Trends in Disaster Philanthropy
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Enhancing Psychological Support
Appeal No. MDRCN001 CHINA: FLOODS 2006 17 October 2007 The Federation’s mission is to improve the lives of vulnerable people by mobilizing the power of humanity. It is the world’s largest humanitarian organization and its millions of volunteers are active in over 185 countries. In Brief Final Report; Period covered: 2 August 2006 - 31 July 2007; Final appeal coverage: 26%. <Click here to link directly to the attached Final Financial Report>. Appeal history: • This appeal was launched on 02 August 2006 seeking CHF 5,950,200 (USD 4,825,791 or EUR 3,782,708) for 12 months to assist 240,000 beneficiaries. • Disaster Relief Emergency Funds (DREF) allocated: CHF 213,000 Related Emergency or Annual Appeals: 2006-2007 China Appeal MAACN001 2006-2007 East Asia Appeal MAA54001 Operational Summary: Every year, China is crippled by various natural disasters. In 2006, natural disasters were responsible for the deaths of at least 3,186 people. Over 13.8 million people were evacuated and relocated, with 1.93 million houses completely destroyed. According to latest statistics provided by the ministry of civil affairs, flooding in 2006 had caused a direct economic loss of USD 24 billion (CHF 30 billion). The Red Cross Society of China first responded to meet the emergency needs in Hunan province arising from typhoon Bilis. The Disaster Relief Emergency Fund allocated CHF 213,000 to initial relief distributions. A flood affected village in Hunan province. RCSC/International Federation Through the Federation’s China Floods Emergency Appeal (MDRCN001) launched on 2 August 2006, CHF 1.57 million was raised to provide additional support to beneficiaries through the national society. -
The Surface Energy Balance in a Cold-Arid Permafrost Environment
https://doi.org/10.5194/tc-2019-286 Preprint. Discussion started: 9 March 2020 c Author(s) 2020. CC BY 4.0 License. The surface energy balance in a cold-arid permafrost environment, Ladakh Himalaya, India John Mohd Wani1, Renoj J. Thayyen2*, Chandra Shekhar Prasad Ojha1, and Stephan Gruber3 1Department of Civil Engineering, Indian Institute of Technology (IIT) Roorkee, India, 2Water Resources System Division, National Institute of Hydrology, Roorkee, India ([email protected]; [email protected]), 3Department of Geography & Environmental Studies, Carleton University, Ottawa, Canada Abstract: Cryosphere of the cold-arid trans-Himalayan region is unique with its significant permafrost cover. While the information on the permafrost characteristics and its extent started emerging, the governing energy regimes of this cryosphere region is of particular interest. This paper present the results of Surface Energy Balance (SEB) studies carried out in the upper 5 Ganglass catchment in the Ladakh region of India, which feed directly to the River Indus. The point SEB is estimated using the one-dimensional mode of GEOtop model from 1 September 2015 to 31 August 2017 at 4727 m a.s.l elevation. The model is evaluated using field monitored radiation components, snow depth variations and one-year near-surface ground temperatures and showed good agreement with the respective simulated values. The study site has an air 10 temperature range of – 23.7 to 18.1 °C with a mean annual average temperature (MAAT) of - 2.5 and ground surface temperature range of -9.8 to 19.1 °C. For the study period, the surface energy balance characteristics of the cold-arid site show that the net radiation was the major component with mean value of 28.9 W m-2, followed by sensible heat flux (13.5 W m-2) and latent heat flux (12.8 W m-2), and the ground heat flux was equal to 0.4 W m-2. -
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 -
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. -
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. -
Observational Analysis of Heavy Rainfall Mechanisms Associated with Severe Tropical Storm Bilis (2006) After Its Landfall
