Selective Retreat Scenarios for the Po River Delta
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
XXIII COARSE ANGLING European Championship
XXIII COARSE ANGLING European CHAMpIONSHIP CAVANELLA PO – MAY 20 and 21 2017 Welcome, dear angler friends, I am delighted to express on my name and on behalf of the Italian Sport Fishing and Underwater Activities Federation (FIPSAS), the best greetings to all participants at this Coarse Angling European Championships that this year is going to take place from May 20th until 21th 2017, in a charming area of Veneto Region, along the “Canalbianco” bank. I am sure that all attending athletes, who will join Rovigo as well as all managers, judges and stewards will find a way to explore and appreciate our beauties and taste Veneto people’s hospitality and of all those who have made all efforts for the organization of this sport fishing important event. I am particularly delighted to express my warmest welcoming to all in the aim to live together some happy days in the name of sport. A special “good luck” to all Judges convened to manage this race, in the certainty of their professional and fair commitment they have also expressed in precedent occasions. Finally, I wish to thank the organizing Committee and his President, the local authorities and all journalists for their support and contribution for this event’s good success. The FIPSAS President Prof. Ugo Claudio Matteoli OFFICIAL PROGRAMME From: Sunday 14 May 2017 (arrival of teams) To: Monday 22 May 2017 (departure of teams) INFORMATION ABOUT LOREO CITY This city is located in the “Basso Polesine” between the Adige and the Po river. A series of little streets leading into “Piazza Longhena”, which preserves its ancient appearance next to the Cathedral (1658), rich of many artworks. -
PESHTIGO RIVER DELTA Property Owner
NORTHEAST - 10 PESHTIGO RIVER DELTA WETLAND TYPES Drew Feldkirchner Floodplain forest, lowland hardwood, swamp, sedge meadow, marsh, shrub carr ECOLOGY & SIGNIFICANCE supports cordgrass, marsh fern, sensitive fern, northern tickseed sunflower, spotted joe-pye weed, orange This Wetland Gem site comprises a very large coastal • jewelweed, turtlehead, marsh cinquefoil, blue skullcap wetland complex along the northwest shore of Green Bay and marsh bellflower. Shrub carr habitat is dominated three miles southeast of the city of Peshtigo. The wetland by slender willow; other shrub species include alder, complex extends upstream along the Peshtigo River for MARINETTE COUNTY red osier dogwood and white meadowsweet. Floodplain two miles from its mouth. This site is significant because forest habitats are dominated by silver maple and green of its size, the diversity of wetland community types ash. Wetlands of the Peshtigo River Delta support several present, and the overall good condition of the vegetation. - rare plant species including few-flowered spikerush, The complexity of the site – including abandoned oxbow variegated horsetail and northern wild raisin. lakes and a series of sloughs and lagoons within the river delta – offers excellent habitat for waterfowl. A number This Wetland Gem provides extensive, diverse and high of rare animals and plants have been documented using quality wetland habitat for many species of waterfowl, these wetlands. The area supports a variety of recreational herons, gulls, terns and shorebirds and is an important uses, such as hunting, fishing, trapping and boating. The staging, nesting and stopover site for many migratory Peshtigo River Delta has been described as the most birds. Rare and interesting bird species documented at diverse and least disturbed wetland complex on the west the site include red-shouldered hawk, black tern, yellow shore of Green Bay. -
A Synthesis of Information I
