Philippines - Tropical Cyclones

Total Page:16

File Type:pdf, Size:1020Kb

Philippines - Tropical Cyclones 15 September 2014: Mexico – Philippines - Tropical Cyclones MEXICO - Tropical Cyclone ODILE PHILIPPINES, CHINA, VIETNAM - Tropical Cyclone KALMAEGI Storm surge (JRC) of 2.6 m max. US CHINA forecast for early 16 Sept. TAIWAN MEXICO Storm surge (JRC) of 1.1 m max. forecast late afternoon of 15 Sept. Luzon 15 Sep 06:00 UTC 120 km/h sust. winds 15 Sep 9:00 UTC VIET NAM 185 km/h sust. winds Legend Population Density (p/sq. km) LANDSCAN2007 PHILIPPINES MEXICO <VALUE> 0 • ODILE made landfall near Cabo San Lucas (Baja California Sur) on 15 September at 4.45 1 - 5 UTC with max. sustained winds of 205 km/h 6 - 25 (Category 3 Hurricane). 7 000 people are 26 - 50 PHILIPPINES, CHINA, VIETNAM reported evacuated and shelters for up to Legend 51 - 100 • Typhoon KALMAEGI (known in the Philippines as LUIS) 30 000 people have been set up. POP. DENSITY TRACK COLOURS made landfall on 14 September in northern Luzon, causing • As of 15 September 13.00 UTC local Media (pop/km101-2) 500 Tropical Depression flash floods and landslides. reports blocked roads and power cuts in the 501 - 2 500 Tropical Storm • According to NDRRMC (as of 15 September), three people area. 2 501 - 5 000 Typhoon were killed, another three were injured, 128 were rescued, • A Hurricane Warning is in effect for the whole WIND BUFFER 17 633 people were affected and displaced in northern southern half of the Baja California Peninsula. 5 001 - 130 000 64 km/h and central Luzon. • In the next 24h it is forecast to weaken while TRMM Last 7 days 92 km/h • KALMAEGI is currently passing over the South China Sea. moving over the southern part of Baja Acc. Rain (NASA) It is forecast to reach the coast of eastern Hainan and California Sur. Strong winds, storm surge and Strom surge (JRC) 119 km/h southern Guangdong early on 16 September; then heavy rains (150-300 mm up to 450 mm) 0.5 – 1.5 m Area of track uncertainty continue moving towards northern Vietnam. may affect the Baja California Peninsula. 1.5 – 2.6 m JRC calculations Storm Surge • Heavy rains, strong winds and storm surge may affect the (GDACS, NOAA, CONAGUA, Media) Affected Districts 1.0 – 2.0 m (*) Chinese provinces of Guangdong, Hainan, Guangxi and parts of northern Viet Nam on 16-17 September (see map). (GDACS, PAGASA, CMA, ).
Recommended publications
  • 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.
    [Show full text]
  • Member Report (Malaysia)
    MEMBER REPORT (MALAYSIA) ESCAP/WMO Typhoon Committee 15th Integrated Workshop Video Conference 1-2 December 2020 Organised by Viet Nam Table of Contents I. Overview of tropical cyclones which have affected/impacted Malaysia in 2020 1. Meteorological Assessment (highlighting forecasting issues/impacts) 2. Hydrological Assessment (highlighting water-related issues/impact) (a) Flash flood in Kajang & Kuala Lumpur in July and September 2020 (b) Enhancement of Hydrological Data Management for DID Malaysia (c) Hydrological Instrumentation Updates for Malaysia (d) Drought Monitoring Updates 3. Socio-Economic Assessment (highlighting socio-economic and DRR issues/impacts) 4. Regional Cooperation Assessment (highlighting regional cooperation successes and challenges) II. Summary of progress in Priorities supporting Key Result Areas 1. Annual Operating Plan (AOP) for Working Group of Meteorology [AOP4: Radar Integrated Nowcasting System (RaINS)] 2. Annual Operating Plan (AOP) for Working Group of Hydrology (AOP2, AOP4, AOP5, AOP6) 3. The Government of Malaysia’s Commitment Towards Supporting the Sendai Framework for Disaster Risk Reduction I. Overview of tropical cyclones which have affected/impacted Malaysia in 2020 1. Meteorological Assessment (highlighting forecasting issues/impacts) During the period of 1 November 2019 to 31 October 2020, 27 tropical cyclones (TCs) formed over the Western Pacific Ocean, the Philippines waters as well as the South China Sea. Eight of the TCs entered the area of responsibility of the Malaysian Meteorological Department (MET Malaysia) as shown in Figure 1. The TCs, which consisted of seven typhoons and a tropical storm that required the issuance of strong winds and rough seas warnings over the marine regions under the responsibility of MET Malaysia, are listed in Table 1.