JUNE 2009 G A O E T A L . 1881 Observational Analysis of Heavy Rainfall Mechanisms Associated with Severe Tropical Storm Bilis (2006) after Its Landfall SHUANZHU GAO China National Meteorological Center, Beijing, China ZHIYONG MENG Department of Atmospheric Sciences, School of Physics, Peking University, Beijing, China FUQING ZHANG Department of Meteorology, The Pennsylvania State University, University Park, Pennsylvania LANCE F. BOSART Department of Atmospheric Sciences, University at Albany, State University of New York, Albany, New York (Manuscript received 5 June 2008, in final form 8 December 2008) ABSTRACT This observational study attempts to determine factors responsible for the distribution of precipitation over large areas of southern China induced by Bilis, a western North Pacific Ocean severe tropical storm that made landfall on the southeastern coast of mainland China on 14 July 2006 with a remnant circulation that persisted over land until after 17 July 2006. The heavy rainfalls associated with Bilis during and after its landfall can be divided into three stages. The first stage of the rainfall, which occurred in Fujian and Zhejiang Provinces, could be directly induced by the inner-core storm circulation during its landfall. The third stage of rainfall, which occurred along the coastal areas of Guangdong and Fujian Provinces, likely resulted from the interaction between Bilis and the South China Sea monsoon enhanced by topographical lifting along the coast. The second stage of the rainfall, which appeared inland around the border regions between Jiangxi, Hunan, and Guangdong Provinces, caused the most catastrophic flooding and is the primary focus of the current study. It is found that during the second stage of the rainfall all three ingredients of deep moist convection (moisture, instability, and lifting) are in place. -
Climate Vulnerability in Asia's High Mountains
Climate Vulnerability in Asia’s High Mountains COVER: VILLAGE OF GANDRUNG NESTLED IN THE HIMALAYAS. ANNAPURNA AREA, NEPAL; © GALEN ROWELL/MOUNTAIN LIGHT / WWF-US Climate Vulnerability in Asia’s High Mountains May 2014 PREPARED BY TAYLOR SMITH Independent Consultant [email protected] This report is made possible by the generous support of the American people through the United States Agency for International Development (USAID). The contents are the responsibility of WWF and do not necessarily reflect the views of USAID or the United States Government. THE UKOK PLATEAU NATURAL PARK, REPUBLIC OF ALTAI; © BOGOMOLOV DENIS / WWF-RUSSIA CONTENTS EXECUTIVE SUMMARY .........................................1 4.2.1 Ecosystem Restoration ........................................... 40 4.2.2 Community Water Management .............................. 41 State of Knowledge on Climate Change Impacts .................. 1 4.3 Responding to Flooding and Landslides ....................... 41 State of Knowledge on Human Vulnerability ......................... 1 4.3.1 Flash Flooding ......................................................... 41 Knowledge Gaps and Policy Perspective .............................. 3 4.3.2 Glacial Lake Outburst Floods .................................. 42 Recommendations for Future Adaptation Efforts ................. 3 4.3.3 Landslides ............................................................... 43 4.4 Adaptation by Mountain Range ....................................... 44 Section I 4.4.1 The Hindu Kush–Karakorum–Himalaya Region -
World Bank Document
Document of The World Bank FOR OFFICIAL USE ONLY Public Disclosure Authorized Report No. 82638-PH INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT SUPPLEMENTAL FINANCING DOCUMENT Public Disclosure Authorized FOR PROPOSED SUPPLEMENTAL FINANCING IN THE AMOUNT OF US$500 MILLION TO THE REPUBLIC OF THE PHILIPPINES FOR Public Disclosure Authorized THE PHILIPPINES SECOND DEVELOPMENT POLICY LOAN TO FOSTER MORE INCLUSIVE GROWTH FOR POST TYPHOON RECOVERY December 04, 2013 Poverty Reduction and Economic Management Sector Department Philippines East Asia and Pacific Region Public Disclosure Authorized This document has a restricted distribution and may be used by recipients only in the performance of their official duties. Its contents may not otherwise be disclosed without World Bank authorization. GOVERNMENT'S FISCAL YEAR January 1 – December 31 CURRENCY EQUIVALENTS Currency unit: Philippine Pesos (PHP) as of November 12, 2013 US$ 1 = PHP43.59 Currency Unit US$1.00 ABBREVIATIONS AND ACRONYMS AIR Applied Insurance Research JBIC Japan Bank for International Cooperation BPO Business Processing and Outsourcing KALAHI- Kapitbisig Laban Sa Kahirapan- CIDSS Comprehensive and Integrated Delivery of Social Services BSP Bangko Sentral ng Pilipinas LBP Land Bank of the Philippines CAS Country Assistance Strategy LDP Letter of Development Policy CAT-DDO Catastrophe Draw Down Option LGU Local Government Unit CCT Conditional Cash Transfer NCDDP National Community Driven Development Project COA Commission on Audit NDRRMC National Disaster Risk Reduction -
