March 27, 1964 Regional Effects
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CMI Cook Inlet Surface Current Mapping Final Report
OCS Study MMS 2006-032 Final Report CODAR in Alaska Principal Investigator: Dave Musgrave, PhD Associate Professor School of Fisheries and Ocean Sciences University of Alaska Fairbanks P.O. Box 757220 Fairbanks, AK 99775-7220 (907) 474-7837 [email protected] CoAuthor: Hank Statscewich, MS School of Fisheries and Ocean Sciences University of Alaska Fairbanks P.O. Box 757220 Fairbanks, AK 99775-7220 (907) 474-5720 [email protected] June 2006 Contact information e-mail: [email protected] phone: 907.474.1811 fax: 907.474.1188 postal: Coastal Marine Institute School of Fisheries and Ocean Sciences P.O. Box 757220 University of Alaska Fairbanks Fairbanks, AK 99775-7220 ii Table of Contents List of Tables ................................................................................................................................. iv List of figures................................................................................................................................. iv Abstract........................................................................................................................................... v Introduction..................................................................................................................................... 1 Methods........................................................................................................................................... 2 Results............................................................................................................................................ -
Nos Cook Inlet Operational Forecast System: Model Development and Hindcast Skill Assessment
NOAA Technical Report NOS CS 40 NOS COOK INLET OPERATIONAL FORECAST SYSTEM: MODEL DEVELOPMENT AND HINDCAST SKILL ASSESSMENT Silver Spring, Maryland September 2020 noaa National Oceanic and Atmospheric Administration U.S. DEPARTMENT OF COMMERCE National Ocean Service Coast Survey Development Laboratory Office of Coast Survey National Ocean Service National Oceanic and Atmospheric Administration U.S. Department of Commerce The Office of Coast Survey (OCS) is the Nation’s only official chartmaker. As the oldest United States scientific organization, dating from 1807, this office has a long history. Today it promotes safe navigation by managing the National Oceanic and Atmospheric Administration’s (NOAA) nautical chart and oceanographic data collection and information programs. There are four components of OCS: The Coast Survey Development Laboratory develops new and efficient techniques to accomplish Coast Survey missions and to produce new and improved products and services for the maritime community and other coastal users. The Marine Chart Division acquires marine navigational data to construct and maintain nautical charts, Coast Pilots, and related marine products for the United States. The Hydrographic Surveys Division directs programs for ship and shore-based hydrographic survey units and conducts general hydrographic survey operations. The Navigational Services Division is the focal point for Coast Survey customer service activities, concentrating predominately on charting issues, fast-response hydrographic surveys, and Coast Pilot -
Identifying N Rite Ria and Establishing Pakameters
IDENTIFYING N RITE RIA AND ESTABLISHING imperative that only those areas which are suitable for ecolourism be developed arid erlsure that ecotourism criteria are matched PAKAMETERS FOR FOREST-BASED with the resource base characteristics of the region. This paper describes a methodology to identify sites based on determining fist the criteria and attributes of ecotourism and second by ECOTOUKISM LN NORTHERN ONTARIO, matching the value range of these criteria to the region's resource base inventory. The problems in defining ecotourism and identi- CANADA I fying the linkages between ecotourism and other forms of tourism and related environmental management concepts are discussed in Stephen W. Boyd the contcxt of explaining the difficulty in identifying appropriate ecotourism criteria. Next the elements of ccolourism, suitable to ~~nsultant/DoctoralCandidate, The University of Western