    [Show full text]
  • TUESDAY 16* Philippines 3,479* 1,167*
    TUESDAY TYPHOON KALMAEGI 19 NOV 2019 PHILIPPINES 1230 HRS (UTC +7) FLASH UPDATE #2 Population Exposed (Estimated exposure by the PDC) Map source: Philippines Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) Initial Effects* *Estimations are based on data reported/confirmed by National Disaster 3,479* 1,167* 15* 16* Management Organisations of each AFFECTED DISPLACED FLOODED DAMAGED respective ASEAN Member State PERSONS PERSONS BARANGAYS HOUSES and other verified sources Philippines • Tropical Storm KALMAEGI (locally named RAMON in the Philippines), which strengthened into a Severe Tropical Storm on 18 November 2019, has now further developed into a Typhoon and currently moving slowly west-northwest towards Babuyan Islands, north of Luzon, Philippines as of 10:00 (UTC+7). • According to forecast by the Joint Typhoon Warning Center (JTWC), Typhoon KALMAEGI is moving at about 4 kph, and is expected to weaken over the next 24 hours. Based on the current forecast (the storm's center and path), the Typhoon is within 112 km from northern seaboard of the Philippines, and the center is expected to make landfall in the afternoon or evening today, 19 November 2019, with sustained winds of about 148 kph. • The Philippines Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) stated that moderate with frequent heavy rains will prevail over Batanes, northern portion of Cagayan (including the Babuyan Islands), Apayao and the northern portion of Ilocos Norte provinces. • The Philippines’ National Disaster Risk Reduction Management Council (NDRRMC) reported flood incidents, ranging from 0.5m to 1m of flood water, in 15 barangays/villages in Camarines Sur and Romblon provinces due to persistent heavy rains associated with the typhoon.
    [Show full text]
  • Upper Ocean Response to Typhoon Kalmaegi and Sarika in the South China Sea from Multiple-Satellite Observations and Numerical Simulations
    remote sensing Article Upper Ocean Response to Typhoon Kalmaegi and Sarika in the South China Sea from Multiple-Satellite Observations and Numerical Simulations Xinxin Yue 1, Biao Zhang 1,* ID , Guoqiang Liu 1,2, Xiaofeng Li 3 ID , Han Zhang 4 and Yijun He 1 ID 1 School of Marine Sciences, Nanjing University of Information Science and Technology, Nanjing 210044, China; [email protected] (X.Y.); [email protected] (G.L.); [email protected] (Y.H.) 2 Bedford Institute of Oceanography, Fisheries and Oceans, Dartmouth, NS B2Y 4A2, Canada 3 GST at National Oceanic and Atmospheric Administration (NOAA)/NESDIS, College Park, MD 20740-3818, USA; [email protected] 4 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Hangzhou 310012, China; [email protected] * Correspondence: [email protected] Received: 12 December 2017; Accepted: 22 February 2018; Published: 24 February 2018 Abstract: We investigated ocean surface and subsurface physical responses to Typhoons Kalmaegi and Sarika in the South China Sea, utilizing synergistic multiple-satellite observations, in situ measurements, and numerical simulations. We found significant typhoon-induced sea surface cooling using satellite sea surface temperature (SST) observations and numerical model simulations. This cooling was mainly caused by vertical mixing and upwelling. The maximum amplitudes were 6 ◦C and 4.2 ◦C for Typhoons Kalmaegi and Sarika, respectively. For Typhoon Sarika, Argo temperature profile measurements showed that temperature response beneath the surface showed a three-layer vertical structure (decreasing-increasing-decreasing). Satellite salinity observations showed that the maximum increase of sea surface salinity (SSS) was 2.2 psu on the right side of Typhoon Sarika’s track, and the maximum decrease of SSS was 1.4 psu on the left.
