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An Informed System Development Approach to Tropical Cyclone Track and Intensity Forecasting
Linköping Studies in Science and Technology Dissertations. No. 1734 An Informed System Development Approach to Tropical Cyclone Track and Intensity Forecasting by Chandan Roy Department of Computer and Information Science Linköping University SE-581 83 Linköping, Sweden Linköping 2016 Cover image: Hurricane Isabel (2003), NASA, image in public domain. Copyright © 2016 Chandan Roy ISBN: 978-91-7685-854-7 ISSN 0345-7524 Printed by LiU Tryck, Linköping 2015 URL: http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-123198 ii Abstract Introduction: Tropical Cyclones (TCs) inflict considerable damage to life and property every year. A major problem is that residents often hesitate to follow evacuation orders when the early warning messages are perceived as inaccurate or uninformative. The root problem is that providing accurate early forecasts can be difficult, especially in countries with less economic and technical means. Aim: The aim of the thesis is to investigate how cyclone early warning systems can be technically improved. This means, first, identifying problems associated with the current cyclone early warning systems, and second, investigating if biologically based Artificial Neural Networks (ANNs) are feasible to solve some of the identified problems. Method: First, for evaluating the efficiency of cyclone early warning systems, Bangladesh was selected as study area, where a questionnaire survey and an in-depth interview were administered. Second, a review of currently operational TC track forecasting techniques was conducted to gain a better understanding of various techniques’ prediction performance, data requirements, and computational resource requirements. Third, a technique using biologically based ANNs was developed to produce TC track and intensity forecasts. -
Natural Disaster Management
Lesson Learned Presentation Ministry of Social Welfare, Relief and Resettlement, The Republic of the Union of Myanmar 1 Contents • Hazards Profile of Myanmar • Legislation • National Framework • Institutional Arrangement • AADMER Implementation and ASEAN Related Activities • DRR Activities of Ministry of Social Welfare, Relief and Resettlement • Experiences • Lesson Learned • Way Forward 2 Hazard Profile of Myanmar 33 Hazard Profile (Fire) (Flood) (Storm) (Earthquake) (Tsunami) (Landslide) (Drought) (Epidemic) 4 Potential Hazards and Prone Areas in Myanmar Fire All round the country Flood Annual flood occur in Kayin State, Bago Region, Mandalay Region, Ayaeyarwaddy Region. Especially townships and villages which are situated along the rivers banks of Ayaryarwaddy, Sittaung, Thanlwin, Madauk and Shwe Kyin. Cyclone Thanintharyi region, Mon State, Rakhine State, Yangon Region and AyaeyarWaddy Region 55 Earthquake can occur around the country, Nay Pyi Taw, Bago, Sagaing and Mandalay Regions and Shan State are earthquake prone areas. Tsunami Costal areas such as Rakhine and Mon States and Ayaeyarwaddy, Yangon and Thanintharyi Regions Drought Central Myanmar (Sagaing, Magwe,and Mandalay regions) Landslide Hilly Region (Kachin,Chin, Shan and Rakhine 66 St t d Th i th i Ri) Legislation 77 Legislation • The Disaster Management Law with (9) Chapters has been enacted on 31st July 2013. • Title and Definition • Objectives (a) to implement natural disaster management programmes systematically and expeditiously in order to reduce disaster risks; (b) -
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Emergency Market Mapping and Analysis (EMMA) Understanding the Fish Market System in Kyauk Phyu Township Rakhine State. Annex to the Final report to DfID Post Giri livelihoods recovery, Kyaukphyu Township, Rakhine State February 14 th 2011 – November 13 th 2011 August 2011 1 Background: Rakhine has a total population of 2,947,859, with an average household size of 6 people, (5.2 national average). The total number of households is 502,481 and the total number of dwelling units is 468,000. 