Volcanic Ash Contingency Plan Afi Region
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Historical Volcanism and the State of Stress in the East African Rift System
Wadge, G. , Biggs, J., Lloyd, R., & Kendall, J. M. (2016). Historical volcanism and the state of stress in the East African Rift System. Frontiers in Earth Science, 4, [86]. https://doi.org/10.3389/feart.2016.00086 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.3389/feart.2016.00086 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Frontiers Media at http://journal.frontiersin.org/article/10.3389/feart.2016.00086/full. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ ORIGINAL RESEARCH published: 30 September 2016 doi: 10.3389/feart.2016.00086 Historical Volcanism and the State of Stress in the East African Rift System G. Wadge 1*, J. Biggs 2, R. Lloyd 2 and J.-M. Kendall 2 1 Centre for Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET), Department of Meteorology, University of Reading, Reading, UK, 2 Centre for Observation and Modelling of Earthquakes, Volcanoes and Tectonics (COMET), School of Earth Sciences, University of Bristol, Bristol, UK Crustal extension at the East African Rift System (EARS) should, as a tectonic ideal, involve a stress field in which the direction of minimum horizontal stress is perpendicular to the rift. -
Historical Volcanism and the State of Stress in the East African Rift System
Historical volcanism and the state of stress in the East African Rift System Article Accepted Version Open Access Wadge, G., Biggs, J., Lloyd, R. and Kendall, J.-M. (2016) Historical volcanism and the state of stress in the East African Rift System. Frontiers in Earth Science, 4. 86. ISSN 2296- 6463 doi: https://doi.org/10.3389/feart.2016.00086 Available at http://centaur.reading.ac.uk/66786/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . To link to this article DOI: http://dx.doi.org/10.3389/feart.2016.00086 Publisher: Frontiers media All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online 1 Historical volcanism and the state of stress in the East African 2 Rift System 3 4 5 G. Wadge1*, J. Biggs2, R. Lloyd2, J-M. Kendall2 6 7 8 1.COMET, Department of Meteorology, University of Reading, Reading, UK 9 2.COMET, School of Earth Sciences, University of Bristol, Bristol, UK 10 11 * [email protected] 12 13 14 Keywords: crustal stress, historical eruptions, East African Rift, oblique motion, 15 eruption dynamics 16 17 18 19 20 21 Abstract 22 23 Crustal extension at the East African Rift System (EARS) should, as a tectonic ideal, 24 involve a stress field in which the direction of minimum horizontal stress is 25 perpendicular to the rift. -
ETHIOPIA - National Hot Spot Map 31 May 2010
ETHIOPIA - National Hot Spot Map 31 May 2010 R Legend Eritrea E Tigray R egion !ª D 450 ho uses burned do wn d ue to th e re ce nt International Boundary !ª !ª Ahferom Sudan Tahtay Erob fire incid ent in Keft a hum era woreda. I nhabitan ts Laelay Ahferom !ª Regional Boundary > Mereb Leke " !ª S are repo rted to be lef t out o f sh elter; UNI CEF !ª Adiyabo Adiyabo Gulomekeda W W W 7 Dalul E !Ò Laelay togethe r w ith the regiona l g ove rnm ent is Zonal Boundary North Western A Kafta Humera Maychew Eastern !ª sup portin g the victim s with provision o f wate r Measle Cas es Woreda Boundary Central and oth er imm ediate n eeds Measles co ntinues to b e re ported > Western Berahle with new four cases in Arada Zone 2 Lakes WBN BN Tsel emt !A !ª A! Sub-city,Ad dis Ababa ; and one Addi Arekay> W b Afa r Region N b Afdera Military Operation BeyedaB Ab Ala ! case in Ahfe rom woreda, Tig ray > > bb The re a re d isplaced pe ople from fo ur A Debark > > b o N W b B N Abergele Erebtoi B N W Southern keb eles of Mille and also five kebeles B N Janam ora Moegale Bidu Dabat Wag HiomraW B of Da llol woreda s (400 0 persons) a ff ected Hot Spot Areas AWD C ases N N N > N > B B W Sahl a B W > B N W Raya A zebo due to flo oding from Awash rive r an d ru n Since t he beg in nin g of th e year, Wegera B N No Data/No Humanitarian Concern > Ziquala Sekota B a total of 967 cases of AWD w ith East bb BN > Teru > off fro m Tigray highlands, respective ly. -
Modelling the Current Fractional Cover of an Invasive Alien Plant and Drivers of Its Invasion in a Dryland Ecosystem