    [Show full text]
  • Origin and Maintenance of the Long-Lasting, Outer Mesoscale Convective System in Typhoon Fengshen (2008)
    2838 MONTHLY WEATHER REVIEW VOLUME 142 Origin and Maintenance of the Long-Lasting, Outer Mesoscale Convective System in Typhoon Fengshen (2008) BUO-FU CHEN Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan RUSSELL L. ELSBERRY Department of Meteorology, Naval Postgraduate School, Monterey, California CHENG-SHANG LEE Department of Atmospheric Sciences, National Taiwan University, and Taiwan Typhoon and Flood Research Institute, National Applied Research Laboratories, Taipei, Taiwan (Manuscript received 27 January 2014, in final form 21 March 2014) ABSTRACT Outer mesoscale convective systems (OMCSs) are long-lasting, heavy rainfall events separate from the inner-core rainfall that have previously been shown to occur in 22% of western North Pacific tropical cyclones (TCs). Environmental conditions accompanying the development of 62 OMCSs are contrasted with the conditions in TCs that do not include an OMCS. The development, kinematic structure, and maintenance mechanisms of an OMCS that occurred to the southwest of Typhoon Fengshen (2008) are studied with Weather Research and Forecasting Model simulations. Quick Scatterometer (QuikSCAT) observations and the simulations indicate the low-level TC circulation was deflected around the Luzon terrain and caused an elongated, north–south moisture band to be displaced to the west such that the OMCS develops in the outer region of Fengshen rather than spiraling into the center. Strong northeasterly vertical wind shear contributed to frictional convergence in the boundary layer, and then the large moisture flux convergence in this moisture band led to the downstream development of the OMCS when the band interacted with the monsoon flow. As the OMCS developed in the region of low-level monsoon westerlies and midlevel northerlies associated with the outer circulation of Fengshen, the characteristic structure of a rear-fed inflow with a leading stratiform rain area in the cross-line direction (toward the south) was established.
    [Show full text]
  • The Impact of Dropwindsonde on Typhoon Track Forecasts in DOTSTAR and T-PARC
    1 Eyewall Evolution of Typhoons Crossing the Philippines and Taiwan: An 2 Observational Study 3 Kun-Hsuan Chou1, Chun-Chieh Wu2, Yuqing Wang3, and Cheng-Hsiang Chih4 4 1Department of Atmospheric Sciences, Chinese Culture University, Taipei, Taiwan 5 2Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan 6 3International Pacific Research Center, and Department of Meteorology, University of 7 Hawaii at Manoa, Honolulu, Hawaii 8 4Graduate Institute of Earth Science/Atmospheric Science, Chinese Culture University, 9 Taipei, Taiwan 10 11 12 13 14 Terrestrial, Atmospheric and Oceanic Sciences 15 (For Special Issue on “Typhoon Morakot (2009): Observation, Modeling, and 16 Forecasting Applications”) 17 (Accepted on 10 May, 2011) 18 19 ___________________ 20 Corresponding Author’s address: Kun-Hsuan Chou, Department of Atmospheric Sciences, 21 National Taiwan University, 55, Hwa-Kang Road, Yang-Ming-Shan, Taipei 111, Taiwan. 22 ([email protected]) 1 23 Abstract 24 This study examines the statistical characteristics of the eyewall evolution induced by 25 the landfall process and terrain interaction over Luzon Island of the Philippines and Taiwan. 26 The interesting eyewall evolution processes include the eyewall expansion during landfall, 27 followed by contraction in some cases after re-emergence in the warm ocean. The best 28 track data, advanced satellite microwave imagers, high spatial and temporal 29 ground-observed radar images and rain gauges are utilized to study this unique eyewall 30 evolution process. The large-scale environmental conditions are also examined to 31 investigate the differences between the contracted and non-contracted outer eyewall cases 32 for tropical cyclones that reentered the ocean.
