Urbanisation and Natural Disaster: Systematic Review

Total Page:16

File Type:pdf, Size:1020Kb

Urbanisation and Natural Disaster: Systematic Review URBANISATION AND NATURAL DISASTER – A SYSTEMATIC REVIEW NOVEMBER 2017 The authors of this report are: 1. Shahed Hossain (icddr,b) 2. Kim Spurway (UNSW) 3. Anthony B. Zwi (UNSW) 4. Nafisa Lira Huq (icddr,b) 5. Razib Mamun (icddr,b) 6. Rubana Islam (icddr,b) 7. Iffat Nowrin (icddr,b) 8. Saraban Ether (icddr,b) 9. Jacqui Bonnitcha (Independent consultant) 10. Ngamindra Dahal (SIAS) 11. Alayne M. Adams (icddr,b) Funding This is an independent report commissioned under the DFID Systematic Review Programme for South Asia. This material has been funded by South Asia Research Hub, Research and Evidence Division, Government of UK. The views expressed do not necessarily reflect the UK Government’s official policies. Acknowledgments We would like to express our thanks and acknowledge the support of Professor Sandy Oliver and colleagues (Dr Mukdarut Bangpan; Claire Stansfield; Jeff Brunton) at EPPI-Centre, Department of Social Science, UCL Institute of Education, UK, Hari Dhungana and Kamal Devkota from SIAS, Hemant Ojha, Krishna Shrestha and Nahid Sultana (NS) from UNSW, Professor Shariful Islam (BSSMU, Bangladesh) for advice and feedback. We also thank PricewaterhouseCoopers Private Limited (PwC, India) for managing the DFID Systematic Review Programme for South Asia. Conflicts of interest There were no conflicts of interest in the writing of this report. Contributions The opinions expressed in this publication are not necessarily those of SARH-DFID, the EPPI- Centre or PwC. Responsibility for the views expressed remains solely with the authors. i Citation Hossain S, Spurway K, Zwi A.B., Huq N.L., Mamun R, Islam R, Nowrin I, Ether S, Bonnitcha J, Dahal N and Adams A.M. (2017) What is the impact of urbanisation on risk of, and vulnerability to, natural disasters? What are the effective approaches for reducing exposure of urban population to disaster risks? London: EPPI-Centre, Social Science Research Unit, UCL Institute of Education, University College London. Picture Source: https://www.flickr.com/photos/dfid/ © Copyright Authors of the systematic reviews on the EPPI-Centre website (http://eppi.ioe.ac.uk/) hold the copyright for their reviews. The authors give permission for users of the review to display and print the contents of the review for their own non-commercial use, provided that the materials are not modified, copyright and other proprietary notices contained in the materials are retained, and the source of the material is cited clearly, following the citation details provided. Otherwise, users are not permitted to duplicate, reproduce, republish, distribute, or store the review without written permission. ii CONTENTS List of Figures ................................................................................. iv List of abbreviations .......................................................................... v Summary ........................................................................................ 1 1. Background ................................................................................. 9 2. Methods .................................................................................... 19 3. Findings of the review .................................................................. 25 4. Policy and Practice Implications ...................................................... 58 5. Discussion and Recommendation ..................................................... 60 6. Strengths and limitations of the review ............................................. 70 7. Conclusions ............................................................................... 72 8. References ................................................................................ 73 9. APPENDICES ............................................................................... 84 iii LIST OF FIGURES Figure 1: Comparison of urban and rural population growth ............................ 9 Figure 2: Conceptual Framework ................................................................... 17 Figure 3: Proposed Theory of Change ........................................................... 18 Figure 4: Flow chart of study selection process ............................................. 26 Figure 5: Distribution of included literature on natural disasters sites in South and East Asia ................................................................................................. 27 iv LIST OF ABBREVIATIONS ACCRA African Climate Change Resilience Alliance ADB Asian Development Bank ADPC Asian Disaster Preparedness Centre ALNAP Active Learning Network for Accountability and Performance CBDRM Community-Based Disaster Risk Management CBRMA Community-Based Risk Management Arrangements CBDRR Community-Based Disaster Risk Reduction CCA Climate Change Adaptation CECI Centre for International Studies and Cooperation CENESTA Centre for Sustainable Development, Iran DFID Department for International Development (UK) DRR Disaster Risk Reduction DRM Disaster Risk Management FAO Food and Agriculture Organization of the United Nations GFDRR Global Facility for Disaster Reduction and Recovery HFA Hyogo Framework for Action icddr,b International Centre for Diarrhoeal Disease Research, Bangladesh ICIMOD