Northern Ontario. are presented along with the criteria and the Ontario, Department of Geography, Social Science Building, methodology. A final section addresses the implications of the Inndon, Ontario, Canada, N6A 5C2 methodology to resourw: managers and tourism operators. Richard W. Butler Definition and Linkages Ecotourism is a form of tourism which has been fraught with Professor, The University of Westem Ontario, Department of problems of definition. There is no unifying and generally Geography, Social Science Building, London, Ontario, Canada, accepted definition and many terms have been used to describe N6A 5C2 the same phenomenon. Examples include terms like nature travel (Laarman and Durst 1987), nature-oriented tourism (Durst and Wolfgang IIaider Ingram 1988) and special interest tourism (Inskeep 1987; Weiler and Hall 1992). Scace et al. (1992) identify over thirty-five terms Social Research Scientist, Center for Northern Forest Ecosystem that may be linked to ecotourism, such as sustainable tourism and Research, OMNR, 955 Oliver Road, Thunder Bay, Ontario, alternative tourism. -
The Peninsula of Fear: Chronicle of Occupation and Violation of Human Rights in Crimea
THE PENINSULA OF FEAR: CHRONICLE OF OCCUPATION AND VIOLATION OF HUMAN RIGHTS IN CRIMEA Kyiv 2016 УДК 341.223.1+342.7.03](477.75)’’2014/2016’’=111 ББК 67.9(4Укр-6Крм)412 Composite authors: Sergiy Zayets (Regional Center for Human Rights), Olexandra Matviychuk (Center for Civil Liberties), Tetiana Pechonchyk (Human Rights Information Center), Darya Svyrydova (Ukrainian Helsinki Human Rights Union), Olga Skrypnyk (Crimean Human Rights Group). The publication contains photographs from public sources, o7 cial websites of the state authorities of Ukraine, the Russian Federation and the occupation authorities, Crimean Field Mission for Human Rights, Crimean Human Rights Group, the online edition Crimea.Realities / Radio Svoboda and other media, court cases materials. ‘The Peninsula of Fear : Chronicle of Occupation and Violation of Human Rights in Crimea’ / Under the general editorship of O. Skrypnyk and T. Pechonchyk. Second edition, revised and corrected. – Kyiv: KBC, 2016. – 136 p. ISBN 978-966-2403-11-4 This publication presents a summary of factual documentation of international law violation emanating from the occupation of the autonomous Republic of Crimea and the city of Sevastopol (Ukraine) by the Russian Federation military forces as well as of the human rights violations during February 2014 – February 2016. The publication is intended for the representatives of human rights organizations, civil activists, diplomatic missions, state authorities, as well as educational and research institutions. УДК 341.223.1+342.7.03](477.75)’’2014/2016’’=111 ББК 67.9(4Укр-6Крм)412 ISBN 978-966-2403-11-4 © S. Zayets, O. Matviychuk, T. Pechonchyk, D. Svyrydova, O. Skrypnyk, 2016 Contents Introduction. -
Discovery of a Multispecies Shark Aggregation and Parturition Area in the Ba Estuary, Fiji Islands
Received: 4 October 2017 | Revised: 15 April 2018 | Accepted: 22 April 2018 DOI: 10.1002/ece3.4230 ORIGINAL RESEARCH Discovery of a multispecies shark aggregation and parturition area in the Ba Estuary, Fiji Islands Tom Vierus1,2 | Stefan Gehrig2,3 | Juerg M. Brunnschweiler4 | Kerstin Glaus1 | Martin Zimmer2,5 | Amandine D. Marie1 | Ciro Rico1,6 1School of Marine Studies, Faculty of Science, Technology and Environment, The Abstract University of the South Pacific, Laucala, Population declines in shark species have been reported on local and global scales, Suva, Fiji with overfishing, habitat destruction and climate change posing severe threats. The 2Leibniz Centre for Tropical Marine Research (ZMT), Bremen, Germany lack of species- specific baseline data on ecology and distribution of many sharks, 3Department of Biosciences, University of however, makes conservation measures challenging. Here, we present a fisheries- Exeter, Penryn Campus, UK independent shark survey from the Fiji Islands, where scientific knowledge on locally 4Independent Researcher, Zurich, Switzerland occurring elasmobranchs is largely still lacking despite the location’s role as a shark 5Faculty of Biology/Chemistry, University of hotspot in the Pacific. Juvenile shark abundance in the fishing grounds of the Ba Bremen, Bremen, Germany Estuary (north- western Viti Levu) was assessed with a gillnet- and longline- based 6 Department of Wetland Ecology, Estación survey from December 2015 to April 2016. A total of 103 juvenile sharks identified Biológica de Doñana, Consejo Superior de Investigaciones Científicas (EBD, CSIC), as blacktip Carcharhinus limbatus (n = 57), scalloped hammerhead Sphyrna lewini Sevilla, Spain (n = 35), and great hammerhead Sphyrna mokarran (n = 11) sharks were captured, Correspondence tagged, and released. -