www.nature.com/scientificreports OPEN Modelling the current fractional cover of an invasive alien plant and drivers of its invasion in a dryland Received: 23 July 2018 Accepted: 23 November 2018 ecosystem Published: xx xx xxxx Hailu Shiferaw1,3, Urs Schafner 2, Woldeamlak Bewket3, Tena Alamirew1, Gete Zeleke1, Demel Teketay4 & Sandra Eckert5 The development of spatially diferentiated management strategies against invasive alien plant species requires a detailed understanding of their current distribution and of the level of invasion across the invaded range. The objectives of this study were to estimate the current fractional cover gradient of invasive trees of the genus Prosopis in the Afar Region, Ethiopia, and to identify drivers of its invasion. We used seventeen explanatory variables describing Landsat 8 image refectance, topography, climate and landscape structures to model the current cover of Prosopis across the invaded range using the random forest (RF) algorithm. Validation of the RF algorithm confrmed high model performance with an accuracy of 92% and a Kappa-coefcient of 0.8. We found that, within 35 years after its introduction, Prosopis has invaded approximately 1.17 million ha at diferent cover levels in the Afar Region (12.3% of the surface). Normalized diference vegetation index (NDVI) and elevation showed the highest explanatory power among the 17 variables, in terms of both the invader’s overall distribution as well as areas with high cover. Villages and linear landscape structures (rivers and roads) were found to be more important drivers of future Prosopis invasion than environmental variables, such as climate and topography, suggesting that Prosopis is likely to continue spreading and increasing in abundance in the case study area if left uncontrolled. -
Examining Alternative Livelihoods for Improved Resilience and Transformation in Afar
EXAMINING ALTERNATIVE LIVELIHOODS FOR IMPROVED RESILIENCE AND TRANSFORMATION IN AFAR May 2019 Report photos: Dr. Daniel Temesgen EXAMINING ALTERNATIVE LIVELIHOODS FOR IMPROVED RESILIENCE AND TRANSFORMATION IN AFAR May 2019 This document has been produced with the financial assistance of the European Union. The views expressed herein can in no way be taken to reflect the official opinion of the European Union. Report authors: Daniel Temesga, Amdissa Teshome, Berhanu Admassu Suggested citation: FAO and Tufts University. (2019). Examining Alternative Livelihoods for Improved Resilience and Transformation in Afar. FAO: Addis Ababa, Ethiopia. Implemented by: Feinstein International Center Friedman School of Nutrition Science and Policy Tufts University Africa Regional Office www.fic.tufts.edu © FAO TABLE OF CONTENTS EXECUTIVE SUMMARY ............................................................................................................................... 6 I. BACKGROUND............................................................................................................................................ 8 The Afar Region: context and livelihoods ................................................................................................... 8 The purpose of the study ............................................................................................................................ 8 The study’s approaches and methods ......................................................................................................... -
Evaporites Reveal Pleistocene Basin Dynamics in the Danakil Depression (Northern Afar, Ethiopia)
Evaporites reveal Pleistocene basin dynamics in the Danakil depression (northern Afar, Ethiopia) Valentin Rime1,*, A. Foubert1, R. Fentimen1, H. Negga1, A. El Korh1, T. Adatte2, I. Hajdas3, B. Atnafu4 & T. Kidane5 1 Department of Geosciences, University of Fribourg, Ch. Du Musée 6, Fribourg, Switzerland. 2 Faculty of Geosciences and Environment, University of Lausanne, Switzerland 2 Department of Physics, ETH Zürich, Switzerland 4 School of Earth Sciences, Addis Ababa University, Ethiopia. 5 School of Agricultural, Earth and Environmental Sciences, University of KwaZulu-Natal Durban, South Africa. * [email protected] Welcome! Welcome to my COVID-type presentation! • If you like to know the summary of this study, jump to the next slide. • If you are only interested in the results, jump to page 8. • If you are only interested in the discussion, jump to page 12. • If you are only interested in the conclusion, jump to page 22. Don’t hesitate to comment, ask questions, or make any suggestions to this study! Highlights • Multiproxy study of a drillcore in the Danakil depression, Afar, Ethiopia. • More than 600m of sediments dominated by evaporites most probably formed during the last 130ka. • Formation by evaporation of seawater after flooding of the depression and by remobilization through meteoric water inflow. • High sedimentation rates, important subsidence and rapid extensional tectonics. • Probably the most Recent analogue of Past Salt Giants. Fig. 1: Lithostratigraphic log of the core record Introduction: Geological setting (1) The Danakil depression (Afar, Ethiopia) is a rift valley forming the southernmost part of the Red Sea rift. It is situated between the Ethiopian plateau and the Danakil block and Fig. -
11 HS 000 ETH 013013 A4.Pdf (English)