International Centre for Integrated Mountain Development IFRC International Federation of Red Cross and Red Crescent Societies IPCC Intergovernmental Panel on Climate Change LMIC Low and Middle Income Countries MFI Microfinance Institution NGO Non-Governmental Organisation SAARC South Asian Association for Regional Cooperation SIAS South Asia Institute of Advanced Studies v UNDP United Nations Development Programme UNFCCC United Nations Framework Convention on Climate Change UNSW The University of New South Wales, Australia UNICEF United Nations Children’s Fund UNISDR United Nations International Strategy for Disaster Reduction vi SUMMARY In recent decades the rate and extent of urbanisation has increased markedly and the majority of the world’s people now live in urban areas. These trends are clearly apparent in low and middle income countries, particularly those in South and East Asia (World Bank recent list of LMIC by region). Much of this urban growth is relatively unplanned and has increased the vulnerability of the urban population to the increasing risk of natural disasters and extreme weather events. In addition, vulnerability is further aggravated by other risk factors such as widespread poverty and illiteracy, population migration, increased population density, poor access to services, inadequate nutrition, and poor water and sanitation. Major gaps exist in information on the interface between urbanisation and natural disasters, especially if the added dimensions of risk, vulnerability and resilience are considered. The concept that the impact of disasters is an outcome of ongoing risk processes interacting with hazards, exposure and vulnerabilities is comparatively recent. It is suggested that there are valuable lessons to be learnt from local level initiatives, people’s participation or adaptation of suitable and applicable legislations in the face of such hazards and disasters happening in these cities, countries and regions. RESEARCH QUESTIONS This review aimed to answer two key questions: i. What is the impact of urbanisation on risk of, and vulnerability to, natural disasters? ii. What are the effective approaches for reducing exposure of urban populations to disaster risks? The review aimed to understand the complex relationship between urbanisation, natural disaster, risk and vulnerability. The project approach was based on the concept that risk arises at the interface of four intersecting domains: urbanisation, natural disasters, vulnerability and risk reduction. This was supplemented by a more detailed proposed framework (Theory of Change) capturing the relationships and influences among these dynamic issues and their impacts on risk, vulnerability and resilience. METHODOLOGY A two stage review was undertaken: 1. Stage 1 mapped the range, extent and diversity of literature on these issues. 2. Stage 2 was based on the emergent findings from Stage 1 and sought to examine in more depth the impact and the interrelation of urbanisation with natural disasters with a particular emphasis on the availability of evidence of effective interventions. The findings were further strengthened by a more in-depth analysis of a subset of studies graded as high to medium quality study identified in the Stage 2 review. The Stage 1 scoping review examined 363 studies after primary screening and focused on urban and peri-urban populations from low and middle income countries, all types of natural disaster, along with evidence of any programmes and interventions implemented by governments, NGOs, international organisations or donor agencies. The Stage 2 review synthesized evidence from 32 studies identified from the Stage 1 scoping review focused on the relationships between variables of interest (risk and vulnerability), including the analysis of outcomes and impact of interventions. This helped in documenting the range of risk mitigation approaches that have been described and contributed to deriving lessons concerning their applicability to different contexts, especially those in South and East Asia. The Stage 2 review focused on all disaster types in South and East Asia LMIC countries. All included studies for Stage 2 review were coded according to pre-defined (identified in the proposed theory of change) and emerging codes. The included qualitative and descriptive studies
Recommended publications
  • And Potential Seismic Hazards Within the Southern Tarim Basin
    Kinematics of active deformation across the Western Kunlun mountain range (Xinjiang, China), and potential seismic hazards within the southern Tarim Basin. Christelle Guilbaud, Martine Simoes, Laurie Barrier, Amandine Laborde, Jerome van der Woerd, Haibing Li, Paul Tapponnier, Thomas Coudroy, Andrew Murray To cite this version: Christelle Guilbaud, Martine Simoes, Laurie Barrier, Amandine Laborde, Jerome van der Woerd, et al.. Kinematics of active deformation across the Western Kunlun mountain range (Xinjiang, China), and potential seismic hazards within the southern Tarim Basin.. Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2017, 122 (12), pp.10,398-10,426. 10.1002/2017JB014069. hal-01668711 HAL Id: hal-01668711 https://hal.archives-ouvertes.fr/hal-01668711 Submitted on 21 Aug 2020 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. PUBLICATIONS Journal of Geophysical Research: Solid Earth RESEARCH ARTICLE Kinematics of Active Deformation Across the Western Kunlun 10.1002/2017JB014069 Mountain Range (Xinjiang, China) and
