Myths and Realities Outbreaks and Naturals Disasters
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Typhoon Neoguri Disaster Risk Reduction Situation Report1 DRR Sitrep 2014‐001 ‐ Updated July 8, 2014, 10:00 CET
Typhoon Neoguri Disaster Risk Reduction Situation Report1 DRR sitrep 2014‐001 ‐ updated July 8, 2014, 10:00 CET Summary Report Ongoing typhoon situation The storm had lost strength early Tuesday July 8, going from the equivalent of a Category 5 hurricane to a Category 3 on the Saffir‐Simpson Hurricane Wind Scale, which means devastating damage is expected to occur, with major damage to well‐built framed homes, snapped or uprooted trees and power outages. It is approaching Okinawa, Japan, and is moving northwest towards South Korea and the Philippines, bringing strong winds, flooding rainfall and inundating storm surge. Typhoon Neoguri is a once‐in‐a‐decade storm and Japanese authorities have extended their highest storm alert to Okinawa's main island. The Global Assessment Report (GAR) 2013 ranked Japan as first among countries in the world for both annual and maximum potential losses due to cyclones. It is calculated that Japan loses on average up to $45.9 Billion due to cyclonic winds every year and that it can lose a probable maximum loss of $547 Billion.2 What are the most devastating cyclones to hit Okinawa in recent memory? There have been 12 damaging cyclones to hit Okinawa since 1945. Sustaining winds of 81.6 knots (151 kph), Typhoon “Winnie” caused damages of $5.8 million in August 1997. Typhoon "Bart", which hit Okinawa in October 1999 caused damages of $5.7 million. It sustained winds of 126 knots (233 kph). The most damaging cyclone to hit Japan was Super Typhoon Nida (reaching a peak intensity of 260 kph), which struck Japan in 2004 killing 287 affecting 329,556 people injuring 1,483, and causing damages amounting to $15 Billion. -
Wang, M., M. Xue, and K. Zhao (2016), September 2008
PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE The impact of T-TREC-retrieved wind and radial 10.1002/2015JD024001 velocity data assimilation using EnKF Key Points: and effects of assimilation window • T-TREC-retrieved wind and radial velocity data are assimilated using an on the analysis and prediction ensemble Kalman filter • The relative impacts of two data sets of Typhoon Jangmi (2008) on analysis and prediction changes with assimilation windows Mingjun Wang1,2, Ming Xue1,2,3, and Kun Zhao1 • The combination of retrieved wind and radial velocity produces better 1Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Science, Nanjing University, Nanjing, analyses and forecasts China, 2Center for Analysis and Prediction of Storms, Norman, Oklahoma, USA, 3School of Meteorology, University of Oklahoma, Norman, Oklahoma, USA Correspondence to: M. Xue, Abstract This study examines the relative impact of assimilating T-TREC-retrieved winds (VTREC)versusradial [email protected] velocity (Vr) on the analysis and forecast of Typhoon Jangmi (2008) using an ensemble Kalman filter (EnKF). The VTREC and Vr data at 30 min intervals are assimilated into the ARPS model at 3 km grid spacing over four different Citation: assimilation windows that cover, respectively, 0000–0200, 0200–0400, 0400–0600, and 0000–0600 UTC, 28 Wang, M., M. Xue, and K. Zhao (2016), September 2008. The assimilation of VTREC data produces better analyses of the typhoon structure and intensity The impact of T-TREC-retrieved wind and radial velocity data assimilation than the assimilation of Vr data during the earlier assimilation windows, but during the later assimilation using EnKF and effects of assimilation windows when the coverage of Vr data on the typhoon from four Doppler radars is much improved, the window on the analysis and prediction assimilation of V outperforms V data. -
Philippines: Typhoon Fengshen