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska
Geology of the Prince William Sound and Kenai Peninsula Region, Alaska Including the Kenai, Seldovia, Seward, Blying Sound, Cordova, and Middleton Island 1:250,000-scale quadrangles By Frederic H. Wilson and Chad P. Hults Pamphlet to accompany Scientific Investigations Map 3110 View looking east down Harriman Fiord at Serpentine Glacier and Mount Gilbert. (photograph by M.L. Miller) 2012 U.S. Department of the Interior U.S. Geological Survey Contents Abstract ..........................................................................................................................................................1 Introduction ....................................................................................................................................................1 Geographic, Physiographic, and Geologic Framework ..........................................................................1 Description of Map Units .............................................................................................................................3 Unconsolidated deposits ....................................................................................................................3 Surficial deposits ........................................................................................................................3 Rock Units West of the Border Ranges Fault System ....................................................................5 Bedded rocks ...............................................................................................................................5 -
On the Movement of Beluga Whales in Cook Inlet, Alaska
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Old Dominion University Old Dominion University ODU Digital Commons CCPO Publications Center for Coastal Physical Oceanography 12-2008 On the Movement of Beluga Whales in Cook Inlet, Alaska: Simulations of Tidal and Environmental Impacts Using a Hydrodynamic Inundation Model Tal Ezer Old Dominion University, [email protected] Roderick Hobbs Lie-Yauw Oey Follow this and additional works at: https://digitalcommons.odu.edu/ccpo_pubs Part of the Environmental Indicators and Impact Assessment Commons, Environmental Monitoring Commons, Marine Biology Commons, and the Oceanography Commons Repository Citation Ezer, Tal; Hobbs, Roderick; and Oey, Lie-Yauw, "On the Movement of Beluga Whales in Cook Inlet, Alaska: Simulations of Tidal and Environmental Impacts Using a Hydrodynamic Inundation Model" (2008). CCPO Publications. 117. https://digitalcommons.odu.edu/ccpo_pubs/117 Original Publication Citation Ezer, T., Hobbs, R., & Oey, L.Y. (2008). On the movement of beluga whales in Cook Inlet, Alaska: Simulations of tidal and environmental impacts using a hydrodynamic inundation model. Oceanography, 21(4), 186-195. doi: 10.5670/oceanog.2008.17 This Article is brought to you for free and open access by the Center for Coastal Physical Oceanography at ODU Digital Commons. It has been accepted for inclusion in CCPO Publications by an authorized administrator of ODU Digital Commons. For more information, please contact [email protected]. or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] ofor Th e The to: [email protected] Oceanography approval Oceanography correspondence POall Box 1931, portionthe Send Society. -
Alaska M7.0 Earthquake Response