    [Show full text]
  • Intraplate Earthquakes in North China
    5 Intraplate earthquakes in North China mian liu, hui wang, jiyang ye, and cheng jia Abstract North China, or geologically the North China Block (NCB), is one of the most active intracontinental seismic regions in the world. More than 100 large (M > 6) earthquakes have occurred here since 23 BC, including the 1556 Huax- ian earthquake (M 8.3), the deadliest one in human history with a death toll of 830,000, and the 1976 Tangshan earthquake (M 7.8) which killed 250,000 people. The cause of active crustal deformation and earthquakes in North China remains uncertain. The NCB is part of the Archean Sino-Korean craton; ther- mal rejuvenation of the craton during the Mesozoic and early Cenozoic caused widespread extension and volcanism in the eastern part of the NCB. Today, this region is characterized by a thin lithosphere, low seismic velocity in the upper mantle, and a low and flat topography. The western part of the NCB consists of the Ordos Plateau, a relic of the craton with a thick lithosphere and little inter- nal deformation and seismicity, and the surrounding rift zones of concentrated earthquakes. The spatial pattern of the present-day crustal strain rates based on GPS data is comparable to that of the total seismic moment release over the past 2,000 years, but the comparison breaks down when using shorter time windows for seismic moment release. The Chinese catalog shows long-distance roaming of large earthquakes between widespread fault systems, such that no M ࣙ 7.0 events ruptured twice on the same fault segment during the past 2,000 years.
    [Show full text]
  • SMIP13 Seminar Proceedings OBSERVATIONS from the APRIL 20, 2013 LUSHAN COUNTY, YA'an CITY, SICHUAN PROVINCE, CHINA EARTHQUAKE
    SMIP13 Seminar Proceedings OBSERVATIONS FROM THE APRIL 20, 2013 LUSHAN COUNTY, YA’AN CITY, SICHUAN PROVINCE, CHINA EARTHQUAKE Marshall Lew AMEC Environment & Infrastructure, Inc. Los Angeles, California Abstract The April 20, 2013 Lushan earthquake followed the 2008 Great Wenchuan earthquake by almost five years. Although the rupture also started in the Longmenshan fault zone, the Lushan earthquake is not an aftershock. Although similar damage and disruptions to infrastructure and society occurred, it was of a smaller scale and not unexpected due to the short time for the lessons from Wenchuan to be applied. There were some examples of lessons learned and the strong motion dataset obtained in this event will prove valuable in assessing how effective the actions taken have been. The visual observations were made on May 27 and 28, 2013 in Lushan. Introduction On April 20, 2013, at 8:02 am (Beijing Time), an earthquake occurred in Lushan County of Ya’an City in Sichuan Province in southwestern China. The epicenter was located at 30o 17’ 02” N and 102o 57’ 22” E, about 120 km from the major city of Chengdu; see Figure 1. Ya’an City is a prefecture level city in the western part of Sichuan Province and has a population of about 1.5 million people and is the location of one of China’s main centers for the protection of the endangered giant panda. Sichuan Province is known as the “Province of Abundance.” The province is a leading agricultural region of China and the province is also very rich in mineral resources, including large natural gas reserves.
    [Show full text]
  • Distribution Pattern of Landslides Triggered by the 2014
    International Journal of Geo-Information Article Distribution Pattern of Landslides Triggered by the 2014 Ludian Earthquake of China: Implications for Regional Threshold Topography and the Seismogenic Fault Identification Suhua Zhou 1,2, Guangqi Chen 1 and Ligang Fang 2,* 1 Department of Civil and Structural Engineering, Kyushu University, Fukuoka 819-0395, Japan; [email protected] (S.Z.); [email protected] (G.C.) 2 Department of Geotechnical Engineering, Central South University, Changsha 410075, China * Correspondance: [email protected]; Tel.: +86-731-8253-9756 Academic Editor: Wolfgang Kainz Received: 16 February 2016; Accepted: 11 March 2016; Published: 30 March 2016 Abstract: The 3 August 2014 Ludian earthquake with a moment magnitude scale (Mw) of 6.1 induced widespread landslides in the Ludian County and its vicinity. This paper presents a preliminary analysis of the distribution patterns and characteristics of these co-seismic landslides. In total, 1826 landslides with a total area of 19.12 km2 triggered by the 3 August 2014 Ludian earthquake were visually interpreted using high-resolution aerial photos and Landsat-8 images. The sizes of the landslides were, in general, much smaller than those triggered by the 2008 Wenchuan earthquake. The main types of landslides were rock falls and shallow, disrupted landslides from steep slopes. These landslides were unevenly distributed within the study area and concentrated within an elliptical area with a 25-km NW–SE striking long axis and a 15-km NW–SE striking short axis. Three indexes including landslides number (LN), landslide area ratio (LAR), and landslide density (LD) were employed to analyze the relation between the landslide distribution and several factors, including lithology, elevation, slope, aspect, distance to epicenter and distance to the active fault.