Outer Continental Shelf Environmental Assessment Program * A Synthesis of Information I U.S. DEPARTMENT OF COMMERCE U.S. DEPARTMENT OF THE INTEXIOR National Oceanic and Atmospheric Administration Minerals Management Service National Ocean Service Alaska OCS Region Office of Oceanography and Marine Assessment . .:.% y! Ocean Assessments Division ' t. CU ' k Alaska Office OCS Study, MMS 89-0081 . '.'Y. 4 3 --- NOTICES This report has been prepared as part of the U.S. Department bf Commerce, National Oceanic and Atmospheric Administration's Outer Continental Shelf Environmental Assessment Program, and approved for publication. The inter- pretation of data and opinions expressed in this document are those of the authors. Approval does not necessarily signify that the contents reflect the views and policies of the Department of Commerce or those of the Department of the Interior. The National Oceanic and Atmospheric Administration (NOAA) does not approve, recommend, or endorse any proprietary material mentioned in this publication. No reference shall be made to NOAA or to this publication in any advertising or sales promotion which would indicate or imply that NOAA approves, recommends, or endorses any proprietary product or proprietary material mentioned herein, or which has as its purpose or intent to cause directly or indirectly the advertised product to be used or purchased because of this publication. Cover: LandsatTMimage of the Yukon Delta taken on Julg 22, 1975, showing the thamal gradients resulting from Yukon River discharge. In this image land is dqicted in sesof red indicating warmer temperatures versus the dark blues (colder temperatures) of Bering Sea waters. Yukon River water, cooh than the surround- ing land but wanner than marine waters, is represented bg a light aqua blue. -
European Commission
14.7.2020 EN Offi cial Jour nal of the European Union C 231/7 V (Announcements) OTHER ACTS EUROPEAN COMMISSION Publication of the amended single document following the approval of a minor amendment pursuant to the second subparagraph of Article 53(2) of Regulation (EU) No 1151/2012 (2020/C 231/03) The European Commission has approved this minor amendment in accordance with the third subparagraph of Article 6(2) of Commission Delegated Regulation (EU) No 664/2014 (1). The application for approval of this minor amendment can be consulted in the Commission’s eAmbrosia database. SINGLE DOCUMENT ‘Radicchio di Chioggia’ EU No: PGI-IT-0484-AM01 – 5.12.2019 PDO () PGI (X) 1. Name(s) ‘Radicchio di Chioggia’ 2. Member State or third country Italy 3. Description of the agricultural product or foodstuff 3.1. Type of product Class 1.6. Fruit, vegetables and cereals, fresh or processed 3.2. Description of the product to which the name in (1) applies The ‘Radicchio di Chioggia’ PGI is reserved for products obtained from plants belonging to the Asteracee family, Cichorium genus, inthybus species, silvestre variety. ‘Radicchio di Chioggia’ comes in two types: ‘early’ and ‘late’. The plant has roundish, closely interlaced leaves forming a characteristic spherical head. The leaves are red to deep red in colour with white central veins. The distinctive characteristics of the two types are: — ‘early’: closed head, weighing between 200 and 600 grams, with characteristic scarlet to amaranth-coloured, crispy leaves, with a sweet to slightly bitter taste, — ‘late’: very compact head, weighing between 200 and 600 grams, with deep amaranth-coloured, fairly crispy leaves, with a bitter taste. -
Analyzing Trends of Dike-Ponds Between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China
sustainability Article Analyzing Trends of Dike-Ponds between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China Fengshou Li 1, Kai Liu 1,* , Huanli Tang 2, Lin Liu 3,4,* and Hongxing Liu 4,5 1 Guangdong Key Laboratory for Urbanization and Geo-simulation, Guangdong Provincial Engineering Research Center for Public Security and Disaster, School of Geography and Planning, Sun Yat-Sen University, Guangzhou 510275, China; [email protected] 2 Guangzhou Zengcheng District Urban and Rural Planning and Surveying and Mapping Geographic Information Institute, Guangzhou 511300, China; [email protected] 3 Center of Geo-Informatics for Public Security, School of Geographic Sciences, Guangzhou University, Guangzhou 510006, China 4 Department of Geography and Geographic Information Science, University of Cincinnati, Cincinnati, OH 45221, USA; [email protected] 5 Department of Geography, the University of Alabama, Tuscaloosa, AL 35487, USA * Correspondence: [email protected] (K.L.); [email protected] (L.L.); Tel.: +86-020-8411-3044 (K.L.); +1-513-556-3429 (L.L.); Fax: +86-020-8411-3057 (K.L. & L.L.) Received: 27 August 2018; Accepted: 26 September 2018; Published: 30 September 2018 Abstract: Dike-ponds have experienced significant changes in the Pearl River Delta region over the past several decades, especially since China’s economic reform, which has seriously affected the construction of ecological environments. In order to monitor the evolution of dike-ponds, in this study we use multi-source remote sensing images from 1978 to 2016 to extract dike-ponds in several periods using the nearest neighbor classification method. -
