Bulletin of World Volcanism December 2012
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Stratospheric Aerosol Layer Perturbation Caused by the 2019
Stratospheric aerosol layer perturbation caused by the 2019 Raikoke and Ulawun eruptions and their radiative forcing Corinna Kloss, Gwenaël Berthet, Pasquale Sellitto, Felix Ploeger, Ghassan Taha, Mariam Tidiga, Maxim Eremenko, Adriana Bossolasco, Fabrice Jegou, Jean-Baptiste Renard, et al. To cite this version: Corinna Kloss, Gwenaël Berthet, Pasquale Sellitto, Felix Ploeger, Ghassan Taha, et al.. Stratospheric aerosol layer perturbation caused by the 2019 Raikoke and Ulawun eruptions and their radiative forcing. Atmospheric Chemistry and Physics, European Geosciences Union, 2021, 21 (1), pp.535-560. 10.5194/acp-21-535-2021. hal-03142907 HAL Id: hal-03142907 https://hal.archives-ouvertes.fr/hal-03142907 Submitted on 18 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. Distributed under a Creative Commons Attribution| 4.0 International License Atmos. Chem. Phys., 21, 535–560, 2021 https://doi.org/10.5194/acp-21-535-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Stratospheric aerosol layer -
Geological Survey Professional Paper 1022-C
GEOLOGICAL SURVEY PROFESSIONAL PAPER 1022-C POSTGLACIAL VOLCANIC DEPOSITS ATMOUNTBAKER, WASHINGTON AND POTENTIAL HAZARDS FROM FUTURE ERUPTIONS FRONTISPIECE.- East side of Mount Baker. Boulder Creek, in the center of the photograph, flows into Baker Lake. Postglacial Volcanic Deposits at Mount Baker, Washington, and Potential Hazards from Future Eruptions By JACK H. HYDE and DWIGHT R CRANDELL VOLCANIC ACTIVITY AT MOUNT BAKER, WASHINGTON G E 0 L 0 G I CAL SURVEY P R 0 FE S S I 0 N A L PAPER 1 0 2 2 -C An assessment of potential hazards at Mount Baker is based on the volcano's eruptive behavior during the last 10, 000 years UNITED STATES GOVERNMENT PRINTING OFFICE, \Y ASHINGTON : 1978 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director First Printing 1978 Second Printing 1981 Library of Congress Cataloging in Publication Data Hyde, Jack H. J'()stglacial volcanic deposits at Mount Baker. Washington, and potential hazards from future eruptions. (Volcanic activity at Mount Baker, Washington) Geological Survey Professional Paper 1022-C Bibliography: p. 16 Supt. of Docs. No.: I 19.16:1022-C I. Volcanic ash, tuff, etc.-Washington (State)-Baker, Mount. 2. Volcanism-Washington (State)-Baker, Mount. 3. Volcanic activity prediction. I. Crandell, Dwight Raymond, 1923- joint author. II. Title: Postglacial volcanic deposits at Mount Baker, Washington, and potential hazards from future eruptions. III. Series: IV. Series: United States Geological Survey Professional Paper 1022-C. QE46I.H976 55 1.2'2'09797 77-5891 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. -
Explosive Earth
Natural Hazards Explosive Earth One of the most beautiful pictures taken of the Earth is known as the Blue Marble. Taken from space, it is the epitome of serenity. The Earth really looks like a small marble with swirls of blue, white, green and brown, as it floats placidly in the vastness of space. However, the Volcano Variety picture is misleading, for Mother Earth is geologically restless and Based on history of activity often explodes in acts so violent that we call them, natural hazards. Active: These volcanoes are currently erupting, or exhibiting unrest through earthquakes and/or gas emissions. Natural hazards are defined as, “those Volcano Architecture Dormant: These volcanoes are inactive, but have not been so long elements of the physical environment, harmful A volcano constitutes a vent, a pipe, a enough to be declared extinct. to man and caused by forces extraneous to crater, and a cone. him.” The prefix “natural” shows that these Vent: This is the opening through which Extinct: These volcanoes have been exclude phenomenon that are a result of volcanic material is ejected. A central vent inactive in all of recorded history. human action. An event that causes large underlies the summit crater of the volcano. Based on shape numbers of fatalities and/or tremendous loss It is connected to a magma chamber, of property is a “natural disaster.” which is the main storage area for material Volcanic cone: Volcanic cones are among that is finally ejected. the simplest volcano formations. These are Violent Volcano Pipe: This is a passageway through which built up of ejected material around a volcanic One of the most explosively violent events the ejected magma rises to the surface. -
USGS Open-File Report 2009-1133, V. 1.2, Table 3
Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041 -