    [Show full text]
  • Fault Behavior and Lower Crustal Rheology Inferred from the First Seven Years of Postseismic GPS Data After the 2008 Wenchuan Earthquake
    Originally published as: Diao, F., Wang, R., Wang, Y., Xiong, X., Walter, T. R. (2018): Fault behavior and lower crustal rheology inferred from the first seven years of postseismic GPS data after the 2008 Wenchuan earthquake. - Earth and Planetary Science Letters, 495, pp. 202—212. DOI: http://doi.org/10.1016/j.epsl.2018.05.020 Manuscript to be submitted to EPSL 1 Fault behaviour and lower crustal rheology inferred from the first seven years of 2 postseismic GPS data after the 2008 Wenchuan earthquake 3 4 Faqi Diaoa, Rongjiang Wangb*, Yuebing Wangc, Xiong Xionga and Thomas R. Walterb 5 a. Institute of Geophysics and Geomatics, China University of Geosciences, Wuhan 430074, 6 China 7 b. GFZ German Research Centre for Geosciences, Telegrafenberg, D-14473 Potsdam, 8 Germany 9 c. National Earthquake Infrastructure Service, Beijing 100045, China 10 *Corresponding author: Rongjiang Wang ([email protected]) 11 12 Abstract 13 Long-term and wide-area geodetic observations may allow identifying distinct postseismic 14 deformation processes following large earthquakes, and thus can reveal fault behaviour 15 and permit quantifying complexities in lithospheric rheology. In this paper, the first 7 16 years of GPS (Global Positioning System) displacement data following the 2008 Mw7.9 17 Wenchuan earthquake are used to study the relevant mechanisms of postseismic 18 deformation. Two simple models that consider either afterslip or viscoelastic relaxation as 19 the unitary mechanism of the postseismic deformation are tested at first. After analysing 20 the limitations and complementarity of these two separated models, a combined model 21 incorporating the two main mechanisms is presented.
    [Show full text]
  • 1 Seismic Velocity Reduction and Accelerated Recovery Due to Earthquakes on the Longmenshan Fault
    1 Seismic velocity reduction and accelerated recovery due to earthquakes on the Longmenshan fault 2 Shunping Pei1,2, Fenglin Niu3,4, Yehuda Ben-Zion5, Quan Sun2, Yanbing Liu2, Xiaotian Xue2, Jinrong Su6, 3 Zhigang Shao7 4 1CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences (CAS), 5 Beijing 100101, China 6 2 CAS Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, 7 Chinese Academy of Sciences(CAS), Beijing 100101, China 8 3State Key Laboratory of petroleum Resource and Prospecting, and Unconventional Gas Institute, China 9 University of Petroleum at Beijing, Beijing 102249, China 10 4Department of Earth, Environmental and Planetary Sciences, Rice University, 6100 Main Street, 11 Houston, TX 77005, USA 12 5Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089, USA 13 6Earthquake Administration of Sichuan Province, Chengdu 610041, China 14 7Institute of Earthquake Science, China Earthquake Administration, Beijing 100029, China 15 Correspondence and requests for materials should be addressed to F.N. ([email protected]). 16 17 Various studies report on temporal changes of seismic velocities in the crust and attempt to relate 18 the observations to changes of stress and material properties around faults. While there is growing 19 number of observations on co-seismic velocity reductions, detailed observations of healing phases 20 are generally lacking. Here we report on pronounced co-seismic reduction of velocities around two 21 locked sections (asperities) of the Longmenshan fault with large slip during the 2008 Mw 7.9 22 Wenchuan earthquake, and subsequent healing of the velocities. The healing phase is accelerated 23 significantly at the southern asperity right after the nearby 2013 Mw 6.6 Lushan earthquake.
