. The statements about the ecological implications if Northwest Staten Island/Harbor Herons SNWA sea level rise causes a total loss of habitat, our is an important nesting and foraging area for 253 ability to say what the impact might be if only a herons, ibises, egrets, gulls, and waterfowl. -
How New York City Used an Ecosystem Services Strategy
How New York City Used an Ecosystem Services Strategy Carried out Through an Urban-Rural Partnership to Preserve the Pristine Quality of Its Drinking Water and Save Billions of Dollars and What Lessons It Teaches about Using Ecosystem Services by Albert F. Appleton November 2002 New York City This paper was previously presented at The Katoomba Conference / Tokyo, November 2002 Introduction The New York City Water system serves nine million people, eight million in New York City and one million in the suburbs north of the City. It provides these customers with 1.2 billion gallons of water a day, delivered to 600, 000 residential and 200,000 commercial building in the City, and close to two dozen local water systems in New York’s northern suburbs. New York City is a surface water system that gathers its water from three watersheds located well north of the City. These watersheds cover an area of 2,000 square miles (830,000 hectares), nearly the size of the state of Delaware. The City's Croton River watershed, which was created in the 1830s and expanded in the 1880s, is located 15 to 25 miles (25 to 40 kilometers) north of the City and east of the Hudson River in Westchester and Putnam counties. This area was originally rural, but since World War II it has become (or is now becoming) largely suburban. The Croton supplies 10% of the City's water supply. The City's main watershed is now the Catskill-Delaware watershed system west of the Hudson River. It encompasses most of the Catskill Mountains, a rural area of farms, forests, small towns and a growing number of vacation home developments. -
Relating Major Ions and Nutrients to Watershed Conditions Across a Mixed-Use, Water-Supply Watershed
J. N. Am. Benthol. Soc., 2006, 25(4):887–911 Ó 2006 by The North American Benthological Society Relating major ions and nutrients to watershed conditions across a mixed-use, water-supply watershed 1 2 3 Charles L. Dow , David B. Arscott , AND J. Denis Newbold Stroud Water Research Center, 970 Spencer Road, Avondale, Pennsylvania 19311 USA Abstract. Stream inorganic chemistry was sampled under summer baseflow conditions from 2000 to 2002 at 60 sites as part of a large-scale, enhanced water-quality monitoring project (the Project) across New York City’s drinking-water-supply watersheds. The 60 stream sites were evenly divided between regions east and west of the Hudson River (EOH and WOH, respectively). EOH sites had generally higher ionic concentrations than WOH sites, reflecting differences in land use and geology. Within each region, variability in inorganic chemistry data between sites was far greater than annual variability within sites. Geology was an important factor controlling underlying baseflow chemistry differences within and between regions. However, after taking into account geological controls, anthropogenic land uses primarily defined ion and nutrient baseflow chemistry patterns at regional and watershed levels. In general, watershed-scale landscape attributes had either the strongest relationships with analytes or had relationships with analytes that did not differ fundamentally from relationships of riparian- or reach- scale landscape attributes. Individual analyses indicated no dominant watershed-scale landscape attribute that could be used to predict instream inorganic chemistry concentrations, and no single ion or nutrient was identified as the best indicator of a given anthropogenic land use. Our results provide a comprehensive baseline of information for future water-quality assessments in the region and will aid in examining other components of the Project. -
Report on Coastal Vulnerability and Sea Level Rise
Report on Coastal Vulnerability and Sea Level Rise December 8, 2014 Photo of Beach Road after Hurricane Sandy of 2012. Photo by: L. Konopko Report on Coastal Vulnerability and Sea Level Rise ThisThis Report was developed in consultation of the Town of Stony Point NYRCR Planning Committee Gurran Kane, Co-Chair Steven Scurti, Co-Chair Steve Beckerle Robert Burns Rebecca Casscles Wellington Casscles Supervisor Geoff Finn Luanne Konopko Kevin Maher Jim McDonnell Steve Porath Dominick Posillipo Rick Struck in cooperation with and with funding assistance byby:::: The New York Department of Environmental Conservation - Hudson River Estuary Program The New England Interstate Water Pollution Control Commission This information was prepared for the Hudson River Estuary program, New York State Department of Environmental Conservation, with support from the New York State Environmental Protection Fund, in cooperation with the New England Interstate Water Pollution Control Commission. The viewpoints expressed here do not necessarily represent those of NEIWPCC or NYSDEC, nor does mention of trade names, commercial products, or causes constitute endorsement or recommendation for use. 2 December 8, 2014 Report on Coastal Vulnerability and Sea Level Rise Table of Contents Introduction ............................................................................................................................................................................ 1 Purpose .................................................................................................................................................................................. -
The History Of
