Gulf Hypoxia Action Plan 2008 (Pdf)
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Hypoxia Infographic
Understanding HYP XIA Hypoxia is an environmental phenomenon where the concentration of dissolved oxygen in the water column decreases to a level that can no longer 1 support living aquatic organisms. The level is often considered to be 2 mg O2 per liter of water or lower. Hypoxic and anoxic (no oxygen) waters have existed throughout geologic time, but their occurrence in shallow coastal and estuarine areas appears to be increasing as a result of human activities. 2 What causes hypoxia? In 2015, scientists determined the Gulf of Mexico dead zone to be 6,474 square miles, which is an area about the size of Connecticut and Rhode Island combined. 3 Major events leading to the formation of hypoxia in the Gulf of Mexico include: Coastal Hypoxia and Eutrophication Sunlight Watershed Areas of anthropogenically-influenced n> In the past century, Hypoxia has become a global concern with estuarine and coastal hypoxia. 550 over 550 coastal areas identified as experiencing this issue. 4 Runoff and nutrient 1 loading of the Mississippi River. Nutrient-rich water from the Mississippi River forms 1960 a surface lens. 1970 Combined, Dead Zones 1980 cover 4x the area of the 1990 Great Lakes. % 2000 Nutrient-enhanced 4 2 primary production, Only a small fraction of the 550-plus Number of dead zones has approximately Today, there is currently about 1,148,000 km2 or eutrophication. hypoxia zones exhibited any signs doubled each decade since the 1960’s. 5 of seabed covered by Oxygen Minimum Phytoplankton growth of improvement. 5 Zones (OMZs) (<0.5 ml of O /liter) 5 is fueled by nutrients. -
Gulf of Mexico Hypoxia Monitoring Strategy
Gulf of Mexico Hypoxia Monitoring Strategy Hypoxia Zone Areal Extent (km2) Interpolation Observations Data Analysis Workshop Steering Committee Trevor Meckley, Alan Lewitus, A White Paper by the Steering Committee of the: Dave Scheurer, Dave Hilmer NOAA National Ocean Service, National 6th Annual NOAA/NGI Hypoxia Research Centers of Coastal Ocean Science Coordination Workshop: Establishing a Steve Ashby Cooperative Hypoxic Zone Monitoring Program Northern Gulf Institute convened by the NOAA National Centers for Steve DiMarco Texas A&M University Coastal Ocean Science and Northern Gulf Institute Steve Giordano on 12-13 September 2016 at the Mississippi State NOAA National Marine Fisheries Service University Science and Technology Center at Rick Greene NASA's Stennis Space Center in Mississippi. EPA Office of Research and Development Stephan Howden University of Southern Mississippi Barb Kirkpatrick Gulf of Mexico Coastal Ocean Observing System Troy Pierce EPA Gulf of Mexico Program Nancy Rabalais Louisiana Universities Marine Consortium Rick Raynie Louisiana Coastal Protection and Restoration Authority Mike Woodside USGS National Water Quality Program Abstract The Gulf of Mexico Hypoxia Monitoring Strategy is a resource to inform the proceedings of the 6th Annual NOAA/NGI Hypoxia Research Coordination Workshop: Establishing a Cooperative Hypoxic Zone Monitoring Program. It provides a framework for a cooperative hypoxia monitoring program based on programmatic and financial requirements that are designed to meet management needs. The Monitoring Strategy includes sections on management drivers, current monitoring capabilities and gaps, and projected programmatic, data, and financial requirements based on the input of multiple partners and the responses from a survey of modelers currently applying deterministic 3D time variable models to Gulf hypoxia assessment and prediction. -
GEOG 101 PLACE NAME LIST for EXAM THREE