    [Show full text]
  • Earthquake Phenomenology from the Field the April 20, 2013, Lushan Earthquake Springerbriefs in Earth Sciences
    SPRINGER BRIEFS IN EARTH SCIENCES Zhongliang Wu Changsheng Jiang Xiaojun Li Guangjun Li Zhifeng Ding Earthquake Phenomenology from the Field The April 20, 2013, Lushan Earthquake SpringerBriefs in Earth Sciences For further volumes: http://www.springer.com/series/8897 Zhongliang Wu · Changsheng Jiang · Xiaojun Li Guangjun Li · Zhifeng Ding Earthquake Phenomenology from the Field The April 20, 2013, Lushan Earthquake 1 3 Zhongliang Wu Guangjun Li Changsheng Jiang Earthquake Administration of Sichuan Xiaojun Li Province Zhifeng Ding Chengdu China Earthquake Administration China Institute of Geophysics Beijing China ISSN 2191-5369 ISSN 2191-5377 (electronic) ISBN 978-981-4585-13-2 ISBN 978-981-4585-15-6 (eBook) DOI 10.1007/978-981-4585-15-6 Springer Singapore Heidelberg New York Dordrecht London Library of Congress Control Number: 2014939941 © The Author(s) 2014 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied specifically for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer.
    [Show full text]
  • Structure-Controlled Asperities of the 1920 Haiyuan M8.5 and 1927
    www.nature.com/scientificreports OPEN Structure‑controlled asperities of the 1920 Haiyuan M8.5 and 1927 Gulang M8 earthquakes, NE Tibet, China, revealed by high‑resolution seismic tomography Quan Sun1,2, Shunping Pei1,2,3*, Zhongxiong Cui4, Yongshun John Chen5, Yanbing Liu1,2, Xiaotian Xue1,2, Jiawei Li1,2, Lei Li1,2 & Hong Zuo1,2 Detailed crustal structure of large earthquake source regions is of great signifcance for understanding the earthquake generation mechanism. Numerous large earthquakes have occurred in the NE Tibetan Plateau, including the 1920 Haiyuan M8.5 and 1927 Gulang M8 earthquakes. In this paper, we obtained a high‑resolution three‑dimensional crustal velocity model around the source regions of these two large earthquakes using an improved double‑diference seismic tomography method. High‑ velocity anomalies encompassing the seismogenic faults are observed to extend to depths of 15 km, suggesting the asperity (high‑velocity area) plays an important role in the preparation process of large earthquakes. Asperities are strong in mechanical strength and could accumulate tectonic stress more easily in long frictional locking periods, large earthquakes are therefore prone to generate in these areas. If the close relationship between the aperity and high‑velocity bodies is valid for most of the large earthquakes, it can be used to predict potential large earthquakes and estimate the seismogenic capability of faults in light of structure studies. Earthquakes occur when the stored energy in the Earth’s lithosphere is suddenly released. Large earthquakes usually cause great hazards on natural environment and/or humans. Tere has been an obvious surge of great earthquakes with magnitudes ≥ 8.0 during the past decade with great diversity at various aspects 1.
    [Show full text]
  • Triggered Slip on a Back Reverse Fault in the Mw6.8 2013 Lushan, China Earthquake Revealed by Joint Inversion of Local Strong Mo
    Tectonophysics 672–673 (2016) 24–33 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Triggered slip on a back reverse fault in the Mw6.8 2013 Lushan, China earthquake revealed by joint inversion of local strong motion accelerograms and geodetic measurements Guohong Zhang a,b,⁎,EricA.Hetlandb,XinjianShana, Martin Vallée c, Yunhua Liu a, Yingfeng Zhang a, Chunyan Qu a a State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China b Earth and Environmental Sciences, University of Michigan, Ann Arbor, USA c Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR 7154 CNRS, Paris, France article info abstract Article history: The 2013 Mw6.8 Lushan, China earthquake occurred in the southwestern end of the Longmenshan fault zone. We Received 4 June 2015 jointly invert local strong motion data and geodetic measurements of coseismic surface deformation, including Received in revised form 11 January 2016 GPS and InSAR, to obtain a robust model of the rupture process of the 2013 Lushan earthquake. Our joint inver- Accepted 13 January 2016 sion best model involves the rupture of two opposing faults during the Lushan earthquake, a main fault and a sec- Available online 6 February 2016 ondary fault. It is only when the secondary fault is included that both the GPS and InSAR measurements are fit along with the near-field strong motion. Over 75% of the computed moment was released in slip on the main Keywords: Triggered fault slip fault segment, a northwest dipping, listric thrust fault, with buried thrust and dextral strike-slip at hypocenter Back reverse fault depths, and with only minor slip closer to the surface.
