New York Bight
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Past Tibor T. Polgar Fellowships
Past Tibor T. Polgar Fellowships The Hudson River estuary stretches from its tidal limit at the Federal Dam at Troy, New York, to its merger with the New York Bight, south of New York City. Within that reach, the estuary displays a broad transition from tidal freshwater to marine conditions that are reflected in its physical composition and the biota it supports. These characteristics present a major opportunity and challenge for researchers to describe the makeup and workings of a complex and dynamic ecosystem. The Tibor T. Polgar Fellowship Program provides funds for graduate and undergraduate students to study selected aspects of the physical, chemical, biological, and public policy realms of the estuary. Since its inception in 1985, the program has provided approximately $1 million in funding to 189 students and can boast the involvement of 116 advisors from 64 institutions. The program is named in memory of Dr. Tibor T. Polgar, an estuarine biologist who was a key advisor to the Hudson River Foundation for Science and Environmental Research when the fellowship program was created. The program is conducted jointly by the Hudson River Foundation and the New York State Department of Environmental Conservation. The fellowships are funded by the Foundation. Past reports of the Tibor T. Polgar Fellowship program are listed below. Download the entire report or particular sections as PDF files. Final Reports of the Tibor T. Polgar Fellowship Program, 2019 - Sarah Fernald, David Yozzo, and Helena Andreyko, editors I. Use of Gadolinium to Track Sewage Effluent Through the Poughkeepsie, New York Water System – Matthew Badia, Dr. -
Modeling Regional Coastal Evolution in the Bight Of
MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, Johan Reyns To cite this version: Ondoa Gregoire Abessolo, Magnus Larson, Rafael Almar, Bruno Castelle, Edward Anthony, et al.. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA. Coastal Sediments’19, May 2019, Tampa, United States. 10.1142/9789811204487_0178. hal-02394959 HAL Id: hal-02394959 https://hal.archives-ouvertes.fr/hal-02394959 Submitted on 11 Dec 2019 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. MODELING REGIONAL COASTAL EVOLUTION IN THE BIGHT OF BENIN, GULF OF GUINEA, WEST AFRICA ONDOA GREGOIRE ABESSOLO1,2, MAGNUS LARSON3, RAFAEL ALMAR1, BRUNO CASTELLE4, EDWARD J. ANTHONY5, J. REYNS6,7 1. LEGOS, OMP, UMR 5566 (CNRS/CNES/IRD/Université de Toulouse), 14 Avenue Edouard Belin, 31400, Toulouse, France. [email protected], [email protected]. 2. Ecosystems and Fisheries Resources Laboratory, University of Douala, BP 2701, Douala, Cameroun. 3. Department of Water Resources Engineering, Lund University, Box 118, S-221 00, Lund, Sweden. [email protected]. 4. EPOC, OASU, UMR 5805 (CNRS - Université de Bordeaux), Allée Geoffroy Saint- Hilaire – CS 50023 – 33615, Pessac Cedex, France. -
New York City Comprehensive Waterfront Plan
NEW YORK CITY CoMPREHENSWE WATERFRONT PLAN Reclaiming the City's Edge For Public Discussion Summer 1992 DAVID N. DINKINS, Mayor City of New lVrk RICHARD L. SCHAFFER, Director Department of City Planning NYC DCP 92-27 NEW YORK CITY COMPREHENSIVE WATERFRONT PLAN CONTENTS EXECUTIVE SUMMA RY 1 INTRODUCTION: SETTING THE COURSE 1 2 PLANNING FRA MEWORK 5 HISTORICAL CONTEXT 5 LEGAL CONTEXT 7 REGULATORY CONTEXT 10 3 THE NATURAL WATERFRONT 17 WATERFRONT RESOURCES AND THEIR SIGNIFICANCE 17 Wetlands 18 Significant Coastal Habitats 21 Beaches and Coastal Erosion Areas 22 Water Quality 26 THE PLAN FOR THE NATURAL WATERFRONT 33 Citywide Strategy 33 Special Natural Waterfront Areas 35 4 THE PUBLIC WATERFRONT 51 THE EXISTING PUBLIC WATERFRONT 52 THE ACCESSIBLE WATERFRONT: ISSUES AND OPPORTUNITIES 63 THE PLAN FOR THE PUBLIC WATERFRONT 70 Regulatory Strategy 70 Public Access Opportunities 71 5 THE WORKING WATERFRONT 83 HISTORY 83 THE WORKING WATERFRONT TODAY 85 WORKING WATERFRONT ISSUES 101 THE PLAN FOR THE WORKING WATERFRONT 106 Designation Significant Maritime and Industrial Areas 107 JFK and LaGuardia Airport Areas 114 Citywide Strategy fo r the Wo rking Waterfront 115 6 THE REDEVELOPING WATER FRONT 119 THE REDEVELOPING WATERFRONT TODAY 119 THE IMPORTANCE OF REDEVELOPMENT 122 WATERFRONT DEVELOPMENT ISSUES 125 REDEVELOPMENT CRITERIA 127 THE PLAN FOR THE REDEVELOPING WATERFRONT 128 7 WATER FRONT ZONING PROPOSAL 145 WATERFRONT AREA 146 ZONING LOTS 147 CALCULATING FLOOR AREA ON WATERFRONTAGE loTS 148 DEFINITION OF WATER DEPENDENT & WATERFRONT ENHANCING USES -