1 On 22 October 2010, Cyclone Giri made landfall on the western coast of Rakhine State, Myanmar. The category four cyclonic storm caused severe damage to houses, infrastructure, standing crops and fisheries. The majority of the 260,000 people affected were left with few means to secure an income. Even prior to the cyclone, Rakhine State (RS) had some of the worst poverty and social indicators in the country. Children's survival and well-being ranked amongst the worst of all State and Divisions in terms of malnutrition, with prevalence rates of chronic malnutrition of 39 per cent and Global Acute Malnutrition of 9 per cent, according to 2003 MICS. 2 The State remains one of the least developed parts of Myanmar, suffering from a number of chronic challenges including high population density, malnutrition, low income poverty and weak infrastructure. The national poverty index ranks Rakhine 13 out of 17 states, with an overall food poverty headcount of 12%. The overall poverty headcount is 38%, in comparison the national average of poverty headcount of 32% and food poverty headcount of 10%. -
Effect of Major Storms on Morphology and Sediments of a Coastal Lake on the Northwest Florida Barrier Coast Aaron C
Florida State University Libraries Electronic Theses, Treatises and Dissertations The Graduate School 2008 Effect of Major Storms on Morphology and Sediments of a Coastal Lake on the Northwest Florida Barrier Coast Aaron C. Lower Follow this and additional works at the FSU Digital Library. For more information, please contact [email protected] FLORIDA STATE UNIVERSITY COLLEGE OF ARTS AND SCIENCES EFFECT OF MAJOR STORMS ON MORPHOLOGY AND SEDIMENTS OF A COASTAL LAKE ON THE NORTHWEST FLORIDA BARRIER COAST By AARON C. LOWER A Thesis submitted to the Department of Geological Sciences in partial fulfillment of the requirements for the degree of Master of Science Degree Awarded: Summer Semester, 2008 The members of the Committee approve the thesis of Aaron C. Lower defended on March 19, 2008. ___________________________ Joseph F. Donoghue Professor Directing Thesis ___________________________ Anthony J. Arnold Committee Member ___________________________ Sherwood W. Wise Committee Member ___________________________ Stephen J. Kish Committee Member Approved: ___________________________ A. Leroy Odom, Chair, Department of Geological Sciences ii ACKNOWLEDGEMENTS There are many people I would like to thank and recognize for their support throughout my studies. First, I would like to thank my advisor, Dr. Joseph Donoghue, for his continuous support and guidance during the MS program. Many thanks to the late Jim Balsillie, whose field expertise and suggestions proved invaluable to the completion of this thesis. Thanks to Jim Sparr, of the Florida Geological Survey, for his assistance with the GPR surveys. I am grateful to Matt Curren, formerly of the FSU Antarctic Research Facility, for the use of the X-ray machine, darkroom facilities and the storage of my cores. -
Understanding the Characteristics of Rapid Intensity Changes of Tropical Cyclones Over North Indian Ocean
Research Article Understanding the characteristics of rapid intensity changes of Tropical Cyclones over North Indian Ocean Raghu Nadimpalli1 · Shyama Mohanty1 · Nishant Pathak1 · Krishna K. Osuri2 · U. C. Mohanty1 · Somoshree Chatterjee1 Received: 31 August 2020 / Accepted: 21 December 2020 © The Author(s) 2021 OPEN Abstract North Indian Ocean (NIO), which comprises of Bay of Bengal (BoB) and Arabian Sea (AS) basins, is one of the highly poten- tial regions for Tropical Cyclones (TCs) in the world. Signifcant improvements have been achieved in the prediction of the movement of TCs, since the last decade. However, the prediction of sudden intensity changes becomes a challeng- ing task for the research and operational meteorologists. Hence, the present study focuses on fnding the climatological characteristics of such intensity changes over NIO regions. Rapid Intensifcation (RI) is defned as the 24-h maximum sustained surface wind speed rate equal to 30 knots (15.4 ms−1). The results suggest that the TCs formed over the NIO basin are both seasonal and basin sensitive. Since 2000, a signifcant trend is observed in RI TCs over the basin. At least one among three cyclones getting intensifed is of RI category. More number of RI cases have been identifed in the BoB basin than the AS. The post-monsoon season holds more RI and rapid decay cases, with 63% and 90% contribution. Most of the TCs are attaining RI onset in their initial stage. Further, India is receiving more landfalling RI TCs, followed by Bangladesh and Oman. The east coast of India, Tamil Nadu, and Andhra Pradesh are the most vulnerable states to these RI TCs. -