    [Show full text]
  • Table of Contents
    A field assessment of the April 20, 2013, Mw = 6.6, Lushan, China, Earthquake Table of contents Abstract ............................................................................................................................................. 1 Introduction ....................................................................................................................................... 1 Geology and Tectonics...................................................................................................................... 2 The main shock and aftershocks ....................................................................................................... 2 Ground Motion and Intensity Survey ................................................................................................ 2 Structural Response........................................................................................................................... 3 Lifelines ............................................................................................................................................ 4 Conclusion ........................................................................................................................................ 5 Acknowledgment .............................................................................................................................. 5 References ......................................................................................................................................... 6 Figure
    [Show full text]
  • Changes in Tropospheric Ozone Associated with Strong Earthquakes and Possible Mechanism
    Chapman University Chapman University Digital Commons Biology, Chemistry, and Environmental Sciences Science and Technology Faculty Articles and Faculty Articles and Research Research 5-17-2021 Changes in Tropospheric Ozone Associated With Strong Earthquakes and Possible Mechanism Feng Jing Ramesh P. Singh Follow this and additional works at: https://digitalcommons.chapman.edu/sees_articles Part of the Atmospheric Sciences Commons, Environmental Indicators and Impact Assessment Commons, Environmental Monitoring Commons, Geochemistry Commons, and the Geophysics and Seismology Commons Changes in Tropospheric Ozone Associated With Strong Earthquakes and Possible Mechanism Comments This article was originally published in IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, volume 14, in 2021. https://doi.org/10.1109/JSTARS.2021.3080843 Creative Commons License This work is licensed under a Creative Commons Attribution 4.0 License. 5300 IEEE JOURNAL OF SELECTED TOPICS IN APPLIED EARTH OBSERVATIONS AND REMOTE SENSING, VOL. 14, 2021 Changes in Tropospheric Ozone Associated With Strong Earthquakes and Possible Mechanism Feng Jing , Member, IEEE, and Ramesh P. Singh , Senior Member, IEEE Abstract—The index of ozone anomaly (IOA) has been proposed occurred globally [9], [10]. The changes observed in borehole, to detect changes in tropospheric ozone associated with strong ground, atmospheric, and ionospheric parameters have provided earthquakes. The tropospheric ozone prior and after the 2008 evidence to believe existence of strong coupling between land– Wenchuan earthquake has been analyzed using IOA. Atmospheric infrared sounder ozone volume mixing ratio (O3 VMR) at different atmosphere–ionosphere during the phase of earthquake prepara- pressure levels (600, 500, 400, 300, 200 hPa) for an 18-year period tion [11]–[13].
    [Show full text]
  • Pathways to Earthquake Resilience in China
    Report Pathways to earthquake resilience in China October 2015 Overseas Development Institute 203 Blackfriars Road London SE1 8NJ Tel. +44 (0) 20 7922 0300 Fax. +44 (0) 20 7922 0399 E-mail: [email protected] www.odi.org www.odi.org/facebook www.odi.org/twitter Readers are encouraged to reproduce material from ODI Reports for their own publications, as long as they are not being sold commercially. As copyright holder, ODI requests due acknowledgement and a copy of the publication. For online use, we ask readers to link to the original resource on the ODI website. The views presented in this paper are those of the author(s) and do not necessarily represent the views of ODI. © Overseas Development Institute 2015. This work is licensed under a Creative Commons Attribution-NonCommercial Licence (CC BY-NC 3.0). ISSN: 2052-7209 Cover photo: Photo by GDS, Children receiving the GDS disaster risk reduction kit, Shaanxi Province, China Contents Acknowledgements 9 About the authors 9 Glossary of terms 11 Acronyms 11 1. Introduction 13 John Young 2. Earthquake disaster risk reduction policies and programmes in China 16 Cui Ke, Timothy Sim and Lena Dominelli 3. Current knowledge on seismic hazards in Shaanxi Province 23 By Feng Xijie, Richard Walker and Philip England 4. Community-based approaches to disaster risk reduction in China 30 Lena Dominelli, Timothy Sim and Cui Ke 5. Case study: World Vision’s community disaster response plan in Ranjia village 42 William Weizhong Chen, Ning Li and Ling Zhang 6. Case study: Gender Development Solution’s disaster risk reduction in primary education 46 Zhao Bin 7.
    [Show full text]