    [Show full text]
  • 2008 Tropical Cyclone Review Summarises Last Year’S Global Tropical Cyclone Activity and the Impact of the More Significant Cyclones After Landfall
    2008 Tropical Cyclone 09 Review TWO THOUSAND NINE Table of Contents EXECUTIVE SUMMARY 1 NORTH ATLANTIC BASIN 2 Verification of 2008 Atlantic Basin Tropical Cyclone Forecasts 3 Tropical Cyclones Making US Landfall in 2008 4 Significant North Atlantic Tropical Cyclones in 2008 5 Atlantic Basin Tropical Cyclone Forecasts for 2009 15 NORTHWEST PACIFIC 17 Verification of 2008 Northwest Pacific Basin Tropical Cyclone Forecasts 19 Significant Northwest Pacific Tropical Cyclones in 2008 20 Northwest Pacific Basin Tropical Cyclone Forecasts for 2009 24 NORTHEAST PACIFIC 25 Significant Northeast Pacific Tropical Cyclones in 2008 26 NORTH INDIAN OCEAN 28 Significant North Indian Tropical Cyclones in 2008 28 AUSTRALIAN BASIN 30 Australian Region Tropical Cyclone Forecasts for 2009/2010 31 Glossary of terms 32 FOR FURTHER DETAILS, PLEASE CONTACT [email protected], OR GO TO OUR CAT CENTRAL WEBSITE AT HTTP://WWW.GUYCARP.COM/PORTAL/EXTRANET/INSIGHTS/CATCENTRAL.HTML Tropical Cyclone Report 2008 Guy Carpenter ■ 1 Executive Summary The 2008 Tropical Cyclone Review summarises last year’s global tropical cyclone activity and the impact of the more significant cyclones after landfall. Tropical 1 cyclone activity is reviewed by oceanic basin, covering those that developed in the North Atlantic, Northwest Pacific, Northeast Pacific, North Indian Ocean and Australia. This report includes estimates of the economic and insured losses sus- tained from each cyclone (where possible). Predictions of tropical cyclone activity for the 2009 season are given per oceanic basin when permitted by available data. In the North Atlantic, 16 tropical storms formed during the 2008 season, compared to the 1950 to 2007 average of 9.7,1 an increase of 65 percent.