Island Wakes in the Southern California Bight R
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, C11012, doi:10.1029/2004JC002675, 2005 Island wakes in the Southern California Bight R. M. A. Caldeira,1,2 P. Marchesiello,3 N. P. Nezlin,4 P. M. DiGiacomo,5 and J. C. McWilliams3 Received 19 August 2004; revised 21 February 2005; accepted 14 June 2005; published 18 November 2005. [1] Wind- and current-induced island wakes were investigated using a multiplatform approach of in situ, remote sensing, and numerical model simulations for the Southern California Bight (SCB). Island wind wakes are a result of sheltering from the wind, with weak wind mixing, strong heat storage, and consequent high sea surface temperature (SST). Wind wakes around Santa Catalina Island are most persistent during spring and summer months. Current wakes, caused by the disruption of the poleward traveling California Countercurrent, induce eddies to form off the north end of Catalina Island, and these move poleward every 9–12 days. Current wake eddies induce strong mixing, with low SST and high-density sea surface signatures, whereas wind wakes induce high sea surface temperature signatures associated with the formation of a well-defined shallow thermocline. Current wake eddies vary from 1 to 30 km in diameter. From numerical solutions we predicted the frequency of occurrence of current-induced wakes off Santa Catalina Island. Wind wakes were also observed off all the other islands of the SCB as seen from the analysis of synthetic aperture radar data. Time series analysis of the island mass effect phenomenon has shown a concurrence of low SST and high sea surface chlorophyll for Santa Catalina, San Nicholas, and San Clemente islands that might be related to the seasonality of the California Current and California Countercurrent. -
Stony Brook University
SSStttooonnnyyy BBBrrrooooookkk UUUnnniiivvveeerrrsssiiitttyyy The official electronic file of this thesis or dissertation is maintained by the University Libraries on behalf of The Graduate School at Stony Brook University. ©©© AAAllllll RRRiiiggghhhtttsss RRReeessseeerrrvvveeeddd bbbyyy AAAuuuttthhhooorrr... Submerged Evidence of Early Human Occupation in the New York Bight A Dissertation Presented by Daria Elizabeth Merwin to The Graduate School in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University August 2010 Stony Brook University The Graduate School Daria Elizabeth Merwin We, the dissertation committee for the above candidate for the Doctor of Philosophy degree, hereby recommend acceptance of this dissertation. David J. Bernstein, Ph.D., Advisor Associate Professor, Anthropological Sciences John J. Shea, Ph.D., Chairperson of Defense Associate Professor, Anthropological Sciences Elizabeth C. Stone, Ph.D. Professor, Anthropological Sciences Nina M. Versaggi, Ph.D. Department of Anthropology, Binghamton University This dissertation is accepted by the Graduate School Lawrence Martin Dean of the Graduate School ii Abstract of the Dissertation Submerged Evidence of Early Human Occupation in the New York Bight by Daria Elizabeth Merwin Doctor of Philosophy in Anthropology (Archaeology) Stony Brook University 2010 Large expanses of the continental shelf in eastern North America were dry during the last glacial maximum, about 20,000 years ago. Subsequently, Late Pleistocene and Early Holocene climatic warming melted glaciers and caused global sea level rise, flooding portions of the shelf and countless archaeological sites. Importantly, archaeological reconstructions of human subsistence and settlement patterns prior to the establishment of the modern coastline are incomplete without a consideration of the whole landscape once available to prehistoric peoples and now partially under water. -