Prediction of Landfalling Tropical Cyclones Over East Coast of India in the Global Warming Era
Prediction of Landfalling Tropical Cyclones over East Coast of India in the Global Warming Era U. C. Mohanty School of Earth, Ocean and Climate Sciences Indian Institute of Technology Bhubaneswar Outline of Presentation • Introduction • Mesoscale modeling of TCs with MM5, ARW, NMM and HWRF systems • Conclusions and Future Directions Natural disasters Hydrometeorologi- Geophysical cal Disasters: Disasters: Earthquakes Cyclones Avalanches Flood Land slides Drought Volcanic eruption Tornadoes Dust storms Heat waves Cold waves Warmest 12 years: 1998,2005,2003,2002,2004,2006, 2001,1997,1995,1999,1990,2000 Global warming Period Rate 25 0.1770.052 50 0.1280.026 100 0.0740.018 150 0.0450.012 Years /decade IPCC Introduction • Climate models are becoming most important tools for its increasing efficiency and reliability to capture past climate more realistically with time and capability to provide future climate projections. • Observations of land based weather stations in global network confirm that Earth surface air temperature has risen more than 0.7 ºC since the late 1800s to till date. This warming of average temperature around the globe has been especially sharp since 1970s. • The IPCC predicted that probable range of increasing temperature between 1.4 - 5.8 ºC over 1990 levels by the year 2100. Contd…… • The warming in the past century is mainly due to the increase of green house gases and most of the climate scientists have agreed with IPCC report that the Earth will warm along with increasing green house gases. • In warming environment, weather extremes such as heavy rainfall (flood), deficit rainfall (drought), heat/cold wave, storm etc will occur more frequent with higher intensity. -
Growth of Cyclone Viyaru and Phailin – a Comparative Study
Growth of cyclone Viyaru and Phailin – a comparative study SDKotal1, S K Bhattacharya1,∗, SKRoyBhowmik1 and P K Kundu2 1India Meteorological Department, NWP Division, New Delhi 110 003, India. 2Department of Mathematics, Jadavpur University, Kolkata 700 032, India. ∗Corresponding author. e-mail: [email protected] The tropical cyclone Viyaru maintained a unique quasi-uniform intensity during its life span. Despite beingincontactwithseasurfacefor>120 hr travelling about 2150 km, the cyclonic storm (CS) intensity, once attained, did not intensify further, hitherto not exhibited by any other system over the Bay of Bengal. On the contrary, the cyclone Phailin over the Bay of Bengal intensified into very severe cyclonic storm (VSCS) within about 48 hr from its formation as depression. The system also experienced rapid intensification phase (intensity increased by 30 kts or more during subsequent 24 hours) during its life time and maximum intensity reached up to 115 kts. In this paper, a comparative study is carried out to explore the evolution of the various thermodynamical parameters and possible reasons for such converse features of the two cyclones. Analysis of thermodynamical parameters shows that the development of the lower tropospheric and upper tropospheric potential vorticity (PV) was low and quasi-static during the lifecycle of the cyclone Viyaru. For the cyclone Phailin, there was continuous development of the lower tropospheric and upper tropospheric PV, which attained a very high value during its lifecycle. Also there was poor and fluctuating diabatic heating in the middle and upper troposphere and cooling in the lower troposphere for Viyaru. On the contrary, the diabatic heating was positive from lower to upper troposphere with continuous development and increase up to 6◦C in the upper troposphere. -
Shelter and NFI Cluster Evaluation Cyclone Giri Response, Myanmar October 2010 to January 2011 July 2011 Kerren Hedlund