GEOG 101 PLACE NAME LIST for EXAM THREE Each exam will have a place name location map section based on the list below, plus countries and political units. Consult the appropriate maps in the atlas and textbook to locate these places. The atlas has a detailed INDEX. Exam III will focus on place names from Asia and Oceania. This section of the exam will be in the form of a matching question. You will match the names to numbers on a map. ________________________________________________________________________________ I. CONTINENTS Australia Asia ________________________________________________________________________________ II. OCEANS Pacific Indian Arctic ________________________________________________________________________________ III. ASIA Seas/Gulfs/Bays/Lakes: Caspian Sea Sea of Japan Arabian Sea South China Sea Red Sea Aral Sea Lake Baikal East China Sea Bering Sea Persian Gulf Bay of Bengal Sea of Okhotsk ________________________________________________________________________________ Islands: New Guinea Taiwan Sri Lanka Singapore Maldives Sakhalin Sumatra Borneo Java Honshu Philippines Luzon Mindanao Cyprus Hokkaido ________________________________________________________________________________ Straits/Canals: Str. of Malacca Bosporas Dardanelles Suez Canal Str. of Hormuz ________________________________________________________________________________ Rivers: Huang Yangtze Tigris Euphrates Amur Ob Mekong Indus Ganges Brahmaputra Lena _______________________________________________________________________________ Mountains, Plateaus, -
Guaraníes Y Jesuitas En La Provincia Paraquaria
GUARANIES Y JESUITAS EN LA PROVINCIA PARAQUARIA SEGUN LAS CRONICAS DE MONTOYA, CARDEEL Y PERAMAS (SIGLOS XVII Y XVIII) By FRANCISCO BUSTAMANTE A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2001 Copyright 2001 by Francisco Bustamante ACKNOWLEDGMENTS Many people have contributed to this work. The members of my committee were always available for dialogue and guidance. Professor Felix Bolanos, my chair made many fine and acute observations which were invaluable for the development of this work. He has also served as a role model; I will aspire to imitate him in my academic life. Professor Diane Marring stimulated my interest in research and gave me all the support I needed to accomplish my work. Professor Mark Thurner motivated me even further and always gave me very good advice. I give special thanks to Professor Charles Perrone for his critical observations that enriched my work and helped me see other possibilities for future research. Last but not least, I give very special thanks to Mr. Justino Llanque-Chana from the Latin American Collection, this work could not been completed without his permanent help. in TABLE OF CONTENTS page ACKNOWLEDGMENTS iii ABSTRACT vii 1 INTRODUCCION: LOS TEXTOS Y SU CONTEXTO 1 Objetivo y corpus 2 Bases hermeneuticas 5 Bases metodologicas 17 Textos de las misiones del Paraguay 23 Caracterizacion y justification de los cuatro textos 28 Ruiz de Montoya y su Conquista espiritual 28 Cardiel y sus Declaration de verdady Compendio de Historia del Paraguay . -
Mystique: the Pinnacle of the Ultra-Luxury Lifestyle in Naples
+ NAPLESNEWS.COM z FRIDAY, FEBRUARY 21, 2020 z 27T Mystique: The Pinnacle of the Ultra-Luxury Lifestyle in Naples ocated just steps from the beach and featuring a collection of elegantly-ap- amenities o er custom-designed interior spaces for socializing, including a club pointed and masterfully-designed residences, Mystique is redefi ning luxuri- room, parlor, salon, library and solarium/card room. Mystique also features a the- Lous beachfront living at one of Naples’ most prestigious addresses. ater, billiards room, board room, state-of-the-art health and fi tness club with the lat- The extraordinary lifestyle at this iconic 20-story tower surrounds residents in the est in exercise and wellness equipment, ladies’ and men’s steam rooms and showers, incomparable luxury – from expansive fl oorplans with walls of windows to spacious, and massage rooms with on-call masseurs and masseuses. private terraces showcasing breathtaking views, to world-class service and ameni- Residents may also enjoy the exclusive and renowned amenities of prestigious Peli- ties that cater to an exceptional lifestyle. can Bay, including private beachfront dining, extensive walking and biking trails, “Mystique is truly unique – even among the most luxurious o erings in Naples chau eured tram service, and private access to nearly three miles of unspoiled Gulf and beyond,” said Jennifer Urness, Director of Sales at Mystique. “It begins with the of Mexico beaches. prime location, the quality construction and the advanced technology. The extensive A limited number of estate residences at Mystique remain, ranging in size from resort-style amenities round out the incredible o ering. -