    [Show full text]
  • Resilience of Human Mobility Under the Influence of Typhoons
    Available online at www.sciencedirect.com ScienceDirect Procedia Engineering 118 ( 2015 ) 942 – 949 International Conference on Sustainable Design, Engineering and Construction Resilience of human mobility under the influence of typhoons Qi Wanga, John E. Taylor b,* a Charles E. Via, Jr. Department of Civil and Environmental Engineering, 121 Patton Hall, Blacksburg, VA 24060, U.S.A b Charles E. Via, Jr. Department of Civil and Environmental Engineering, 113 Patton Hall, Blacksburg, VA 24060, U.S.A Abstract Climate change has intensified tropical cyclones, resulting in several recent catastrophic hurricanes and typhoons. Such disasters impose threats on populous coastal urban areas, and therefore, understanding and predicting human movements plays a critical role in evaluating vulnerability and resilience of human society and developing plans for disaster evacuation, response and relief. Despite its critical role, limited research has focused on tropical cyclones and their influence on human mobility. Here, we studied how severe tropical storms could influence human mobility patterns in coastal urban populations using individuals’ movement data collected from Twitter. We selected 5 significant tropical storms and examined their influences on 8 urban areas. We analyzed the human movement data before, during, and after each event, comparing the perturbed movement data to movement data from steady states. We also used different statistical analysis approaches to quantify the strength and duration of human mobility perturbation. The results suggest that tropical cyclones can significantly perturb human movements, and human mobility experienced different magnitudes in different cases. We also found that power-law still governed human movements in spite of the perturbations. The findings from this study will deepen our understanding about the interaction between urban dwellers and civil infrastructure, improve our ability to predict human movements during natural disasters, and help policymakers to improve disaster evacuation, response and relief plans.
    [Show full text]
  • Tropical Cyclones 2019
    << LINGLING TRACKS OF TROPICAL CYCLONES IN 2019 SEP (), !"#$%&'( ) KROSA AUG @QY HAGIBIS *+ FRANCISCO OCT FAXAI AUG SEP DANAS JUL ? MITAG LEKIMA OCT => AUG TAPAH SEP NARI JUL BUALOI SEPAT OCT JUN SEPAT(1903) JUN HALONG NOV Z[ NEOGURI OCT ab ,- de BAILU FENGSHEN FUNG-WONG AUG NOV NOV PEIPAH SEP Hong Kong => TAPAH (1917) SEP NARI(190 6 ) MUN JUL JUL Z[ NEOGURI (1920) FRANCISCO (1908) :; OCT AUG WIPHA KAJIK() 1914 LEKIMA() 1909 AUG SEP AUG WUTIP *+ MUN(1904) WIPHA(1907) FEB FAXAI(1915) JUL JUL DANAS(190 5 ) de SEP :; JUL KROSA (1910) FUNG-WONG (1927) ./ KAJIKI AUG @QY @c NOV PODUL SEP HAGIBIS() 1919 << ,- AUG > KALMAEGI OCT PHANFONE NOV LINGLING() 1913 BAILU()19 11 \]^ ./ ab SEP AUG DEC FENGSHEN (1925) MATMO PODUL() 191 2 PEIPAH (1916) OCT _` AUG NOV ? SEP HALONG (1923) NAKRI (1924) @c MITAG(1918) NOV NOV _` KALMAEGI (1926) SEP NAKRI KAMMURI NOV NOV DEC \]^ MATMO (1922) OCT BUALOI (1921) KAMMURI (1928) OCT NOV > PHANFONE (1929) DEC WUTIP( 1902) FEB 二零一 九 年 熱帶氣旋 TROPICAL CYCLONES IN 2019 2 二零二零年七月出版 Published July 2020 香港天文台編製 香港九龍彌敦道134A Prepared by: Hong Kong Observatory 134A Nathan Road Kowloon, Hong Kong © 版權所有。未經香港天文台台長同意,不得翻印本刊物任何部分內容。 © Copyright reserved. No part of this publication may be reproduced without the permission of the Director of the Hong Kong Observatory. 本刊物的編製和發表,目的是促進資 This publication is prepared and disseminated in the interest of promoting 料交流。香港特別行政區政府(包括其 the exchange of information. The 僱員及代理人)對於本刊物所載資料 Government of the Hong Kong Special 的準確性、完整性或效用,概不作出 Administrative Region
    [Show full text]
  • Response of Coastal Water in the Taiwan Strait to Typhoon Nesat of 2017
    water Article Response of Coastal Water in the Taiwan Strait to Typhoon Nesat of 2017 Renhao Wu 1,2 , Qinghua Yang 1,3 , Di Tian 4, Bo Han 1,2, Shimei Wu 1,2 and Han Zhang 4,* 1 School of Atmospheric Sciences, and Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Zhuhai 519082, China; [email protected] (R.W.); [email protected] (Q.Y.); [email protected] (B.H.); [email protected] (S.W.) 2 Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China 3 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100039, China 4 State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China; [email protected] * Correspondence: [email protected] Received: 29 September 2019; Accepted: 4 November 2019; Published: 7 November 2019 Abstract: The oceanic response of the Taiwan Strait (TWS) to Typhoon Nesat (2017) was investigated using a fully coupled atmosphere-ocean-wave model (COAWST) verified by observations. Ocean currents in the TWS changed drastically in response to significant wind variation during the typhoon. The response of ocean currents was characterised by a flow pattern generally consistent with the Ekman boundary layer theory, with north-eastward volume transport being significantly modified by the storm. Model results also reveal that the western TWS experienced the maximum generated storm surge, whereas the east side experienced only moderate storm surge.