Regional Geologic Framework of the Inner-Continental Shelf Off New York: Baseline Information for Environmental and Resource Management
REGIONAL GEOLOGIC FRAMEWORK OF THE INNER-CONTINENTAL SHELF OFF NEW YORK: BASELINE INFORMATION FOR ENVIRONMENTAL AND RESOURCE MANAGEMENT William C. Schwab, E. Robert Thieler, Bradford Butman, and Marilyn R. Buchholtz ten Brink (U.S. Geological Survey, 384 Woods Hole Road, Woods Hole, MA 02543-2310) A focus for the U.S. Geological Survey (USGS) Coastal and Marine Geology Program is mapping of the shallow Exclusive Economic Zone (EEZ), with an emphasis on the heavily utilized areas of the sea floor offshore of major metropolitan centers. Our objective is to develop a regional synthesis of the sea-floor geology that will provide information for a wide range of management decisions and form a basis for further process-oriented investigations. In 1995, the USGS began a program, in cooperation with the U.S. Army Corps of Engineers (USACE), to generate geologic maps of the sea floor and shallow subsurface for coastal waters offshore of the New York — New Jersey metropolitan area and along the south shore of Long Island (Figure 1). Figure 1: Map showing location of the study area. Bathymetric contours are in meters. Boxed area shows extent of geophysical and geologic survey. The New York Bight Apex is one of the most heavily populated impacted coastal regions of the United States. Major issues in the New York — New Jersey area include: the long- term fate and effect of contaminated sediments; identification of acceptable sites for disposal of dredged material; identification of offshore sand and gravel resources; coastal erosion; and alterations of the benthic habitat caused by bottom trawling. A regional synthesis of the sea floor geology is needed to provide the information necessary to address these issues from a system-wide perspective. -
Science for Solutions
Science for Solutions NOAA COASTAL OCEAN PROGRAM Decision Analysis Series No. 15 Characterization of Hypoxia Topic 1 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico Nancy N. Rabalais, R. Eugene Turner, Dubravko Justic´, Quay Dortch, and William J. Wiseman, Jr. May 1999 U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Ocean Service Coastal Ocean Program GULF OF MEXICO HYPOXIA ASSESSMENT This report is the first in a series of six reports developed as the scientific basis for an integrated assessment of the causes and consequences of hypoxia in the Gulf of Mexico, as requested by the White House Office of Science and Technology Policy and as required by Section 604a of P.L. 105-383. For more information on the assessment and the assessment process, please contact the National Centers for Coastal Ocean Science at (301) 713-3060. DECISION ANALYSIS SERIES The Decision Analysis Series has been established by NOAA's Coastal Ocean Program (COP) to present documents for coastal decision mak- ers which contain analytical treatments of major issues or topics. The is- sues, topics, and principal investigators have been selected through an extensive peer review process. To learn more about the COP or the De- cision Analysis Series, please write to: NOAA National Centers for Coastal Ocean Science Coastal Ocean Program 1315 East-West Highway, Room 9700 Silver Spring, Maryland 20910 phone: 301-713-3338 fax: 301-713-4044 web: http://www.cop.noaa.gov e-mail: [email protected] Cover image: Extent of bottom water with dissolved oxygen less than 2 mg/l for July 1996 (based on data of Rabalais, Turner, and Wiseman). -
New York Ocean Action Plan 2016 – 2026