LOUISIANA K. Meyer-Arendt Department of Geography
65. USA--LOUISIANA K. Meyer-Arendt D.W. Davis Department of Geography Department of Earth Science Mississippi State University Nicholls State University Starkville, Mississippi 38759 Thibodaux, Louisiana 70301 United States of America United States of America INTRODUCTION Louisiana's 40,000 Inn 2 coastal zone developed over the last 7,000 years by the progradation, aggradation, and accretion of sediments introduced via various courses of the Mississippi River (Frazier 1967). The deltaic plain (32,000 km'), through which the modern river cuts diagon ally !Fig , 1), consists of vast wetlands and waterbodies. With eleva tions ranging from sea level up to 1.5 m, it is interrupted by natural levee ridges which decrease distally until they disappear beneath the marsh surface. The downdrift chenier plain of southwest Louisiana (8,000 km') consists of marshes, large round-to-oblong lakes, and stranded, oak covered beach ridges known as cheniers (Howe et al. 1935). This landscape is the result of alternating long-term phases of shoreline accretion and erosion that were dependent upon the proximit of an active sediment-laden river, and a low-energy marine environment (Byrne et al. 1959). Since the dyking of the Mississippi River, fluvial sedimentation in the deltaic plain has effectively been halted. Today, most Missis sippi River sediment is deposited on the outer continental shelf; only at the mouth of the Atchafalaya River distributary is deltaic sedimen tation subaerially significant (Adams and Baumann 1980). Over mos of the coastal zone, subsidence, saltwater intrusion, wave erosion, canalization, and other hydrologic modification have led to a rapid increase in the surface area of water (Davis 1986, Walker e al. -
Zooplankton Community Response to Seasonal Hypoxia: a Test of Three Hypotheses
diversity Article Zooplankton Community Response to Seasonal Hypoxia: A Test of Three Hypotheses Julie E. Keister *, Amanda K. Winans and BethElLee Herrmann School of Oceanography, University of Washington, Box 357940, Seattle, WA 98195, USA; [email protected] (A.K.W.); [email protected] (B.H.) * Correspondence: [email protected] Received: 7 November 2019; Accepted: 28 December 2019; Published: 1 January 2020 Abstract: Several hypotheses of how zooplankton communities respond to coastal hypoxia have been put forward in the literature over the past few decades. We explored three of those that are focused on how zooplankton composition or biomass is affected by seasonal hypoxia using data collected over two summers in Hood Canal, a seasonally-hypoxic sub-basin of Puget Sound, Washington. We conducted hydrographic profiles and zooplankton net tows at four stations, from a region in the south that annually experiences moderate hypoxia to a region in the north where oxygen remains above hypoxic levels. The specific hypotheses tested were that low oxygen leads to: (1) increased dominance of gelatinous relative to crustacean zooplankton, (2) increased dominance of cyclopoid copepods relative to calanoid copepods, and (3) overall decreased zooplankton abundance and biomass at hypoxic sites compared to where oxygen levels are high. Additionally, we examined whether the temporal stability of community structure was decreased by hypoxia. We found evidence of a shift toward more gelatinous zooplankton and lower total zooplankton abundance and biomass at hypoxic sites, but no clear increase in the dominance of cyclopoid relative to calanoid copepods. We also found the lowest variance in community structure at the most hypoxic site, in contrast to our prediction. -
Hypoxia the Gulf of Mexico’S Summertime Foe