The History of 1 INDEX Introduction........................................................................................Page 3 The Hudson River & the Highlands……………………………………………….….…..Page 14 The Van Cortlandts – 1698 to 1853……………………………………………….….….Page 18 Louisa Sophia Ludlow – 1853 to 1876……………………………………………........Page 57 Louis W.Stevenson – 1876 to 1887………………………………………………..….….Page 91 Emma E. Stevenson – 1887 to 1899…………………………………………………....Page 142 Henry Jackson Morton Jr. – 1899 to 1901……………………………………………....Page 154 Ernest E. Slocum – 1901 to 1903………………………………………………….……Page 166 Greenhalge – 1903 to 1905……………………………………………………………..Page 168 Maud & William Boag – 1905 to 1914…………………………………………………..Page 174 Collin Kemper & Hope Latham – 1914 to 1942…………………………………………...Page 186 The Guiles – 1942 to 1952………………………………………………………….…Page 265 The Matzners – 1952 to 1966………………………………………………….....…..Page 274 The Cummings – 1966 to 1975……………………………………………………..….Page 285 GianninaPradella& Milan Olich – 1975 to 2005……………………………..………….Page 289 Richard Friedberg – 2005 to 2011………………………………………………..……Page 295 Arlene & Brent Perrott – 2011 to Present…………………………………………..…..Page 299 Myths, Legends and Ghosts……………………………………………………….….Page 303 2 INTRODUCTION Oldstone sits above the banks of the Hudson River, its gray, thick stone walls firmly anchored to the soil and rock of the Hudson Highlands. With Peekskill to the south, Bear Mountain Bridge and Westpoint just to the north, it is surrounded by some of the most beautiful and historic sites on the Hudson River. When Oldstone -
Windows on History
EXPLORING THE HUDSON RIVER VALLEY NATIONAL HERITAGE AREA Windows on History A rail journey through the Hudson River Valley, between New York City and Albany, is more than a trip from point A to point B. It’s a voyage through a landscape rich in history and beauty. Just look out the window… Na lley tion Va al r H e e v r i i t R a g n e o A s r d e u a H Na lley tion Va al r H e e v r i i t R a g n e o A s r d e u a H W ELCOME TO THE HUDSON RIVER VALLEY! RAVELING THROUGH THIS HISTORIC REGION, you will discover the people, places, and events that formed our national identity, and led Congress to designate the Hudson River Valley as a National Heritage Area in 1996. The Hudson River has also been designated one of our country’s Great American Rivers. TAs you journey between New York’s Pennsylvania station and the Albany- Rensselaer station, this guide will interpret the sites and features that you see out your train window, including historic sites that span three centuries of our nation’s history. You will also learn about the communities and cultural resources that are located only a short journey from the various This project was made station stops. possible through a partnership between the We invite you to explore the four million acres Hudson River Valley that make up the Hudson Valley and discover its National Heritage Area rich scenic, historic, cultural, and recreational and I Love NY. -
V-1 Reconstructing the Paleoecology Of
RECONSTRUCTING THE PALEOECOLOGY OF HAVERSTRAW TIDAL MARSHLANDS A Final Report of the Tibor T. Polgar Fellowship Program Lucy Gill Polgar Fellow Department of Ecology, Evolution and Environmental Biology Columbia University New York, NY 10027 Project Advisor: Dorothy Peteet Lamont-Doherty Earth Observatory Columbia University Palisades, NY 10964 Gill, L. and D. Peteet. 2018. Reconstructing the Paleoecology of Haverstraw Tidal Marshlands. Section V:1-43 pp. In D.J. Yozzo, S.H. Fernald, and H. Andreyko (eds.), Final Reports of the Tibor T. Polgar Fellowship Program, 2015. Hudson River Foundation. V-1 ABSTRACT Climate change, a timely topic, cannot be understood solely by analyzing modern- day ecosystems. Sediment stratigraphy from tidal marshes is an important source of paleoecological data, as these ecosystems experience high rates of deposition and preserve organic material well. Although Hudson River Valley marshes have been extensively researched, work has focused on the four areas protected by the Hudson River National Estuarine Research Reserve (HRNERR). The marshlands of Haverstraw in Rockland County are comparable to the HRNERR sites in their capacity for biodiversity, carbon sequestration, and other important ecological functions. They are, however, understudied. This study uses loss-on-ignition and macrofossil analysis in combination with X-ray fluorescence spectroscopy to construct a high-resolution paleoenvironmental record. Biotic and geochemical zones have been identified and correlated with archaeological and historical data to assess the influence of anthropogenic activity in the area. The organic:inorganic maxima evidenced likely correspond to a pre- industrial period, characterized by burning events associated with increasing populations and concentrated settlement, as well as agricultural practices. -
Indian Point Unit 3 Revision 7 to Updated Final Safety Analysis
IP3 FSAR UPDATE CHAPTER 2 SITE AND ENVIRONMENT 2.1 SUMMARY OF CONCLUSIONS This Chapter sets forth the site and environmental data which together formed the basis for many of the criteria for designing the facility and for evaluating the routine and accidental releases of radioactive liquids and gases to the environment. These data support the conclusion that there will be no undue risk to public health and safety due to plant operation. The strength of this conclusion rests with these data and the determinations (also included in this report) of several independent consultants, each speaking within a particular area of expertise - health physics, demography, geology, seismology, hydrology or meteorology, as the case may be. The task of evaluating the environmental characteristics of the area was facilitated by the fact that more than 12 years of studies and measurements of environmental characteristics were undertaken. For over twenty years, measurements have been made of the effects on the environment of releases from at least one operating nuclear power facility at the Indian Point Site. Conservative projections have been made of the growth of population in the area and these projections have been taken into account in plant design and operation as to control the effects of accidents. Population estimates are presented in subchapter 2.4. The census data for 1990 reveals that the population within a 10-mile radius of the site was approximately 238,043 whereas the 2000 estimated population is 564,200. The land is now zoned principally for residential and state park usage although there is some industrial activity and a little agricultural and grazing activity.