NEW YORK OCEAN ACTION PLAN 2016 – 2026 In collaboration with state and federal agencies, municipalities, tribal partners, academic institutions, non- profits, and ocean-based industry and tourism groups. Acknowledgments The preparation of the content within this document was developed by Debra Abercrombie and Karen Chytalo from the New York State Department of Environmental Conservation and in cooperation and coordination with staff from the New York State Department of State. Funding was provided by the New York State Environmental Protection Fund’s Ocean & Great Lakes Program. Other New York state agencies, federal agencies, estuary programs, the New York Ocean and Great Lakes Coalition, the Shinnecock Indian Nation and ocean-based industry and user groups provided numerous revisions to draft versions of this document which were invaluable. The New York Marine Sciences Consortium provided vital recommendations concerning data and research needs, as well as detailed revisions to earlier drafts. Thank you to all of the members of the public and who participated in the stakeholder focal groups and for also providing comments and revisions. For more information, please contact: Karen Chytalo New York State Department of Environmental Conservation [email protected] 631-444-0430 Cover Page Photo credits, Top row: E. Burke, SBU SoMAS, M. Gove; Bottom row: Wolcott Henry- 2005/Marine Photo Bank, Eleanor Partridge/Marine Photo Bank, Brandon Puckett/Marine Photo Bank. NEW YORK OCEAN ACTION PLAN | 2016 – 2026 i MESSAGE FROM COMMISSIONER AND SECRETARY The ocean and its significant resources have been at the heart of New York’s richness and economic vitality, since our founding in the 17th Century and continues today. -
HEP Habitat Status Report 2001.Pdf
New York/New Jersey Harbor Estuary Program Habitat Workgroup ;1 regional partnership of federal, state, interstate, and local agencies, citizens, and scientists working together to protect and restore the habitat and living resources of the estuary, its tributaries, and the New York/Nc•F]ersey Bight City of New York/Parks & Recreation Natural Resources Group Rudolph W. Giuliani, Maym Henry J. Stem, Commissioner Marc A. Matsil, Chief, Natllfal Resources Group Chair, Habitat Workgroup, NY/NJ Harbor Estuary Program Status Report Sponsors National Pish and Wildlife Foundation City of New York/Parks & Recreation U.S. Environmental Protection Agency New Jersey Department of Environmental Protection The Port Authority of New York & New Jersey City Parks Foundation HydroQual, Inc. Malcolm Pirnie, Inc. Lawler, Matusky & Skelly Engineers, LLP This document is approved by the New York/New Jersey Harbor Estuary Prowam Policr Committee. The Policy Committee's membership includes the U.S. linvironmental Protection !lgency, U.S. ,lrmr Corps of!ingineers, New York State Department of nnvimnmental Conservation, New Jersey Department of Environmental Protection, New York Local Government Representative (New York C'i~1· Dep;~rtment of Enl'imnmentnl Protection), Newjcrsey lJ>enl Government Rcpresentati1·e (Newark V?atershed Conservation and De,·elopment Corporation), and a Rcprcsent;JtiFe of the Citizens/Scientific and Technical Advisory Committees. Funds for this project were pnwided through settlement funds from the National Pish and \Vildlif(: Foundation. April 2001 Cover: Blue mussels (Mytilus edulis). North Brother Island. Bronx Opposite: Pelham Bay Park, Bronx New York/New Jersey Harbor Estuary Program Habitat Workgroup 2001 Status Report Table of Contents 4 Introduction 8 Section 1: Acquisition and Restoration Priorities 9 I. -
Island Wakes in the Southern California Bight R.M
