Lonsdale Bight Investigations Review and Options Overview
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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. -
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. -
Ees Inquiry Greater Geelong Planning Scheme: Amendment C150 and Pp673/2007
Environment Effects Act 1978 Planning and Environment Act 1987 EES INQUIRY GREATER GEELONG PLANNING SCHEME: AMENDMENT C150 AND PP673/2007 STOCKLAND WATERWAYS AND RESIDENTIAL DEVELOPMENT POINT LONSDALE REPORT OF THE PANEL Panel: Kathryn Mitchell William O’Neil Peter Sheehan Catherine Wilson October 2008 EES: Stockland Waterways and Residential Development, Point Lonsdale Greater Geelong Scheme: Amendment C150 and PP673/2007 Report of the Panel: October 2008 EES INQUIRY and GREATER GEELONG PLANNING SCHEME: AMENDMENT C150 AND PP673/2007 STOCKLAND WATERWAYS AND RESIDENTIAL DEVELOPMENT REPORT OF THE PANEL Kathryn Mitchell, Chair William O’Neil, Member Peter Sheehan, Member Catherine Wilson, Member October 2008 EES: Stockland Waterways and Residential Development, Point Lonsdale Greater Geelong Scheme: Amendment C150 and PP673/2007 Report of the Panel: October 2008 TABLE OF CONTENTS PAGE NO. EXECUTIVE SUMMARY.......................................................................................................1 PART 1: BACKGROUND......................................................................................................5 1. INTRODUCTION.................................................................................................6 1.1 THE PANEL ...................................................................................................................6 1.2 TERMS OF REFERENCE ..................................................................................................7 1.3 SUBMISSIONS AND HEARINGS......................................................................................8 -
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 Bight
NEW YORK BIGHT RESTORATION PLAN REPORT TO CONGRESS NEW YORK BIGHT RESTORATION PLAN FINAL REPORT MARCH 1993 A PRODUCT ,.·F THE NEW YORK-NEW JERSa:'. 1j;U>\RY PROGR/,.� MANAGEMENT cu;·:�·.:RENCE TABLE OF CONTENTS EXECUTIVE SUMMARY S-1 Use Impairments and Precipitating Pollutant Factors S-1 Floatable Debris S-2 Pathogen Contamination S-2 Toxic Contamination S-3 Nutrient and Organic Enrichment S-4 Habitat Loss and Degradation S-5 Program Administration S-5 INTRODUCTION 1 General 1 Congressional Mandate 1 Prior Reports and Activities 2 Preliminary Problem Assessment 3 RESTORATION PLAN MODULES 4 Floatable Debris 5 Introduction 5 Short-term Floatables Action Plan 5 Comprehensive Floatables Plan 6 Independent Activities and Public Education 7 MARPOL Annex V 7 Recycling and Waste Reduction 8 Program Constraints 8 Program Follow-Up 9 Pathogen Contamination 9 Introduction 9 Beach/Shellfish Bed Closure Action Plan 9 Ocean Dumping Ban Act 10 Combined Sewer Overflow (CSO) Abatement Program 10 Alternative Pathogenic Indicator Study 10 Program Constraints 11 Program Follow-Up 11 3. Toxic Contamination 11 Introduction 11 Problem Characterization 12 Total Maximum Daily Load/Wasteload Allocation (TMDL/WLA) 13 Antidegradation 14 TABLE OF CONTENTS (cont.) Toxic Contamination (cont.) Dredged Material Management 14 Ecosystem Indicators 16 Other Existing Programs and Authorities 16 Program Constraints and Follow-Up 17 Nutrient and Organic Enrichment 17 Introduction 17 Problem Characterization 17 Eutrophication Modeling 18 Ecosystem Indicators 18 Program Constraints and Follow-Up 19 5. Habitat Loss and Degradation 19 Introduction 19 Habitat Inventory 19 Regulatory Programs 20 Non-Regulatory Approach 20 Geographic Targeting 20 Program Constraints 20 Program Follow-Up 21 A Comprehensive Focus 21 Program Administration 22 LIST OF FIGURES Figure 1 - The New York Bight 2 Figure 2 - The New York-New Jersey Harbor 3 Figure 3 - Management Conference Membership and Structure 5 ATTACHMENTS 1. -
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. -
THE PINNIPEDS of the CALIFORNIA CURRENT California
ANTONELIS AND FISCUS: PINNIPEDS OF THE CALIFORNIA CURRENT CalCOFI Rep., Vol. XXI, 1980 THE PINNIPEDS OF THE CALIFORNIA CURRENT GEORGE A. ANTONELIS. JR. AND CLIFFORD H. FISCUS Marine Mammal Division Northwest and Alaska Fisheries Center National Marine Fisheries Service National Oceanic and Atmospheric Administration 7600 Sand Point Way, N.E. Seattle, WA 981 15 ABSTRACT 10s pequenos peces en 10s cardumenes y peces ana- There are six species of pinnipeds-California sea dromos. Los dos focidos, otra vez con ciertas excep- lion, Zalophus californianus; northern sea lion, Eume- ciones, predan especies diferentes. Aparentemente, el topias jubatus; northern fur seal, Callorhinus ursinus; elefante marino se alimenta en aguas mas profundas que Guadalupe fur seal, Arctocephalus townsendi; harbor la foca peluda, alimentindose de especies demersales seal, Phoca uitulina richardsi; and northern elephant y benticas, y la foca peluda se alimenta de especiesdemer- seal, Mirounga angustirostris-that inhabit the study sales costeras y neriticas, entrando ocasionalmente en rios area of the California Cooperative Oceanic Fisheries y aguas estuarinas haciendopresa de 10s peces anadromos Investigations (CalCOFI). y otros pequeiios peces que entran regularmente en estas The numbers of animals in each population are given; aguas. the size, distribution, and seasonal movements are de- scribed. The known prey species of the pinnipeds are INTRODUCTION listed for each species. The otariids, with certain excep- The California Current, its components, and the Cali- tions, consume the same kinds of prey, although in slight- fornia Cooperative Oceanic Fisheries Investigations ly different amounts. In general they feed most commonly (CalCOFI) station plan have been described many times on the smaller schooling fishes and squids of the epi- in the past and are well known (Kramer et al. -