Louisiana Coastal Wetlands Planning, Protection and Restoration News September 2004 Number 26 HYPOXIA THE GULF OF MEXICO’S SUMMERTIME FOE More Nitrogen Upstream, Fewer Filters Downstream Caernarvon: A Case Study WaterMarks Interview: John Day, LSU www.lacoast.gov September 2004 Number 26 WaterMarks is published three times a Louisiana Coastal Wetlands Planning, Protection and Restoration News year by the Louisiana Coastal Wetlands Conservation and Restoration Task Force to communicate news and issues Contents of interest related to the Coastal Wetlands Planning, Protection and Restoration Act of 1990. This legislation 3 Hypoxia: funds wetlands enhancement projects The Gulf of Mexico’s Summertime Foe nationwide, designating approximately $50 million annually for work in More Nitrogen Upstream, Louisiana. The state contributes 6 Fewer Filters Downstream 15 percent of the total cost of the project. Can Wetlands Restoration 8 Revitalize Offshore Waters? Caernarvon: 10 A Case Study What Lies Ahead 12 for the Dead Zone? Please address all questions, comments and changes of address to: WaterMarks Interview: James D. Addison 14 John Day, LSU WaterMarks Editor New Orleans District US Army Corps of Engineers P.O. Box 60267 Special thanks to Doug Daigle, Mississippi River Basin Alliance; Dugan Sabins, New Orleans, LA 70160-0267 (504) 862-2201 Louisiana State Hypoxia Committee; Ken Teague, U.S. Environmental Protection Agency; and Robert Twilley, Louisiana State University, for their assistance with e-mail: this issue of WaterMarks. [email protected] For more information about Louisiana’s coastal wetlands and the efforts planned and under way to ensure their survival, check out these sites on the web: www.lacoast.gov www.btnep.org www.saveLAwetlands.org About the Cover Blue Runners, a common Gulf Subscribe species, have the ability to escape To receive WaterMarks, e-mail [email protected] from waters with low oxygen con- For current meetings, events, and other news concerning Louisiana’s coastal tent. -
The Economics of Dead Zones: Causes, Impacts, Policy Challenges, and a Model of the Gulf of Mexico Hypoxic Zone S
58 The Economics of Dead Zones: Causes, Impacts, Policy Challenges, and a Model of the Gulf of Mexico Hypoxic Zone S. S. Rabotyagov*, C. L. Klingy, P. W. Gassmanz, N. N. Rabalais§ ô and R. E. Turner Downloaded from Introduction The BP Deepwater Horizon oil spill in the Gulf of Mexico in 2010 increased public awareness and http://reep.oxfordjournals.org/ concern about long-term damage to ecosystems, and casual readers of the news headlines may have concluded that the spill and its aftermath represented the most significant and enduring environmental threat to the region. However, the region faces other equally challenging threats including the large seasonal hypoxic, or “dead,” zone that occurs annually off the coast of Louisiana and Texas. Even more concerning is the fact that such dead zones have been appearing worldwide at proliferating rates (Conley et al. 2011; Diaz and Rosenberg 2008). Nutrient over- enrichment is the main cause of these dead zones, and nutrient-fed hypoxia is now widely at Iowa State University on January 27, 2014 considered an important threat to the health of aquatic ecosystems (Doney 2010). The rather alarming term dead zone is surprisingly appropriate: hypoxic regions exhibit oxygen levels that are too low to support many aquatic organisms including commercially desirable species. While some dead zones are naturally occurring, their number, size, and *School of Environmental and Forest Sciences, University of Washington, Seattle, Washington, USA; e-mail: [email protected] yCenter for Agricultural and Rural Development, -
Coupling and Decoupling of High Biomass Phytoplankton Production and Hypoxia in a Highly Dynamic Coastal System: the Changjiang (Yangtze River) Estuary
fmars-07-00259 May 26, 2020 Time: 17:51 # 1 ORIGINAL RESEARCH published: 28 May 2020 doi: 10.3389/fmars.2020.00259 Coupling and Decoupling of High Biomass Phytoplankton Production and Hypoxia in a Highly Dynamic Coastal System: The Changjiang (Yangtze River) Estuary Feng Zhou1,2*, Fei Chai1,3*, Daji Huang1, Mark Wells3,1, Xiao Ma1, Qicheng Meng1, Huijie Xue3,4, Jiliang Xuan1, Pengbin Wang1,5, Xiaobo Ni1, Qiang Zhao6, Chenggang Liu1,5, Jilan Su5 and Hongliang Li1 1 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China, 2 School of Oceanography, Shanghai Jiao Tong University, Shanghai, China, 3 School Edited by: of Marine Science, University of Maine, Orono, ME, United States, 4 State Key Laboratory of Tropical Oceanography, South Marta Marcos, China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China, 5 Key