Dispersal of Larval Suckers at the Williamson River Delta, Upper Klamath Lake, Oregon, 2006–09
Prepared in cooperation with the Bureau of Reclamation Dispersal of Larval Suckers at the Williamson River Delta, Upper Klamath Lake, Oregon, 2006–09 Scientific Investigations Report 2012–5016 U.S. Department of the Interior U.S. Geological Survey Cover: Inset: Larval sucker from Upper Klamath Lake, Oregon. (Photograph taken by Allison Estergard, Student, Oregon State University, Corvallis, Oregon, 2011.) Top: Photograph taken from the air of the flooded Williamson River Delta, Upper Klamath Lake, Oregon. (Photograph taken by Charles Erdman, Fisheries Technician, Williamson River Delta Preserve, Klamath Falls, Oregon, 2008.) Bottom left: Photograph of a pop net used by The Nature Conservancy to collect larval suckers in Upper Klamath Lake and the Williamson River Delta, Oregon. (Photograph taken by Heather Hendrixson, Director, Williamson River Delta Preserve, Klamath Falls, Oregon, 2006.) Bottom middle: Photograph of a larval trawl used by Oregon State University to collect larval suckers in Upper Klamath Lake and the Williamson River Delta, Oregon. (Photograph taken by David Simon, Senior Faculty Research Assistant, Oregon State University, Corvallis, Oregon, 2010.) Bottom right: Photograph of a plankton net used by the U.S. Geological Survey to collect larval suckers in Upper Klamath Lake and the Williamson River Delta, Oregon. (Photographer unknown, Klamath Falls, Oregon, 2009.) Dispersal of Larval Suckers at the Williamson River Delta, Upper Klamath Lake, Oregon, 2006–09 By Tamara M. Wood, U.S. Geological Survey, Heather A. Hendrixson, The Nature Conservancy, Douglas F. Markle, Oregon State University, Charles S. Erdman, The Nature Conservancy, Summer M. Burdick, U.S. Geological Survey, Craig M. Ellsworth, U.S. Geological Survey, and Norman L. -
Losses of Salt Marsh in China: Trends, Threats and Management
Losses of salt marsh in China: Trends, threats and management Item Type Article Authors Gu, Jiali; Luo, Min; Zhang, Xiujuan; Christakos, George; Agusti, Susana; Duarte, Carlos M.; Wu, Jiaping Citation Gu J, Luo M, Zhang X, Christakos G, Agusti S, et al. (2018) Losses of salt marsh in China: Trends, threats and management. Estuarine, Coastal and Shelf Science 214: 98–109. Available: http://dx.doi.org/10.1016/j.ecss.2018.09.015. Eprint version Post-print DOI 10.1016/j.ecss.2018.09.015 Publisher Elsevier BV Journal Estuarine, Coastal and Shelf Science Rights NOTICE: this is the author’s version of a work that was accepted for publication in Estuarine, Coastal and Shelf Science. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Estuarine, Coastal and Shelf Science, [, , (2018-09-18)] DOI: 10.1016/j.ecss.2018.09.015 . © 2018. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http:// creativecommons.org/licenses/by-nc-nd/4.0/ Download date 09/10/2021 17:12:34 Link to Item http://hdl.handle.net/10754/628759 Accepted Manuscript Losses of salt marsh in China: Trends, threats and management Jiali Gu, Min Luo, Xiujuan Zhang, George Christakos, Susana Agusti, Carlos M. Duarte, Jiaping Wu PII: S0272-7714(18)30220-8 DOI: 10.1016/j.ecss.2018.09.015 Reference: YECSS 5973 To appear in: Estuarine, Coastal and Shelf Science Received Date: 15 March 2018 Revised Date: 21 August 2018 Accepted Date: 14 September 2018 Please cite this article as: Gu, J., Luo, M., Zhang, X., Christakos, G., Agusti, S., Duarte, C.M., Wu, J., Losses of salt marsh in China: Trends, threats and management, Estuarine, Coastal and Shelf Science (2018), doi: https://doi.org/10.1016/j.ecss.2018.09.015. -
“Major World Deltas: a Perspective from Space