2018 M7.0 Anchorage, Alaska, Earthquake RESPONSE Date and Time: November 30, 2018, 8:29:29 am Location: N 61.323°, W 149.923° (7 miles north of Anchorage) Area of Effect: Strong to very strong shaking felt from northern Kenai Peninsula to Matanuska-Susitna Valley; light to moderate shaking felt throughout southcentral and interior Alaska. Initial earthquake followed 6 minutes later by M5.7 aftershock. Fatalities: 0 Damage: Power outages and gas leaks; damage to roads, railroads, and buildings; and closures of schools, businesses, and government offices throughout Anchorage bowl and Mat-Su Valley. Tsunami: Tsunami warnings were sent out within minutes of the earthquake. No tsunami waves Lateral spreading disrupted Vine Road near Wasilla. Many reported. failures of engineered materials occurred on or adjacent to water-saturated lowlands. (Photo credit: U.S. Geological Survey) Alaska Seismic Hazard Safety Commission Alaska Earthquake Center 2018 Cook Inlet Earthquake 1 Points to Ponder Proximity matters The Anchorage earthquake occurred 7 miles north of Anchorage and caused extensive damage, while the 2002 M7.9 Denali earthquake, which occurred about 170 miles north of Anchorage, caused no damage in the area. Anchorage population is approximately 325,00, Mat-Su 104,000 & Kenai Borough 50,000= 479,000 Entire state population is 710,000 Earthquake-resilient construction saves lives The population affected by the Anchorage earthquake generally reside in structures built in accordance with seismic building codes or using construction techniques that are resistant to earthquake shaking, and no lives were lost. Areas where codes were not enforced saw higher damage as a result Infrastructure is vulnerable to earthquake damage Construction codes for roads and embankments are not as successful as building codes for structures. -
Greenhouse Effect and Sea Level Rise: the Cost of Holding Back the Sea
Originally in Coastal Management, Volume 19, pp. 171-204 (1991) Greenhouse Effect and Sea Level Rise: The Cost of Holding Back the Sea JAMES G.TITUS Office of Policy Analysis U.S. Environmental Protection Agency Washington, DC 20460 RICHARD A. PARK School of Public and Environmental Affairs Indiana University Bloomington, IN 47405 STEPHEN P. LEATHERMAN Department of Geography University of Maryland College Park, MD 20742 J. RICHARD WEGGEL Department of Civil and Architectural Engineering Drexel University Philadelphia, PA 19104 MICHAEL S. GREENE The Bruce Company Washington, DC 20024 PAUL W. MAUSEL Department of Geography and Geology Indiana State University Terre Haute, IN 47809 SCOTT BROWN JCA Associates Mt. Laurel, NJ 08054 GARY GAUNT Science Applications International Corporation Mclean, VA 22102 MANJIT TREHAN Indiana University and Purdue University at Indianapolis Indianapolis, IN 46202 GARY YOHE Department of Economics Wesleyan University Middletown, CT 06457 1 Greenhouse Effect and Sea Level Rise: The Cost of Holding Back the Sea Abstract: Previous studies suggest that the expected global warming from the greenhouse effect could raise sea level 50 to 200 centimeters (2 to 7 feet) in the next century. This article presents the first nationwide assessment of the primary impacts of such a rise on the United States: (1) the cost of protecting ocean resort communities by pumping sand onto beaches and gradually raising barrier islands in place; (2) the cost of protecting developed areas along sheltered waters through the use of levees (dikes) and bulkheads; and (3) the loss of coastal wetlands and undeveloped lowlands. The total cost for a one-meter rise would be $270-475 billion, ignoring future development. -
The 1964 Prince William Sound Earthquake Subduction Zone Steven C
Adv. Geophys. ms. Last saved: 2/12/2003 6:lO:OO PM 1 Crustal Deformation in Southcentral Alaska: The 1964 Prince William Sound Earthquake Subduction Zone Steven C. Cohen Geodynamics Branch, Goddard Space Flight Center, Greenbelt, MD 2077 1 email: Steven.C.Cohen @ .nasa.gov; phone: 301-6 14-6466 Jeffrey T. Freymueller Geophysical Institute, University of Alaska, Fairbanks, AK 99775 Outline: 1. Introduction 2. Tectonic, Geologic, and Seismologic Setting 3. Observed Crustal Motion 3.1 Coseismic Crustal Motion 3.2 Preseismic and Interseismic (pre-1964) Crustal Motion 3.3 Postseismic and Interseismic (post-1964) Crustal Motion 4. Models of Southcentral Alaska Preseismic and Postseismic Crustal Deformation 5. Conclusions 6. References Adv. Geophys. ms. Last saved: a1 a2003 6:lO:OO PM 2 1. Introduction The M, = 9.2 Prince William Sound (PWS) that struck southcentral Alaska on March 28, 1964, is one of the important earthquakes in history. The importance of this