Laboratory of Marine University of the Balearic Islands, Ecosystem Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou, China, 6 Ningbo Marine Spain Environment Monitoring Center Station, Ministry of Natural Resources, Ningbo, China Reviewed by: Sabine Schmidt, The global increase in coastal hypoxia over the past decades has resulted from a Centre National de la Recherche Scientifique (CNRS), France considerable rise in anthropogenically-derived nutrient loading. The spatial relationship Antonio Olita, between surface phytoplankton production and subsurface hypoxic zones often can Italian National Research Council (CNR), Italy be explained by considering the oceanographic conditions associated with basin size, *Correspondence: shape, or bathymetry, but that is not the case where nutrient-enriched estuarine Feng Zhou waters merge into complex coastal circulation systems. -
Scientific Assessment of Hypoxia in U.S. Coastal Waters
Scientific Assessment of Hypoxia in U.S. Coastal Waters 0 Dissolved oxygen (mg/L) 6 0 Depth (m) 80 32 Salinity 34 Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health September 2010 This document should be cited as follows: Committee on Environment and Natural Resources. 2010. Scientific Assessment of Hypoxia in U.S. Coastal Waters. Interagency Working Group on Harmful Algal Blooms, Hypoxia, and Human Health of the Joint Subcommittee on Ocean Science and Technology. Washington, DC. Acknowledgements: Many scientists and managers from Federal and state agencies, universities, and research institutions contributed to the knowledge base upon which this assessment depends. Many thanks to all who contributed to this report, and special thanks to John Wickham and Lynn Dancy of NOAA National Centers for Coastal Ocean Science for their editing work. Cover and Sidebar Photos: Background Cover and Sidebar: MODIS satellite image courtesy of the Ocean Biology Processing Group, NASA Goddard Space Flight Center. Cover inset photos from top: 1) CTD rosette, EPA Gulf Ecology Division; 2) CTD profile taken off the Washington coast, project funded by Bonneville Power Administration and NOAA Fisheries; Joseph Fisher, OSU, was chief scientist on the FV Frosti; data were processed and provided by Cheryl Morgan, OSU); 3) Dead fish, Christopher Deacutis, Rhode Island Department of Environmental Management; 4) Shrimp boat, EPA. Council on Environmental Quality Office of Science and Technology Policy Executive Office of the President Dear Partners and Friends in our Ocean and Coastal Community, We are pleased to transmit to you this report, Scientific Assessment ofHypoxia in u.s. -
Is the Gulf of Taranto an Historic Bay?*
Ronzitti: Gulf of Taranto IS THE GULF OF TARANTO AN HISTORIC BAY?* Natalino Ronzitti** I. INTRODUCTION Italy's shores bordering the Ionian Sea, particularly the seg ment joining Cape Spartivento to Cape Santa Maria di Leuca, form a coastline which is deeply indented and cut into. The Gulf of Taranto is the major indentation along the Ionian coast. The line joining the two points of the entrance of the Gulf (Alice Point Cape Santa Maria di Leuca) is approximately sixty nautical miles in length. At its mid-point, the line joining Alice Point to Cape Santa Maria di Leuca is approximately sixty-three nautical miles from the innermost low-water line of the Gulf of Taranto coast. The Gulf of Taranto is a juridical bay because it meets the semi circular test set up by Article 7(2) of the 1958 Geneva Convention on the Territorial Sea and the Contiguous Zone. 1 Indeed, the waters embodied by the Gulf cover an area larger than that of the semi circle whose diameter is the line Alice Point-Cape Santa Maria di Leuca (the line joining the mouth of the Gulf). On April 26, 1977, Italy enacted a Decree causing straight baselines to be drawn along the coastline of the Italian Peninsula.2 A straight baseline, about sixty nautical miles long, was drawn along the entrance of the Gulf of Taranto between Cape Santa Maria di Leuca and Alice Point. The 1977 Decree justified the drawing of such a line by proclaiming the Gulf of Taranto an historic bay.3 The Decree, however, did not specify the grounds upon which the Gulf of Taranto was declared an historic bay.