Emergency appeal n° MDRPH004 Philippines: GLIDE n° TC-2008-000093-PHL Operations update n° 4 31 December 2008 Typhoon Fengshen Period covered by this Ops Update: 24 September to 15 December 2008 Appeal target (current): CHF 8,310,213 (USD 8 million or EUR 5.1 million); with this Operations Update, the appeal has been revised to CHF 1,996,287 (USD 1,878,149 or EUR 1,343,281) <click here to view the attached Revised Emergency Appeal Budget> Appeal coverage: To date, the appeal is 87%. Funds are urgently needed to enable the Philippine National Red Cross to provide assistance to those affected by the typhoon.; <click here to go directly to the updated donor response A transitional shelter house in the midst of being built in the municipality of report, or here to link to contact Santa Barbara, Ilo Ilo province. Photo: Philippine National Red Cross. details > Appeal history: • A preliminary emergency appeal was launched on 24 June 2008 for CHF 8,310,213 (USD 8 million or EUR 5.1 million) for 12 months to assist 6,000 families. • Disaster Relief Emergency Fund (DREF): CHF 200,000 was allocated from the International Federation’s DREF. Summary: The onslaught of typhoon Fengshen which hit the Philippines on 18 June 2008, followed by floods and landslides, have left in its wake urgent needs among poverty-stricken communities. According to the National Disaster Coordinating Council (NDCC), approximately four million people have been affected through out the country by typhoon Fengshen. More than 81,000 houses were totally destroyed and a further 326,321 seriously damaged. -
The Influence of Assimilating Dropsonde Data on Typhoon Track
908 MONTHLY WEATHER REVIEW VOLUME 139 The Influence of Assimilating Dropsonde Data on Typhoon Track and Midlatitude Forecasts MARTIN WEISSMANN,* FLORIAN HARNISCH,* CHUN-CHIEH WU,1 PO-HSIUNG LIN,1 YOICHIRO OHTA,# KOJI YAMASHITA,# YEON-HEE KIM,@ EUN-HEE JEON,@ TETSUO NAKAZAWA,& AND SIM ABERSON** * Deutsches Zentrum fu¨r Luft- und Raumfahrt, Institut fu¨r Physik der Atmospha¨re, Oberpfaffenhofen, Germany 1 Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan # Japan Meteorological Agency, Tokyo, Japan @ National Institute of Meteorological Research, Korea Meteorological Agency, Seoul, South Korea & Meteorological Research Institute, Tsukuba, Japan ** NOAA/AOML/Hurricane Research Division, Miami, Florida (Manuscript received 9 February 2010, in final form 21 April 2010) ABSTRACT A unique dataset of targeted dropsonde observations was collected during The Observing System Re- search and Predictability Experiment (THORPEX) Pacific Asian Regional Campaign (T-PARC) in the autumn of 2008. The campaign was supplemented by an enhancement of the operational Dropsonde Ob- servations for Typhoon Surveillance near the Taiwan Region (DOTSTAR) program. For the first time, up to four different aircraft were available for typhoon observations and over 1500 additional soundings were collected. This study investigates the influence of assimilating additional observations during the two major typhoon events of T-PARC on the typhoon track forecast by the global models of the European Centre for Medium- Range Weather Forecasts (ECMWF), the Japan Meteorological Agency (JMA), the National Centers for Environmental Prediction (NCEP), and the limited-area Weather Research and Forecasting (WRF) model. Additionally, the influence of T-PARC observations on ECMWF midlatitude forecasts is investigated. All models show an improving tendency of typhoon track forecasts, but the degree of improvement varied from about 20% to 40% in NCEP and WRF to a comparably low influence in ECMWF and JMA. -
Disaster Preparedness Level, Graph Showed the Data in %, Developed on the Basis of Survey Conducted in Region Vi