    [Show full text]
  • Member Report
    MEMBER REPORT ESCAP/WMO Typhoon Committee 9th IWS SOCIALIST REPUBLIC OF VIET NAM 20 - 24 October 2014 ESCAP-UN Conference Center, Bangkok, Thailand CONTENTS I. Overview of tropical cyclones which have affected/impacted Member’s area since the last Typhoon Committee Session ............................................................ 1 1. Meteorological assessment .................................................................................. 1 1.1. Typhoon Rammasun (1409) ............................................................................ 1 1.2. Typhoon Kalmaegi (1415) .............................................................................. 2 2. Hydrological Assessment ..................................................................................... 2 2.1. Flood situations by Tropical cyclone in the North ......................................... 3 2.2. Flood situations by Tropical cyclone in the Central and Highland area ......... 6 3. Socio-Economic Assessment ................................................................................ 6 3.1. Damage Situation in 2013 ............................................................................... 6 3.2. Damage Situation in 2012 ............................................................................... 6 3.3. Damage Situation in 2011 ............................................................................... 7 II. Summary of progress in Key Result Areas ....................................................... 7 III. Update of Members’ Working Groups representatives
    [Show full text]
  • Prediction of Overbank Flows with Coupling 1D Flash Flood Routing Model and 3D Coastal Ocean Model
    Prediction of Overbank Flows with Coupling 1D Flash Flood Routing Model and 3D Coastal Ocean Model Prof. Wen-Cheng Liu Department of Civil and Disaster Prevention Engineering, National United University, Miaoli Taiwan Taiwan Typhoon and Flood Research Institute National Applied Research Laboratories, Taipei Taiwan September 7, 2013 Outline Introduction Description of study site Methodology Model calibration and verification Model applications Conclusions 2 Introduction Taiwan is located at the intersection of the Euro- Asian continent and the Pacific Ocean, and it suffers from typhoons during summer and fall seasons. Annual rainfall: 2500mm The categorized paths of typhoon’s low-pressure center passed Taiwan from 1987 to 2007. 3 Introduction Over the past years, Taiwan has experienced several severe flood disasters involving major river basins. One of important feature is the overtopping levees at upriver reaches due to extremely rainfall during typhoons events. Typhoon Nair 4 (2001) Introduction It is common practice to apply different modeling system for coastal waters and river system in hydrodynamic modeling community. 3D models are designed for the horizontal and vertical variability in coastal waters, while 1D river models are designed to accurately represent complicated river geometries. 5 Purpose To deal with the complicated river and coastal ocean interaction, a 3D coastal ocean model coupled with a 1D river system model is proposed for simulating the overbank discharge hydrographs under Typhoon Kalmaegi (2008) hit central Taiwan. Schematic diagram of the coupling of 1D-3D models. 6 Description of study site The Wu River system includes mainstem of Wu River and main tributaries, Fazi River, Dali river, Han River, and Maoluo River.
    [Show full text]