A Bight Is Born
Islands in the Stream 2002: Exploring Underwater Oases A Bight is Born FOCUS Limestone The origin and structure of the southeast coastline Taconic Orogeny and continental shelf (South Atlantic Bight) Microcontinent Collisions GRADE LEVEL Alleghenian Orogeny 9 -12 (Earth Science) Equator (may be adapted to 7th-8th grade Earth Science Piedmont Standards) Monadnocks Rift basins FOCUS QUESTION Erosion What is the South Atlantic Bight and how was it Coastal formed? Volcanic Sediment LEARNING OBJECTIVES Continental shelf Students will sequence and model the events lead- Regresses ing to the formation of the southeastern coast of the Ecosystems United States, including the formation of the South Atlantic Bight. The words listed as key words are integral to the unit. There are no formal signs in American Sign Students will examine what forces have changed Language for any of these words and many are the structure of this area over geologic time, pre- difficult to lipread. Having the vocabulary list on dict what changes are yet to occur and how these the board as a reference during the lesson will be changes have and may affect the populations living extremely helpful. This activity presents a great in this area, including man. deal of new material and requires a large amount of reading and attention. Many new words which ADDITIONAL INFORMATION FOR TEACHERS OF DEAF STUDENTS might be unfamiliar are included. This activity is In addition to the words listed as Key Words, the best conducted as a review or as an activity after following words should be part of the vocabulary the concepts have been taught. -
Planning and Environment Act 1987 GREATER GEELONG PLANNING SCHEME AMENDMENT C165 QUEENSCLIFFE PLANNING SCHEME AMENDMENT C22 EXPL
Planning and Environment Act 1987 GREATER GEELONG PLANNING SCHEME AMENDMENT C165 QUEENSCLIFFE PLANNING SCHEME AMENDMENT C22 EXPLANATORY REPORT Who is the planning authority? The amendments have been prepared by the Minister for Planning. The Minister for Planning is the planning authority for the amendments. The amendments have been prepared at the request of the Greater Geelong City Council and the Queenscliffe Borough Council. Land affected by the amendments. Amendment C165 to the Greater Geelong Planning Scheme applies to all land in the Point Lonsdale township located within the municipal bounds of the City of Greater Geelong (located generally west of Fellows Road). Amendment C22 to the Queenscliffe Planning Scheme applies to all land in the Point Lonsdale township located within the municipal bounds of the Borough of Queenscliffe (locally generally east of Fellows Road). The extent of the Point Lonsdale township is shown on the Point Lonsdale Structure Plan Map (contained in the Point Lonsdale Structure Plan April 2009). What the amendment does. The amendments make changes to the Local Planning Policy Frameworks of the Greater Geelong Planning Scheme and Queenscliffe Planning Scheme to recognise the Point Lonsdale Structure Plan April 2009. The changes are as follows: Greater Geelong Planning Scheme The amendment (C165) proposes to amend the Local Planning Policy Framework as follows: • In Clause 21.14-include land use and policy directions for Point Lonsdale; recognise the Point Lonsdale Structure Plan April 2009 as a reference document; and insert the Point Lonsdale Structure Plan Map. Queenscliffe Planning Scheme The amendment (C22) proposes to amend the Local Planning Policy Framework as follows: • In Clause 21.04 – recognise the community vision for Point Lonsdale and insert the Point Lonsdale Structure Plan Map. -
'Tongue of Land' Is the Wadawurrung / Wathaurong
DJILLONG Djillong: ‘tongue of land’ is the Wadawurrung / Wathaurong Aboriginal name for Geelong TIMELINE www.djillong.net.au At least 65,000 years ago Evidence of Aboriginal people living on the Australian continent and of the world’s earliest human art. (French cave painting 5,000 years ago, the Mona Lisa, 14th century) 1600s 1688 William Dampier (England) lands on the west coast of Australia. 1700s 1770 Captain James Cook (England) lands on the east coast of Australia. 1800s 1800 Lt James Grant (Lady Nelson ship) sails through Bass Strait. 1802 Dispossession in the Geelong district begins as Lieutenant John Murray takes possession of Port Phillip in King George III’s name and raises the British flag. First contact between Wadawurrung and the Europeans. William Buckley escapes from Capt. Collins’ temporary settlement at Sorrento and walks around Port Phillip Bay. Later he is invited to join the Mon:mart clan of Wadawurrung People when Kondiak:ruk 1803 (Swan Wing) declares him her husband returned from the dead. Aboriginal people believed that the dead were reincarnated in a white form. They call Buckley Morran:gurk (Ghost blood). 1820s 1824 Hume & Hovell arrive on Wadawurrung land at Corio Bay and are greeted by Wadawurrung resistance. In Tasmania settlers are authorised to shoot Aboriginal people. Martial law is declared in Bathurst (NSW) after violent clashes between settlers and Aboriginal people. 1827 Batman and Gellibrand apply to the colonial government for Kulin nation land. 1828 Martial law declared in Tasmania where the Solicitor General says ‘the Aborigines are the open enemies of the King and in a state of actual warfare against him’.