The Rakhine Coast One month after Giri. Photo courtesy of Solidarities International and National Compassionate Volunteers. Shelter and NFI Cluster Evaluation Cyclone Giri Response, Myanmar October 2010 to January 2011 July 2011 Kerren Hedlund This evaluation has been managed by IFRC’s Shelter and Settlements Department in cooperation with the Planning and Evaluation Department. IFRC is committed to upholding its Framework for Evaluation. The framework is designed to promote reliable, useful, ethical evaluations that contribute to organizational learning, accountability, and our mission to best serve those in need. It demonstrates the IFRC’s commitment to transparency, providing a publicly accessible document to all stakeholders so that they may better understand and participate in the evaluation function. International Federation of Red Cross and Red Crescent Societies (IFRC) Case postale 372 1211 Genève 19 Suisse Tel: +41 22 730 4222 Fax: +41 22 733 0395 www.ifrc.org Disclaimer The opinions expressed are those of the author(s), and do not necessarily reflect those of the International Federation of Red Cross and Red Crescent Societies. Responsibility for the opinions expressed in this report rests solely with the author(s). Publication of this document does not imply endorsement by the IFRC of the opinions expressed. 2 CONTENT ACRONYMS.......................................................................................................................................................................... 4 EXECUTIVE SUMMARY ........................................................................................................................................................ -
Rehabilitation, Reconstruction & Development a Post Cyclone Nargis Initiative
Rehabilitation, Reconstruction & Development A Post Cyclone Nargis Initiative 1 2 Metta Development Foundation Table of Contents Forward, Executive Director 2 A Post Cyclone Nargis Initiative - Executive Summary 6 01. Introduction – Waves of Change The Ayeyarwady Delta 10 Metta’s Presence in the Delta. The Tsunami 11 02. Cyclone Nargis –The Disaster 12 03. The Emergency Response – Metta on Site 14 04. The Global Proposal 16 The Proposal 16 Connecting Partners - Metta as Hub 17 05. Rehabilitation, Reconstruction and Development August 2008-July 2011 18 Introduction 18 A01 – Relief, Recovery and Capacity Building: Rice and Roofs 18 A02 – Food Security: Sowing and Reaping 26 A03 – Education: For Better Tomorrows 34 A04 – Health: Surviving and Thriving 40 A05 – Disaster Preparedness and Mitigation: Providing and Protecting 44 A06 – Lifeline Systems and Transportation: The Road to Safety 46 Conclusion 06. Local Partners – The Communities in the Delta: Metta Meeting Needs 50 07. International Partners – The Donor Community Meeting Metta: Metta Day 51 08. Reporting and External Evaluation 52 09. Cyclones and Earthquakes – Metta put anew to the Test 55 10. Financial Review 56 11. Beyond Nargis, Beyond the Delta 59 12. Thanks 60 List of Abbreviations and Acronyms 61 Staff Directory 62 Volunteers 65 Annex 1 - The Emergency Response – Metta on Site 68 Annex 2 – Maps 76 Annex 3 – Tables 88 Rehabilitation, Reconstruction & Development A Post Cyclone Nargis Initiative 3 Forword Dear Friends, Colleagues and Partners On the night of 2 May 2008, Cyclone Nargis struck the delta of the Ayeyarwady River, Myanmar’s most densely populated region. The cyclone was at the height of its destructive potential and battered not only the southernmost townships but also the cities of Yangon and Bago before it finally diminished while approaching the mountainous border with Thailand. -
Real-Time Track Prediction of Tropical Cyclones Over the North Indian Ocean Using the ARW Model
2476 JOURNAL OF APPLIED METEOROLOGY AND CLIMATOLOGY VOLUME 52 Real-Time Track Prediction of Tropical Cyclones over the North Indian Ocean Using the ARW Model KRISHNA K. OSURI AND U. C. MOHANTY School of Earth, Ocean and Climate Sciences, Indian Institute of Technology Bhubaneswar, Odisha, India A. ROUTRAY National Centre for Medium Range Weather Forecasting, Noida, India M. MOHAPATRA India Meteorological Department, New Delhi, India DEV NIYOGI Purdue University, West Lafayette, Indiana (Manuscript received 18 November 2012, in final form 9 July 2013) ABSTRACT The performance of the Advanced Research version of the Weather Research and Forecasting (ARW) model in real-time prediction of tropical cyclones (TCs) over the north Indian Ocean (NIO) at 27-km res- olution is evaluated on the basis of 100 forecasts for 17 TCs during 2007–11. The analyses are carried out with