“MAJOR WORLD DELTAS: A PERSPECTIVE FROM SPACE” James M. Coleman Oscar K. Huh Coastal Studies Institute Louisiana State University Baton Rouge, LA TABLE OF CONTENTS Page INTRODUCTION……………………………………………………………………4 Major River Systems and their Subsystem Components……………………..4 Drainage Basin………………………………………………………..7 Alluvial Valley………………………………………………………15 Receiving Basin……………………………………………………..15 Delta Plain…………………………………………………………...22 Deltaic Process-Form Variability: A Brief Summary……………………….29 The Drainage Basin and The Discharge Regime…………………....29 Nearshore Marine Energy Climate And Discharge Effectiveness…..29 River-Mouth Process-Form Variability……………………………..36 DELTA DESCRIPTIONS…………………………………………………………..37 Amu Darya River System………………………………………………...…45 Baram River System………………………………………………………...49 Burdekin River System……………………………………………………...53 Chao Phraya River System……………………………………….…………57 Colville River System………………………………………………….……62 Danube River System…………………………………………………….…66 Dneiper River System………………………………………………….……74 Ebro River System……………………………………………………..……77 Fly River System………………………………………………………...…..79 Ganges-Brahmaputra River System…………………………………………83 Girjalva River System…………………………………………………….…91 Krishna-Godavari River System…………………………………………… 94 Huang He River System………………………………………………..……99 Indus River System…………………………………………………………105 Irrawaddy River System……………………………………………………113 Klang River System……………………………………………………...…117 Lena River System……………………………………………………….…121 MacKenzie River System………………………………………………..…126 Magdelena River System……………………………………………..….…130 -
Science Focus: Dead Zones
SCIENCE FOCUS: DEAD ZONES Creeping Dead Zones This is not the title of a sequel to a Stephen King novel. "Dead zones" in this context are areas where the bottom water (the water at the sea floor) is anoxic — meaning that it has very low (or completely zero) concentrations of dissolved oxygen. These dead zones are occurring in many areas along the coasts of major continents, and they are spreading over larger areas of the sea floor. Because very few organisms can tolerate the lack of oxygen in these areas, they can destroy the habitat in which numerous organisms make their home. The cause of anoxic bottom waters is fairly simple: the organic matter produced by phytoplankton at the surface of the ocean (in the euphotic zone) sinks to the bottom (the benthic zone), where it is subject to breakdown by the action of bacteria, a process known as bacterial respiration. The problem is, while phytoplankton use carbon dioxide and produce oxygen during photosynthesis, bacteria use oxygen and give off carbon dioxide during respiration. The oxygen used by bacteria is the oxygen dissolved in the water, and that’s the same oxygen that all of the other oxygen-respiring animals on the bottom (crabs, clams, shrimp, and a host of mud-loving creatures) and swimming in the water (zooplankton, fish) require for life to continue. The "creeping dead zones" are areas in the ocean where it appears that phytoplankton productivity has been enhanced, or natural water flow has been restricted, leading to increasing bottom water anoxia. If phytoplankton productivity is enhanced, more organic matter is produced, more organic matter sinks to the bottom and is respired by bacteria, and thus more oxygen is consumed. -
The Zambezi River Delta Mangrove Carbon Project: a Pilot Baseline Assessment for REDD+ Reporting and Monitoring
The Zambezi River Delta Mangrove Carbon Project: A Pilot Baseline Assessment for REDD+ Reporting and Monitoring Final Report Prepared by: Christina E. Stringer, Ph. D. Carl C. Trettin, Ph. D. Center for Forested Wetlands Research U.S. Forest Service Stanley J. Zarnoch, Ph. D. Southern Research Station U.S. Forest Service Wenwu Tang, Ph. D. Department of Geography and Earth Sciences University of North Carolina- Charlotte In Collaboration With: World Wildlife Fund - Mozambique: Denise Nicolau, Rito Mabunda Universidade de Eduardo Mondlane: Salomão Bandeira, Celia Macamo National Aeronautics and Space Administration: Temilola Fatoyinbo, Marc Simard U.S. Forest Service: Jason Ko Mozambique Ministry of Agriculture: Joaquím Macuacua 1 September, 2014 Final Report (1 September 2014) Page 1 i. Forward This report summarizes the findings