World Heritage Volcanoes a Thematic Study
World Heritage Convention IUCN World Heritage Studies 2009 Number 8 World Heritage Volcanoes A Thematic Study IUCN Programme on Protected Areas A Global Review of Volcanic World Heritage Properties: Present Situation, Future Prospects and Management Requirements IUCN, International Union for Conservation of Nature Founded in 1948, IUCN brings together States, government agencies and a diverse range of non-govern- mental organizations in a unique world partnership: over 1000 members in all spread across some 140 countries. As a Union, IUCN seeks to infl uence, encourage and assist societies throughout the world to conserve the integrity and diversity of nature and to ensure that any use of natural resources is equitable and ecologically sustainable. A central Secretariat coordinates the IUCN Programme and serves the Union membership, representing their views on the world stage and providing them with the strategies, services, scientifi c knowl- edge and technical support they need to achieve their goals. Through its six Commissions, IUCN draws together over 10,000 expert volunteers in project teams and ac- tion groups, focusing in particular on species and biodiversity conservation and the management of habitats and natural resources. The Union has helped many countries to prepare National Conservation Strategies, and demonstrates the application of its knowledge through the fi eld projects it supervises. Operations are increasingly decentralized and are carried forward by an expanding network of regional and country offi ces, located principally in developing countries. IUCN builds on the strengths of its members, networks and partners to enhance their capacity and to support global alliances to safeguard natural resources at local, regional and global levels. -
Emulating Volcanic Ash Fall for Multi‑Scale Analysis:Development of The
MANILA Record 2014/36 | GeoCat 81611 Emulating volcanic ash fall for multi-scale analysis: Development of the VAPAHR tool and application to the Asia-Pacific region for the United Nations Global Assessment Report 2015 Bear-Crozier, A. N.1, Miller, V.1, Newey, V.1, Horspool, N.1 and Weber, R.1 APPLYING GEOSCIENCE TO AUSTRALIA’S MOST IMPORTANT CHALLENGES www.ga.gov.au Emulating volcanic ash fall for multi-scale analysis: Development of the VAPAHR tool and application to the Asia- Pacific region for the United Nations Global Assessment Report 2015 GEOSCIENCE AUSTRALIA RECORD 2014/36 Bear-Crozier, A. N.1, Miller, V.1, Newey, V.1, Horspool, N.1 and Weber, R.1 1. Geoscience Australia Department of Industry Minister for Industry: The Hon Ian Macfarlane MP Parliamentary Secretary: The Hon Bob Baldwin MP Secretary: Ms Glenys Beauchamp PSM Geoscience Australia Chief Executive Officer: Dr Chris Pigram This paper is published with the permission of the CEO, Geoscience Australia © Commonwealth of Australia (Geoscience Australia) 2014 With the exception of the Commonwealth Coat of Arms and where otherwise noted, all material in this publication is provided under a Creative Commons Attribution 3.0 Australia Licence. (http://www.creativecommons.org/licenses/by/3.0/au/deed.en) Geoscience Australia has tried to make the information in this product as accurate as possible. However, it does not guarantee that the information is totally accurate or complete. Therefore, you should not solely rely on this information when making a commercial decision. Geoscience Australia is committed to providing web accessible content wherever possible. -
Global Volcanic Earthquake Swarm Database 1979-1989
U- S- Department of the Interior U. S. Geological Survey GLOBAL VOLCANIC EARTHQUAKE SWARM DATABASE 1979-1989 by John P. Benoit1 '2 and Stephen R. McNutt1 '2 Open-File Report 96-69 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, of firm names is for the descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Geophysical Institute at the University of Alaska Fairbanks 903 Koyukuk Dr. P.O. Box 757320 Fairbanks, Alaska 99775-7320 2 Alaska Volcano Observatory 1996 CONTENTS DEVELOPMENT AND DESCRIPTION OF THE GLOBAL VOLCANIC EARTHQUAKE SWARM DATABASE...................................................................................................^^ INTRODUCTION .......................................................................................................................................................A DATABASE STRUCTURE AND D£5c/?/pr/o^...................................................................................................................5 Volcano Table ....................................................................................................................................................6 Earthquake Swarm Table....................................................................................................................................6 Eruption Table ...................................................................................................................................................7 -