ETHIOPIA:Humanitarian Concern Areas Map (as of 04 February 2013) Eritrea > !ª !ª> Note: The following newly created woreda boundaries are not Tahtay !ª E available in the geo-database; hence not represented in this Nutrition Hotspot Priority Laelay Erob R R !ª Adiyabo Mereb Ahferom !ª Tahtay Gulomekeda !ª I E map regardless of their nutrition hot spot priority 1 & 2: Adiyabo Leke T D Adiyabo Adwa Saesie Dalul Priority one Asgede Tahtay R S Kafta Werei Tsaedaemba E E Priority 1: Dawa Sarar (Bale zone), Goro Dola (Guji zone), Abichu Tsimbila Maychew !ª A Humera Leke Hawzen Berahle A Niya( North Showa zone) and Burka Dintu (West Hararge Priority two > T I GR AY > Koneba Central Berahle zone) of Oromia region, Mekoy (Nuer zone) of Gambella Western Naeder Kola Ke>lete Awelallo Priority three Tselemti Adet Temben region, Kersadula and Raso (Afder zone), Ararso, Birkod, Tanqua > Enderta !ª Daror and Yo'ale (Degahabour zone), Kubi (Fik zone), Addi Tselemt Zone 2 No Priority given Arekay Abergele Southern Ab Ala Afdera Mersin (Korahe zone), Dhekasuftu and Mubarek (Liben Beyeda Saharti Erebti Debark Hintalo !ª zone), Hadigala (Shinille zone) and Daratole (Warder Abergele Samre > Megale Erebti Bidu Wejirat zone) of Somali region. Dabat Janamora > Bidu International Boundary Alaje Raya North Lay Sahla Azebo > Wegera Endamehoni > > Priority 2: Saba Boru (Guji zone) of Oromia region and Ber'ano Regional Boundary Gonder Armacho Ziquala > A FA R !ª East Sekota Raya Yalo Teru (Gode zone) and Tulu Guled (Jijiga zone) of Somali region. Ofla Kurri Belesa -
ELRP-Integrated Pest Management Plan – IPMP-Component 1 1
Page | ELRP-Integrated Pest Management Plan – IPMP-Component 1 1 TABLE OF CONTENTS EXECUTIVE SUMMARY .............................................................................................. 6 1 INTRODUCTION................................................................................................... 20 1.1 Emergency Locust Response Program ............................................................... 20 1.2 Project Development Objective ......................................................................... 20 1.3 ELRP Project Components ................................................................................ 20 1.4 Selected Pesticides ............................................................................................. 21 1.5 Project Activities ................................................................................................ 22 1.6 Project Beneficiaries .......................................................................................... 23 1.7 Aims and Objectives of IPMP ............................................................................ 23 1.8 Component 1 Implementation Arrangements .................................................... 24 2 STAKEHOLDER ENGAGEMENT ..................................................................... 25 2.1 Stakeholder Identification .................................................................................. 25 2.2 Stakeholder Engagement .................................................................................... 25 2.3 IPMP Disclosure -
Working Paper Or Information Paper
APIRG/19 WP/14 Appendix 3.2J INTERNATIONAL CIVIL AVIATION ORGANIZATION VOLCANIC ASH CONTINGENCY PLAN AFI REGION First Edition - October 2012 THIS DOCUMENT IS ISSUED BY THE DAKAR AND NAIROBI ICAO REGIONAL OFFICES UNDER THE AUTHORITY OF THE APIRG 1 Page 2 of 32 Volcanic Ash Contingency Plan – AFI Region FOREWARD Within and adjacent to the Africa and Indian Ocean (AFI) Region there are areas of volcanic activities which are likely to affect flight in the AFI Region. The major volcanoes in the region are located in the following States: Algeria, Cameroon, Cape Verde Islands, Chad, Comoros Island, Democratic Republic of Congo, Djibouti, Eritrea, Ethiopia, France (Reunion Island), Kenya, Madagascar, Mali, Niger, Nigeria, Rwanda, Sao Tome and Principe, Spain (Canary Islands, Madeira), Sudan, Tanzania and Uganda. The names of the concerned volcano are listed in APPENDIX K (source: Smithsonian Institution). This document is the AFI Air Traffic Management (ATM) Volcanic Ash Contingency Plan which sets out standardised guidelines and procedures for the provision of information to airlines and en-route aircraft before and during a volcanic eruption. Volcanic contamination, of which volcanic ash is the most serious, is a hazard for safe flight operations. Mitigating the hazards posed by volcanic ash in the atmosphere and/or at the aerodrome cannot be resolved in isolation but through collaborative decision-making (CDM) involving all stakeholders concerned. During an eruption volcanic contamination can reach and exceed the cruising altitudes of turbine-powered -