respect to 1) basins of formation, 2) straight-moving and recurving TCs, 3) TC intensity at model initialization, and 4) season of occurrence. The impact of high resolution (18 and 9 km) on TC prediction is also studied. Model results at 27-km resolution indicate that the mean track forecast errors (skill with reference to per- sistence track) over the NIO were found to vary from 113 to 375 km (7%–51%) for a 12–72-h forecast. The model showed a right/eastward and slow bias in TC movement. The model is more skillful in track prediction when initialized at the intensity stage of severe cyclone or greater than at the intensity stage of cyclone or lower. The model is more efficient in predicting landfall location than landfall time. -
Meeting Minutes
INFORMAL EMERGENCY SHELTER COORDINATION CYCLONE GIRI MYANMAR MEETING MINUTES Date 26th October, 2010 - 1500-1630hrs Venue Meeting Room, IFRC Office, Yangon Chair Anno Müller Note taker Aung Thu Win (ESC Information Manager ) Ei Ei Thein (MIMU), Myat Su Win (UNOCHA), Aung Ze Ya (MRCS), Nariko Tomiyama (IOM), Nicolas Participants Guillard (ACF), Malar Win (MRCS), Sabine Linzbichler (DRC, Danish Refugee Council), Tin Htut (UNICEF), Maurice (KMSS), Maung Maung Myint (UNHABITAT), Pyae Phyo Aung (IFRC), Maung Maung Than (JICA), Augustine Piary (Karunar Myanmar), Zin Aye Swe (UNHABITAT), Mu Mu Kyi (UNHABITAT), Aaron Brent (French Red Cross), Jero Candela (Solidarites International), Narendra Singh (IFRC), Masayuki Ishikawa (Embassy of Japan), Agenda item # 0: Welcome notes from the Meeting Chair Meeting chair welcomed the participants and introduced himself. He briefly explained the agenda items and requested the involvement and suggestions from all the partners in order to standardize the response. Agenda item # 1: Introduction of Participants - All the participants introduced themselves - Total of 22 participants from 14 different organizations listed below attended the meeting - The Organizations who attended the meeting are, IOM, ACF, MRCS, IFRC, Danish Refugee Council, UNICEF, Karunar Myanmar (KMSS), UNHABITAT, MIMU, UNOCHA, French Red Cross (FRC), JICA, Japanese Embassy, Solidarites International Agenda item # 2: Role definition of informal ESC team Meeting chair convey the offer from IFRC to the partners for independent coordination of the shelter Discussion response with himself as Coordinator and Aung Thu Win as Information Manager. Considering the informal nature of the Emergency Shelter Coordination at this point not all normal tasks can be performed. By example development of an official stra tegy, representation in the media and coordination with authorities will be difficult in the current situation. -
Hazard Profile of Myanmar: an Introduction 1.1
Table of Contents Table of Contents ............................................................................................................ I List of Figures ................................................................................................................ III List of Tables ................................................................................................................. IV Acronyms and Abbreviations ......................................................................................... V 1. Hazard Profile of Myanmar: An Introduction 1.1. Background ...................................................................................................................... 1 1.2. Myanmar Overview ......................................................................................................... 2 1.3. Development of Hazard Profile of Myanmar : Process ................................................... 2 1.4. Objectives and scope ....................................................................................................... 3 1.5. Structure of ‘Hazard Profile of Myanmar’ Report ........................................................... 3 1.6. Limitations ....................................................................................................................... 4 2. Cyclones 2.1. Causes and Characteristics of Cyclones in the Bay of Bengal .......................................... 5 2.2. Frequency and Impact ....................................................................................................