of the Zambezi River Delta Mangrove Carbon Project. Compact discs containing supporting materials, documents, and data will be provided to WWF- Mozambique, the Ministry of Agriculture, Dept. of Natural Resources Inventory, and Universidade de Eduardo Mondlane, Dept. of Biology, and they will also be made available at the Center for Forested Wetlands Research website (http://www.srs.fs.usda.gov/charleston/) in early 2015. ii. Acknowledgements This work was made possible by US AID support to the USFS under the US AID Mozambique Global Climate Change Sustainable Landscape Program, in collaboration with the Natural Resource Assessment Department of the Government of Mozambique. Denise Nicolau, Itelvino Cunat, and Rito Mabunda provided invaluable logistical support during the planning and implementation of field missions. Celia Macamo and Salamão Bandeira assisted prior to, and during field work, with identification of mangrove and other plant species. -
Comune Di Badia Polesine
COMUNE DI BADIA POLESINE REGOLAMENTO COMUNALE PER LA DIFESA DELL’ASSETTO IDRAULICO DEL TERRITORIO (Approvato con Delibera di Consiglio Comunale n. 34 del 13.11.2008) Comune di Comune di Regolamento per la difesa Badia Polesine dell’assetto idraulico del territorio SOMMARIO ART. 1 – FINALITA’ ............................................................................................................................. 3 ART. 2 – DEFINIZIONE ....................................................................................................................... 3 ART. 3 – UBICAZIONE DI SIEPI, ALBERATURE ED ESSENZE VEGETALI ARBUSTIVE, OBBLIGHI E DIVIETI.......................................................................................................................... 3 ART. 4 – PULIZIA DI FOSSI E SCOLI .............................................................................................. 4 ART. 5 – DISTANZE DI LAVORAZIONI AGRICOLE DAI FOSSI .............................................. 5 ART. 6 – COMPITI DEI PROPRIETARI O DETENTORI DEL FONDO FRONTISTA............. 5 ART. 7 – TOMBINATURA IN ZONA AGRICOLA .......................................................................... 6 ART. 8 – URBANIZZAZIONE DI AREE............................................................................................ 7 ART. 9 – SANZIONI .............................................................................................................................. 8 ART. 10 – ATTUAZIONE DEL REGOLAMENTO.......................................................................... -
Badia Polesine 1855. Storia Di Una Calunnia Del Sangue Nell'italia Dell
UNIVERSITÀ DEGLI STUDI DI UDINE CORSO DI DOTTORATO DI RICERCA IN STORIA: CULTURA E STRUTTURE DELLE AREE DI FRONTIERA CICLO XXVIII TESI DI DOTTORATO DI RICERCA Badia Polesine 1855. Storia di una calunnia del sangue nell’Italia dell’Ottocento DOTTORANDO Dott. Emanuele D’Antonio RELATORE Ch.ma Prof.ssa Maddalena Del Bianco Cotrozzi ANNO ACCADEMICO 2015/2016 1 2 Indice Indice delle abbreviazioni p. 5 Introduzione p. 6 Capitolo primo. La costruzione del caso di Badia. Comunità, istituzioni e omicidio rituale in una cittadina polesana a metà Ottocento p. 17 1. Introduzione p. 17 2. Caliman Ravenna, Giuditta Castilliero e la società badiese p. 20 3. Il sangue di Giuditta. L’accusa del sangue nella comunità cittadina p. 29 4. La calunnia del sangue alla conquista della cittadina. Comunità, istituzioni e antisemitismo p. 43 5. L’arresto dell’ebreo assassino p. 58 Capitolo secondo. Il crollo della calunnia del sangue. Aspetti istituzionali, politici e sociali p. 73 1. Introduzione p. 73 2. La caccia agli ebrei assassini. Omicidio rituale, potere giudiziario e polizia fra il Polesine e le Province venete p. 76 3. L’omicidio rituale diventa un affare di Stato. Potere politico, istituzioni amministrative e Comunità ebraiche nel Veneto della terza dominazione austriaca p. 83 4. La normalizzazione del caso. Politica, istituzioni, società p. 99 3 Capitolo terzo. La calunnia del sangue e l’opinione pubblica. Fra politica e cultura p. 120 1. Introduzione p. 120 2. La sfida della propaganda. L’Annotatore friulano e il caso di Badia p. 125 3. La legittimazione del mito dell’omicidio rituale.