An Outline of the East African Rift Volcanism
2053-38 Advanced Workshop on Evaluating, Monitoring and Communicating Volcanic and Seismic Hazards in East Africa 17 - 28 August 2009 An outline of the East African Rift Volcanism Yirgu Gezahegn Addis Ababa University Ethiopia Advanced Workshop on Evaluating, Monitoring andCommunicating Volcanic and Seismic Hazards in East Africa An outline of the East African Rift volcanism Gezahegn Yirgu, PhD Addis Ababa University 1. Introduction The East African Rift System (EARS) is a more than 3000 km long system of depressions flanked by broad uplifted plateaus. A long record of volcanism in EARS provides invaluable constraints on past and present processes, as well as the various depth levels of magma generation and storage. In this presentation, I outline volcanic processes along the length of the EARS from pre-rift setting through rift initiation to continental breakup. The volcanic evolution of the EARS reveals consistent patterns in the distribution, volume, compositions and sources of volcanic products allowing its subdivision into volcanic provinces. EARS extends from the Red Sea in the north to Mozambique and beyond. The system is characterized by regional topographic uplift, the Ethiopian dome, the Kenyan dome. The principal rift sectors include the Ethiopian, Eastern and Western rift valleys. The Ethiopian and Kenyan branches of the rift are the site of substantially greater volcanism than is observed at the Western rift. Figure 1 Digital Elevation Model of the East African rift System. Black lines are main faults 2. Volcanic Provinces -
Influence of Regional Tectonics and Pre-Existing Structures on the Formation of Elliptical Calderas in the Kenyan Rift
Downloaded from http://sp.lyellcollection.org/ by guest on September 23, 2021 Influence of regional tectonics and pre-existing structures on the formation of elliptical calderas in the Kenyan Rift E. A. M. ROBERTSON1*, J. BIGGS1, K. V. CASHMAN1, M. A. FLOYD2 & C. VYE-BROWN3 1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 2JN, UK 2Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA, USA 3British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK *Corresponding author (e-mail: [email protected]) Abstract: Calderas are formed by the collapse of large magma reservoirs and are commonly ellip- tical in map view. The orientation of elliptical calderas is often used as an indicator of the local stress regime; but, in some rift settings, pre-existing structural trends may also influence the orien- tation. We investigated whether either of these two mechanisms controls the orientation of calderas in the Kenyan Rift. Satellite-based mapping was used to identify the rift border faults, intra-rift faults and orientation of the calderas to measure the stress orientations and pre-existing structural trends and to determine the extensional regime at each volcano. We found that extension in north- ern Kenya is orthogonal, whereas that in southern Kenya is oblique. Elliptical calderas in northern Kenya are orientated NW–SE, aligned with pre-existing structures and perpendicular to recent rift faults. In southern Kenya, the calderas are aligned NE–SW and lie oblique to recent rift faults, but are aligned with pre-existing structures. -
World Bank Document
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Page | ELRP-Integrated Pest Management Plan – IPMP-Component 1 1 TABLE OF CONTENTS EXECUTIVE SUMMARY .............................................................................................. 6 1 INTRODUCTION................................................................................................... 20 1.1 Emergency Locust Response Program ............................................................... 20 1.2 Project Development Objective ......................................................................... 20 1.3 ELRP Project Components ................................................................................ 20 1.4 Selected Pesticides ............................................................................................. 21 1.5 Project Activities ................................................................................................ 22 1.6 Project Beneficiaries .......................................................................................... 23 1.7 Aims and Objectives of IPMP ............................................................................ 23 1.8 Component 1 Implementation Arrangements .................................................... 24 2 STAKEHOLDER ENGAGEMENT ..................................................................... 25 2.1 Stakeholder Identification .................................................................................. 25 2.2 Stakeholder