Glossary of Volcanic Terms
T N THE highlands of Papua New Guinea there exist widespread .1. legends concerning a ‘Time of Darkness’ in which there was no light and ash fell from the skies. The author investigates these legends and, in conjunction with measurement and analysis of the ash, which covers a large area of the highlands, determines that 300 years ago there was a cataclysmic volcanic eruption on Long Island and that the legends are essentially accurate accounts of this gigantic upheaval that is unrecorded in any written records. There are several unique elements in this book. First, a relatively recent volcanic eruption of very large magnitude is identified. Second this event is shown to have initiated a widespread legend varying from place to place only in detail, and spreading across a number of cultural groups. Third the accuracy of the legends is demonstrated by comparison with known volcanic eruptions. The study shows that legends from an area of almost 100,000 km2 and including more than thirty language groups have survived as essentially accurate accounts for about 300 years. This book will have particular appeal to volcanologists and oral historians and a general appeal to readers with an interest in natural hazards. T N THE highlands of Papua New Guinea there exist widespread .1. legends concerning a ‘Time of Darkness’ in which there was no light and ash fell from the skies. The author investigates these legends and, in conjunction with measurement and analysis of the ash, which covers a large area of the highlands, determines that 300 years ago there was a cataclysmic volcanic eruption on Long Island and that the legends are essentially accurate accounts of this gigantic upheaval that is unrecorded in any written records. -
Geothermal Potential of the Cascade and Aleutian Arcs, with Ranking of Individual Volcanic Centers for Their Potential to Host Electricity-Grade Reservoirs
DE-EE0006725 ATLAS Geosciences Inc FY2016, Final Report, Phase I Final Research Performance Report Federal Agency and Organization: DOE EERE – Geothermal Technologies Program Recipient Organization: ATLAS Geosciences Inc DUNS Number: 078451191 Recipient Address: 3372 Skyline View Dr Reno, NV 89509 Award Number: DE-EE0006725 Project Title: Geothermal Potential of the Cascade and Aleutian Arcs, with Ranking of Individual Volcanic Centers for their Potential to Host Electricity-Grade Reservoirs Project Period: 10/1/14 – 10/31/15 Principal Investigator: Lisa Shevenell President [email protected] 775-240-7323 Report Submitted by: Lisa Shevenell Date of Report Submission: October 16, 2015 Reporting Period: September 1, 2014 through October 15, 2015 Report Frequency: Final Report Project Partners: Cumming Geoscience (William Cumming) – cost share partner GEODE (Glenn Melosh) – cost share partner University of Nevada, Reno (Nick Hinz) – cost share partner Western Washington University (Pete Stelling) – cost share partner DOE Project Team: DOE Contracting Officer – Laura Merrick DOE Project Officer – Eric Hass Project Monitor – Laura Garchar Signature_______________________________ Date____10/16/15_______________ *The Prime Recipient certifies that the information provided in this report is accurate and complete as of the date shown. Any errors or omissions discovered/identified at a later date will be duly reported to the funding agency. Page 1 of 152 DE-EE0006725 ATLAS Geosciences Inc FY2016, Final Report, Phase I Geothermal Potential of -
9 Erupciones Volcánicas
178 Eventos geofísicos 9 ○○○○○○○○○○○○○○○○○○○○○ Erupciones volcánicas PETER J. BAXTER Las pérdidas humanas y económicas por erupciones volcánicas han sido minimizadas por las de las inundaciones, los terremotos y los huracanes, pero el potencial de efectos devastadores de las erupciones volcánicas es tan grande que ahora reciben mayor atención. Los principales factores que contribuyen a los desastres volcánicos incluyen la falta de un mapa preciso de las amenazas volcánicas, los escasos recursos dedicados exclusivamente a la monitorización de los más peligrosos y el veloz y continuo crecimiento de las poblaciones, con el resultado de que cerca de 500 millones de personas vivirán en áreas de actividad volcánica a finales de siglo. Existen cientos de