2014 Figures Nature Begins Where Human Predication Ends Typhoon Frank (Fengshen) 17th to 27th June, 2008 Credit: National Institute of Geological Sciences, University of the Philippines, 2012 Tashfeen Siddique – Research Fellow AIM – Stephen Zuellig Graduate School of Development Management 8/15/2014 Nature Begins Where Human Predication Ends Contents Acronyms and Abbreviations: ...................................................................................................... iv Brief History ........................................................................................................................................ 1 Philippines Climate ........................................................................................................................... 2 Chronology of Typhoon Frank ....................................................................................................... 3 Forecasting went wrong .................................................................................................................. 7 Warning and Precautionary Measures ...................................................................................... 12 Typhoon Climatology-Science ..................................................................................................... 14 How Typhoon Formed? .............................................................................................................. 14 Typhoon Structure ..................................................................................................................... -
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. -
Science Discussion Started: 22 October 2018 C Author(S) 2018
Discussions Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2018-127 Earth System Manuscript under review for journal Earth Syst. Sci. Data Science Discussion started: 22 October 2018 c Author(s) 2018. CC BY 4.0 License. Open Access Open Data 1 Field Investigations of Coastal Sea Surface Temperature Drop 2 after Typhoon Passages 3 Dong-Jiing Doong [1]* Jen-Ping Peng [2] Alexander V. Babanin [3] 4 [1] Department of Hydraulic and Ocean Engineering, National Cheng Kung University, Tainan, 5 Taiwan 6 [2] Leibniz Institute for Baltic Sea Research Warnemuende (IOW), Rostock, Germany 7 [3] Department of Infrastructure Engineering, Melbourne School of Engineering, University of 8 Melbourne, Australia 9 ---- 10 *Corresponding author: 11 Dong-Jiing Doong 12 Email: [email protected] 13 Tel: +886 6 2757575 ext 63253 14 Add: 1, University Rd., Tainan 70101, Taiwan 15 Department of Hydraulic and Ocean Engineering, National Cheng Kung University 16 -1 Discussions Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2018-127 Earth System Manuscript under review for journal Earth Syst. Sci. Data Science Discussion started: 22 October 2018 c Author(s) 2018. CC BY 4.0 License. Open Access Open Data 1 Abstract 2 Sea surface temperature (SST) variability affects marine ecosystems, fisheries, ocean primary 3 productivity, and human activities and is the primary influence on typhoon intensity. SST drops 4 of a few degrees in the open ocean after typhoon passages have been widely documented; 5 however, few studies have focused on coastal SST variability. The purpose of this study is to 6 determine typhoon-induced SST drops in the near-coastal area (within 1 km of the coast) and 7 understand the possible mechanism. -
An Incoherent Subseasonal Pattern of Tropical Convective and Zonal Wind
An incoherent subseasonal pattern of tropical convective and zonal wind anomalies contributed to weak signals on both the Wheeler-Hendon (RMM) and CPC MJO indices during the past week. The spatial pattern of upper-level velocity potential anomalies exhibited influences from higher frequency modes, such as tropical cyclone activity over the eastern Pacific and anomalous divergence over Africa. During the past several days, however, these conflicting signals have weakened. Additionally, constructive interference of a strong equatorial Rossby Wave (ERW) and a Kelvin Wave over the eastern Indian Ocean and Maritime Continent contributed to an ongoing large area of enhanced convection. The RMM Index has responded to this evolution and is currently projecting a signal in Phase-4. Dynamical model MJO index forecasts are consistent with a rapid propagation of this signal eastward over the Maritime Continent during the upcoming week, likely due to influence from the Kelvin Wave. Beyond this period, however, the GFS weakens the MJO signal