Appendix 8: Damages Caused by Natural Disasters
Building Disaster and Climate Resilient Cities in ASEAN Draft Finnal Report APPENDIX 8: DAMAGES CAUSED BY NATURAL DISASTERS A8.1 Flood & Typhoon Table A8.1.1 Record of Flood & Typhoon (Cambodia) Place Date Damage Cambodia Flood Aug 1999 The flash floods, triggered by torrential rains during the first week of August, caused significant damage in the provinces of Sihanoukville, Koh Kong and Kam Pot. As of 10 August, four people were killed, some 8,000 people were left homeless, and 200 meters of railroads were washed away. More than 12,000 hectares of rice paddies were flooded in Kam Pot province alone. Floods Nov 1999 Continued torrential rains during October and early November caused flash floods and affected five southern provinces: Takeo, Kandal, Kampong Speu, Phnom Penh Municipality and Pursat. The report indicates that the floods affected 21,334 families and around 9,900 ha of rice field. IFRC's situation report dated 9 November stated that 3,561 houses are damaged/destroyed. So far, there has been no report of casualties. Flood Aug 2000 The second floods has caused serious damages on provinces in the North, the East and the South, especially in Takeo Province. Three provinces along Mekong River (Stung Treng, Kratie and Kompong Cham) and Municipality of Phnom Penh have declared the state of emergency. 121,000 families have been affected, more than 170 people were killed, and some $10 million in rice crops has been destroyed. Immediate needs include food, shelter, and the repair or replacement of homes, household items, and sanitation facilities as water levels in the Delta continue to fall. -
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. -
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. -
China Date: 8 January 2007
Refugee Review Tribunal AUSTRALIA RRT RESEARCH RESPONSE Research Response Number: CHN31098 Country: China Date: 8 January 2007 Keywords: China – Taiwan Strait – 2006 Military exercises – Typhoons This response was prepared by the Country Research Section of the Refugee Review Tribunal (RRT) after researching publicly accessible information currently available to the RRT within time constraints. This response is not, and does not purport to be, conclusive as to the merit of any particular claim to refugee status or asylum. Questions 1. Is there corroborating information about military manoeuvres and exercises in Pingtan? 2. Is there any information specifically about the military exercise there in July 2006? 3. Is there any information about “Army day” on 1 August 2006? 4. What are the aquatic farming/fishing activities carried out in that area? 5. Has there been pollution following military exercises along the Taiwan Strait? 6. The delegate makes reference to independent information that indicates that from May until August 2006 China particularly the eastern coast was hit by a succession of storms and typhoons. The last one being the hardest to hit China in 50 years. Could I have information about this please? The delegate refers to typhoon Prapiroon. What information is available about that typhoon? 7. The delegate was of the view that military exercises would not be organised in typhoon season, particularly such a bad one. Is there any information to assist? RESPONSE 1. Is there corroborating information about military manoeuvres and exercises in Pingtan? 2. Is there any information specifically about the military exercise there in July 2006? There is a minor naval base in Pingtan and military manoeuvres are regularly held in the Taiwan Strait where Pingtan in located, especially in the June to August period.