Island wakes in the Southern California Bight R.M. Caldeira, P. Marchesiello, N. Nezlin, P. Digiacomo, J. C. Mcwilliams To cite this version: R.M. Caldeira, P. Marchesiello, N. Nezlin, P. Digiacomo, J. C. Mcwilliams. Island wakes in the Southern California Bight. Journal of Geophysical Research. Oceans, Wiley-Blackwell, 2005, 110, pp.C11012. 10.1029/2004JC002675.. hal-00280338 HAL Id: hal-00280338 https://hal.archives-ouvertes.fr/hal-00280338 Submitted on 19 Feb 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, C11012, doi:10.1029/2004JC002675, 2005 Island wakes in the Southern California Bight R. M. A. Caldeira,1,2 P. Marchesiello,3 N. P. Nezlin,4 P. M. DiGiacomo,5 and J. C. McWilliams3 Received 19 August 2004; revised 21 February 2005; accepted 14 June 2005; published 18 November 2005. [1] Wind- and current-induced island wakes were investigated using a multiplatform approach of in situ, remote sensing, and numerical model simulations for the Southern California Bight (SCB). Island wind wakes are a result of sheltering from the wind, with weak wind mixing, strong heat storage, and consequent high sea surface temperature (SST). -
Special Aspects of Marine Naming
The UNGEGN International Course on Toponymy, Manila, 2018 Special Aspects of Naming for Marine Toponymy Hyo Hyun Sung Professor, Ewha Womans University 1 CONTENTS 1. Marine Geographical Names 2. Principles, Policies, and Procedures 3. Special Issues for Sea Surface Generic Terms 2 01. Marine Geographical Names 3 1.1 Marine Geographical Names • Marine geographical names can be divided into sea surface feature names and undersea feature names. Marine Geographical Names Sea Surface Undersea Feature Feature Names Names 4 The UNGEGN International Course on Toponymy, Manila, 2018 1.1 Marine Geographical Names • Sea surface feature names can be further classified into feature types in the sea, waterway, rocks in low-tide elevation, and Indentation. Sea Surface Feature Names Rocks in low-tide Sea Waterway Indentation elevation Rock which Strait, Channel, Gulf, Bay, bight, Ocean, Sea covers and Passage Inlet/Creek uncovers 5 The UNGEGN International Course on Toponymy, Manila, 2018 1.1 Marine Geographical Names • In the case of undersea feature names, 43 generic terms were listed in B-6 (IHO, 2013) Archipelagic apron, Guyot(s), Fracture zone, Borderland, Continental rise, Continental shelf, Shelf-edge, Shelf Break, Shelf, Slope, Continental Margin, Mid-oceanic ridge, Shoal(s), Moat, Sill, Abyssal hill(s), Abyssal plain, Saddle, Apron, Median valley, Province, Reef(s), Bank(s), Tablemount(s), Caldera, Spur, Trough, Trench, Peak(s), Seamount(s), Seamount chain, Gap, Passage, Valley(s), Submarine valley(s), Sea valley(s), Promontory, Hill(s), Knoll(s), Terrace(s), Plateau, Basin, Cone, Fan, Seachannel(s), Ridge, Escarpment, Scarp, Levee, Hole, Canyon(s), Pinnacle(s), Rise, Deep(s) Except the GENERIC TERMS USED FOR HARMONIZATION WITH OTHER GAZETTEERS which are used for some features in the GEBCO Gazetteer and in other gazetteers. -
Extent of Mississippi River Water in the Mississippi Bight and Louisiana Shelf Based on Water Isotopes Virginie Sanial, Alan Shiller, Dongjoo Joung, Peng Ho
Extent of Mississippi River water in the Mississippi Bight and Louisiana Shelf based on water isotopes Virginie Sanial, Alan Shiller, Dongjoo Joung, Peng Ho To cite this version: Virginie Sanial, Alan Shiller, Dongjoo Joung, Peng Ho. Extent of Mississippi River water in the Mississippi Bight and Louisiana Shelf based on water isotopes. Estuarine, Coastal and Shelf Science, Elsevier, 2019, 226, pp.106196. 10.1016/j.ecss.2019.04.030. hal-02511271 HAL Id: hal-02511271 https://hal.archives-ouvertes.fr/hal-02511271 Submitted on 18 Mar 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. (VWXDULQH&RDVWDODQG6KHOI6FLHQFH Contents lists available at ScienceDirect Estuarine, Coastal and Shelf Science journal homepage: www.elsevier.com/locate/ecss Extent of Mississippi River water in the Mississippi Bight and Louisiana Shelf 7 based on water isotopes ∗ Virginie Saniala, , Alan M. Shillera,DongJooJoungb, Peng Hoa a University of Southern Mississippi, School of Ocean Science & Engineering, 1020 Balch Boulevard, Stennis Space Center, MS, 39529, USA b University of Rochester, Earth and Environmental Sciences, 227 Hutchison Hall, P.O. Box 270221, Rochester, NY, 14627, USA ARTICLE INFO ABSTRACT Keywords: The northern Gulf of Mexico is a complex and very productive coastal river-dominated system that receives Mississippi River freshwater from numerous rivers including the Mississippi River.