while the CFS, UKMET, and ECMWF models continue a slower eastward propagation over the western Pacific. There is uncertainty whether the enhanced convection over the Maritime Continent associated with the interactions between a more transient Kelvin Wave and the ERW will evolve into a more robust subseasonal signal on the MJO time scale. Due to the consensus among numerous dynamical models, however, impacts of MJO propagation from the Maritime Continent to the West Pacific were considered for this outlook. Tropical cyclones developed over both the eastern and western Pacific basins during the past week. Super Typhoon Neoguri, the third typhoon of 2014 and the first major cyclone, developed east of the Philippines on 3 July. -
Adversus Paganos: Disaster, Dragons, and Episcopal Authority in Gregory of Tours
Adversus paganos: Disaster, Dragons, and Episcopal Authority in Gregory of Tours David J. Patterson Comitatus: A Journal of Medieval and Renaissance Studies, Volume 44, 2013, pp. 1-28 (Article) Published by Center for Medieval and Renaissance Studies, UCLA DOI: 10.1353/cjm.2013.0000 For additional information about this article http://muse.jhu.edu/journals/cjm/summary/v044/44.patterson.html Access provided by University of British Columbia Library (29 Aug 2013 02:49 GMT) ADVERSUS PAGANOS: DISASTER, DRAGONS, AND EPISCOPAL AUTHORITY IN GREGORY OF TOURS David J. Patterson* Abstract: In 589 a great flood of the Tiber sent a torrent of water rushing through Rome. According to Gregory of Tours, the floodwaters carried some remarkable detritus: several dying serpents and, perhaps most strikingly, the corpse of a dragon. The flooding was soon followed by plague and the death of a pope. This remarkable chain of events leaves us with puzzling questions: What significance would Gregory have located in such a narrative? For a modern reader, the account (apart from its dragon) reads like a descrip- tion of a natural disaster. Yet how did people in the early Middle Ages themselves per- ceive such events? This article argues that, in making sense of the disasters at Rome in 589, Gregory revealed something of his historical consciousness: drawing on both bibli- cal imagery and pagan historiography, Gregory struggled to identify appropriate objects of both blame and succor in the wake of calamity. Keywords: plague, natural disaster, Gregory of Tours, Gregory the Great, Asclepius, pagan survivals, dragon, serpent, sixth century, Rome. In 589, a great flood of the Tiber River sent a torrent of water rushing through the city of Rome. -
Exposure and Vulnerability
Determinants of Risk: 2 Exposure and Vulnerability Coordinating Lead Authors: Omar-Dario Cardona (Colombia), Maarten K. van Aalst (Netherlands) Lead Authors: Jörn Birkmann (Germany), Maureen Fordham (UK), Glenn McGregor (New Zealand), Rosa Perez (Philippines), Roger S. Pulwarty (USA), E. Lisa F. Schipper (Sweden), Bach Tan Sinh (Vietnam) Review Editors: Henri Décamps (France), Mark Keim (USA) Contributing Authors: Ian Davis (UK), Kristie L. Ebi (USA), Allan Lavell (Costa Rica), Reinhard Mechler (Germany), Virginia Murray (UK), Mark Pelling (UK), Jürgen Pohl (Germany), Anthony-Oliver Smith (USA), Frank Thomalla (Australia) This chapter should be cited as: Cardona, O.D., M.K. van Aalst, J. Birkmann, M. Fordham, G. McGregor, R. Perez, R.S. Pulwarty, E.L.F. Schipper, and B.T. Sinh, 2012: Determinants of risk: exposure and vulnerability. In: Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation [Field, C.B., V. Barros, T.F. Stocker, D. Qin, D.J. Dokken, K.L. Ebi, M.D. Mastrandrea, K.J. Mach, G.-K. Plattner, S.K. Allen, M. Tignor, and P.M. Midgley (eds.)]. A Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). Cambridge University Press, Cambridge, UK, and New York, NY, USA, pp. 65-108. 65 Determinants of Risk: Exposure and Vulnerability Chapter 2 Table of Contents Executive Summary ...................................................................................................................................67 2.1. Introduction and Scope..............................................................................................................69 -