Great Alaska Earthquake lies more in its scientific than societal impact. While the human losses in the PWS earthquake were certainly tragic, the sociological impact of the earthquake was less than that of is earthquakes that have struck heavily populated locales. By contrast Earth science, particularly tectonophysics, seismology, and geodesy, has benefited enormously from studies of this massive earthquake. The early 1960s was a particularly important time for both seismology and tectonophysics. Seismic instrumentation and analysis techniques were undergoing considerable modernization. For example, the VELA UNIFORM program for nuclear test detection resulted in the deployment of the World Wide Standard Seismographic Network in the late 1950s and early 1960s (Lay and Wallace, 1995). -
Transgressive Systems Tract of a Ria-Type Estuary: the Late Holocene Vilaine River Drowned Valley (France)
Marine Geology 337 (2013) 140–155 Contents lists available at SciVerse ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Transgressive systems tract of a ria-type estuary: The Late Holocene Vilaine River drowned valley (France) C. Traini a,⁎, D. Menier a,b, J.-N. Proust c, P. Sorrel d a Geoarchitecture EA2219, Géosciences Marine & Géomorphologie Littorale, Université de Bretagne Sud, rue Yves Mainguy, 56017 Vannes cedex, France b Universiti Teknologi PETRONAS Tronoh, Perak, Malaysia c UMR CNRS 6118 Géosciences, Université Européenne de Bretagne, Campus de Beaulieu, 35000 Rennes, France d UMR CNRS 5276 LGL-TPE (Laboratoire de Géologie de Lyon: Terre, Planètes, Environnements), Université Claude Bernard–Lyon 1/ENS Lyon, 27-43 bd du 11 Novembre, 69622 Villeurbanne cedex, France article info abstract Article history: The understanding of control parameters of estuarine-infilling at different scales in time and space is impor- Received 24 April 2012 tant for near-future projections and better management of these areas facing sea-level change. During the Received in revised form 18 February 2013 last 20 years, the stratigraphy of late Quaternary estuaries has been extensively investigated leading to the Accepted 19 February 2013 development of depositional models which describe the sedimentary facies distribution according to changes Available online 4 March 2013 in sea level, tidal range and wave activity but few of them describe in detail the influence of the estuarine Communicated by J.T. Wells geomorphology. On the Atlantic coast, recent studies provide a detailed understanding of the sedimentary infill succession of incised valleys during the late Holocene transgression with recent emphasis on the Keywords: macrotidal bay of the Vilaine River in South Brittany. -
Geographical Views on Education for Sustainable Development Proceedings
GEOGRAPHIEDIDAKTISCHE FORSCHUNGEN Herausgegeben im Auftrag des Hochschulverbandes für Geographie und ihre Didaktik e.V. von Hartwig Haubrich Jürgen Nebel Yvonne Schleicher Helmut Schrettenbrunner Volume 42 Sibylle Reinfried, Yvonne Schleicher, Armin Rempfler (Editors) Geographical Views on Education for Sustainable Development Proceedings Lucerne-Symposium, Switzerland July 29-31, 2007 International Geographical Union Commission on Geographical Education Co-organized by the Teacher Training University of Central Switzerland Lucerne ISBN 978-3-925319-29-7 © 2007 Selbstverlag des Hochschulverbandes für Geographie und ihre Didaktik e.V. (HGD) Orders/Bestellungen an: [email protected] Printing/Druck: Schnelldruck-Süd Nürnberg Layout: Carolin Banthleon, Weingarten 2 Acknowledgements ………………………………………...…………………………..7 Sponsors …………………………………………….……………………………………...8 Preface …………………………………………………………………...……...………….9 Sibylle Reinfried (Lucerne), Yvonne Schleicher (Weingarten), Armin Rempfler (Lucerne) Keynote Papers Cultural Evolution And The Concept Of Sustainable Development: From Global To Local Scale And Back…………………………………...…….…………11 Peter Baccini (Zurich) Geography Education For Sustainable Development…………………………...………...27 Hartwig Haubrich (Freiburg) The Alps In Geographical Education And Research…………………………...…………39 Paul Messerli (Berne) Refereed Papers Symposium Session: Outdoor Education and ESD Places Of Sustainability In Cities: An Outdoor-Teaching Approach……………………40 André Odermatt (Zurich), Katja Brundiers (Zurich) Children’s Awareness