peligrosos y explosivos volcanes y sólo algunos de ellos han sido sujetos de un detallado análisis de riesgos. Para avanzar en los estudios de zonificación de amenazas alrededor de los volcanes, la Década Internacional para la Reducción de los Desastres Naturales de las Naciones Unidas (DIRDN) ha designado algunos de los volcanes más peligrosos en los países desarrollados y en vías de desarrollo como los ‘volcanes de la década’ para estudio especial (1) (tabla 9.1). Factores que afectan la ocurrencia y la severidad de los desastres volcánicos Históricamente, unos 600 volcanes han estado activos en el mundo y 100 o más han sido notorios por la frecuencia o la severidad de sus erupciones en áreas pobladas (2,3). En promedio, cerca de 50 volcanes hacen erupción cada año. La mayoría de los 178 Erupciones -
Volcans Monde SI Dec2010
GEOLOGICAL MAP OF THE WORLD AT 1: 25,000,000 SCALE, THIRD EDITION - Compilator: Philippe Bouysse, 2006 ACTIVE AND RECENT VOLCANOES This list of 1508 volcanoes is taken from data of the Global Volcanism Program run by the Smithsonian Institution (Washington, D.C., USA) and downloaded in April 2006 from the site www.volcano.si.edu/world/summary.cfm?sumpage=num. From the Smithsonian's list, 41 locations have been discarded due to a great deal of uncertainties, particularly as concerns doubtful submarine occurrences (mainly ship reports of the 19th and early 20th centuries). Also have been omitted submarine occurrences from the axes of "normal" oceanic accretionary ridges, i.e. not affected by hotspot activity. NOTES Volcano number: the numbering system was developped by the Catalog of Active Volcanoes of the World in the 1930s and followed on by the Smithsonian Institution, namely in the publication of T. Simkin & L.Siebert: Volcanoes of the World (1994). Name and Geographic situation: some complementary information has been provided concerning a more accurate geographic location of the volcano, e.g. in the case of smaller islands or due to political changes (as for Eritrea). Geographic coordinates: are listed in decimal parts of a degree. The position of volcano no. 104-10 (Tskhouk-Karckar, Armenia) was corrected (Lat. 39°.73 N instead of 35°.73 N). An asterisk (*) in column V.F. indicates the position of the center point of a broad volcanic field. Elevation: in meters, positive or negative for submarine volcanoes. Time frame (column T-FR): this is a Smithsonian' classification for the time of the volcano last known eruption: D1= 1964 or later D2= 1900 – 1963 D3= 1800 – 1899 D4= 1700 – 1799 D5= 1500 – 1699 D6= A.D.1 – 1499 D7= B.C. -
Basaltic-Volcano Systems
Basaltic-volcano systems GEORGE P. L. WALKER Hawaii Center for Volcanology, Department of Geology and Geophysics, School of Ocean and Earth Science and Technology, University of Hawaii, Honolulu, HI 96822, USA Abstract: This review and personal account of basaltic volcanism concentrates on the geological aspects and physical controls, unlike most others which concentrate on geo chemistry. It serves as an update to reviews by Wentworth & Macdonald 20 to 40 years ago. The concept of volcanic systems is developed, a system including the plumbing, intrusions, and other accoutrements of volcanism, as well as the volcanic edifice. Five types of systems are described, namely lava-shield volcanoes, stratovolcanoes, flood-basalt fields, mono genetic-volcano fields, and central volcanoes (having silicic volcanics as well as basaltic). It is postulated that the system-type depends on (a) the magma-input rate and (b) the frequency with which magma-batches enter the system (or modulation frequency). These controls determine whether a hot pathway is maintained from the source to the high-level magma chamber, and hence if eruptions are concentrated in the central-vent system. Reviews are given on many aspects: the different kinds of rift zones that volcanoes exhibit, and their controls; the mostly small intrusions, including coherent-intrusion complexes, that occur in and under the volcanic edifices; the great sill swarms that are an alternative to flood basalts; the origin of the craters and calderas of basaltic volcanoes; high-level magma chambers, their locations, and cumulate prisms; the positive Bouguer gravity anomalies that are attributed to cumulates and intrusion complexes; the structures of basaltic lava flows; the characteristics ofbasaltic explosive volcanism and the consequences ofparticipation by non volcanic water; the products of underwater volcanism; the origin and significance ofjoints, formed either by contraction or expansion, in volcanic rocks; and the distribution ofvesicles in basaltic rocks.