1 Looping Tracks Associated with Tropical Cyclones Approaching an Isolated 2 Mountain
1 Looping Tracks Associated with Tropical Cyclones Approaching an Isolated 2 Mountain. Part I: Essential Parameters 3 4 5 Yi-Chih Huang1,@ and Yuh-Lang Lin2,3 6 7 8 1 Research Center for Environmental Changes, Academia Sinica, 9 Taipei, Taiwan 10 2Department of Physics 11 3Department of Energy & Environmental Systems 12 North Carolina A&T State University 13 Greensboro, North Carolina 14 15 16 17 18 19 May 7, 2017 20 Submitted for publication 21 22 23 24 25 26 27 28 29 30 @Corresponding author address: Dr. Yi-Chih Huang, Research Center for Environmental 31 Changes, Academia Sinica, 128 Academia Road, Section 2, Nankang, Taipei, 115, 32 Taiwan. 33 Email: [email protected] 1 34 Abstract 35 Essential parameters for making a looping track when a westward-moving tropical 36 cyclone (TC) approaches a mesoscale mountain are investigated by examining several key 37 nondimensional control parameters with a series of systematic, idealized numerical 38 experiments, such as U/Nh, Vmax/Nh, U/fLx, Vmax/fR, h/Lx, and R/Ly. Here U is the 39 uniform zonal wind velocity, N the Brunt-Vaisala frequency, h the mountain height, f the 40 Coriolis parameter, the maximum tangential velocity at a radius of from the 41 cyclone center and Lx is the halfwidth of the mountain in the east-west direction. It is 42 found that looping tracks (a) tend to occur under small U/Nh and U/fLx, moderate h/Lx, 43 and large Vmax/Nh, which correspond to slow movement (leading to subgeostrophic flow 44 associated with strong orographic blocking), moderate steepness, and strong tangential 45 wind associated with TC vortex; (b) are often accompanied by an area of perturbation high 46 pressure to the northeast of the mountain, which lasts for only a short period; and (c) do 47 not require the existence of a northerly jet. -
A Vortex Relocation Scheme for Tropical Cyclone Initialization in Advanced Research WRF
3298 MONTHLY WEATHER REVIEW VOLUME 138 A Vortex Relocation Scheme for Tropical Cyclone Initialization in Advanced Research WRF LING-FENG HSIAO Central Weather Bureau, and Taiwan Typhoon and Flood Research Institute, Taipei, Taiwan CHI-SANN LIOU Naval Research Laboratory, Monterey, California TIEN-CHIANG YEH Central Weather Bureau, Taipei, Taiwan YONG-RUN GUO National Center for Atmospheric Research, Boulder, Colorado DER-SONG CHEN,KANG-NING HUANG,CHUEN-TEYR TERNG, AND JEN-HER CHEN Central Weather Bureau, Taipei, Taiwan (Manuscript received 6 November 2009, in final form 23 February 2010) ABSTRACT This paper introduces a relocation scheme for tropical cyclone (TC) initialization in the Advanced Research Weather Research and Forecasting (ARW-WRF) model and demonstrates its application to 70 forecasts of Ty- phoons Sinlaku (2008), Jangmi (2008), and Linfa (2009) for which Taiwan’s Central Weather Bureau (CWB) issued typhoon warnings. An efficient and dynamically consistent TC vortex relocation scheme for the WRF terrain- following mass coordinate has been developed to improve the first guess of the TC analysis, and hence improves the tropical cyclone initialization. The vortex relocation scheme separates the first-guess atmospheric flow into a TC circulation and environmental flow, relocates the TC circulation to its observed location, and adds the relocated TC circulation back to the environmental flow to obtain the updated first guess with a correct TC position. Analysis of these typhoon cases indicates that the relocation procedure moves the typhoon circulation to the observed typhoon position without generating discontinuities or sharp gradients in the first guess. Numerical experiments with and without the vortex relocation procedure for Typhoons Sinlaku, Jangmi, and Linfa forecasts show that about 67% of the first-guess fields need a vortex relocation to correct typhoon position errors while eliminates the topographical effect.