Estuarine and Coastal Natural Hazards: an Introduction and Synthesis
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
P1.24 a Typhoon Loss Estimation Model for China
P1.24 A TYPHOON LOSS ESTIMATION MODEL FOR CHINA Peter J. Sousounis*, H. He, M. L. Healy, V. K. Jain, G. Ljung, Y. Qu, and B. Shen-Tu AIR Worldwide Corporation, Boston, MA 1. INTRODUCTION the two. Because of its wind intensity (135 mph maximum sustained winds), it has been Nowhere 1 else in the world do tropical compared to Hurricane Katrina 2005. But Saomai cyclones (TCs) develop more frequently than in was short lived, and although it made landfall as the Northwest Pacific Basin. Nearly thirty TCs are a strong Category 4 storm and generated heavy spawned each year, 20 of which reach hurricane precipitation, it weakened quickly. Still, economic or typhoon status (cf. Fig. 1). Five of these reach losses were ~12 B RMB (~1.5 B USD). In super typhoon status, with windspeeds over 130 contrast, Bilis, which made landfall a month kts. In contrast, the North Atlantic typically earlier just south of where Saomai hit, was generates only ten TCs, seven of which reach actually only tropical storm strength at landfall hurricane status. with max sustained winds of 70 mph. Bilis weakened further still upon landfall but turned Additionally, there is no other country in the southwest and traveled slowly over a period of world where TCs strike with more frequency than five days across Hunan, Guangdong, Guangxi in China. Nearly ten landfalling TCs occur in a and Yunnan Provinces. It generated copious typical year, with one to two additional by-passing amounts of precipitation, with large areas storms coming close enough to the coast to receiving more than 300 mm. -
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. -
Observational Analysis of Tropical Cyclone Formation Associated with Monsoon Gyres
APRIL 2013 W U E T A L . 1023 Observational Analysis of Tropical Cyclone Formation Associated with Monsoon Gyres LIGUANG WU,HUIJUN ZONG, AND JIA LIANG Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, Nanjing, and State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing, China (Manuscript received 6 April 2012, in final form 31 October 2012) ABSTRACT Large-scale monsoon gyres and the involved tropical cyclone formation over the western North Pacific have been documented in previous studies. The aim of this study is to understand how monsoon gyres affect tropical cyclone formation. An observational study is conducted on monsoon gyres during the period 2000–10, with a focus on their structures and the associated tropical cyclone formation. A total of 37 monsoon gyres are identified in May–October during 2000–10, among which 31 monsoon gyres are accompanied with the formation of 42 tropical cyclones, accounting for 19.8% of the total tropical cyclone formation. Monsoon gyres are generally located on the poleward side of the composited monsoon trough with a peak occurrence in August–October. Extending about 1000 km outward from the center at lower levels, the cyclonic circulation of the composited monsoon gyre shrinks with height and is replaced with negative relative vorticity above 200 hPa. The maximum winds of the composited monsoon gyre appear 500–800 km away from 2 the gyre center with a magnitude of 6–10 m s 1 at 850 hPa. In agreement with previous studies, the com- posited monsoon gyre shows enhanced southwesterly flow and convection on the south-southeastern side. -
Boundary Layer Structure in Typhoon Saomai (2006): Understanding the Effects of Exchange Coefficient
Vol.18 No.2 JOURNAL OF TROPICAL METEOROLOGY June 2012 Article ID: 1006-8775(2012) 02-0195-12 BOUNDARY LAYER STRUCTURE IN TYPHOON SAOMAI (2006): UNDERSTANDING THE EFFECTS OF EXCHANGE COEFFICIENT 1 1 1 2 MING Jie (明 杰) , SONG Jin-jie (宋金杰) , CHEN Bao-jun (陈宝君) , WANG Ke-fa (王可发) (1. Key Laboratory of Mesoscale Severe Weather and School of Atmospheric Sciences, Nanjing University, Nanjing 210093 China; 2. Climate Center, Meteorological Bureau of Jiangsu Province, Nanjing 210008 China) Abstract: Recent studies have shown that surface fluxes and exchange coefficients are particularly important to models attempting to simulate the evolution and maintenance of hurricanes or typhoons. By using an advanced research version of the Weather Research and Forecasting (ARW) modeling system, this work aims to study the impact of modified exchange coefficient on the intensity and structures of typhoon Saomai (2006) over the western North Pacific. Numerical experiments with the modified and unmodified exchange coefficients are used to investigate the intensity and structure of the storm, especially the structures of the boundary layer within the storm. Results show that, compared to the unmodified experiment, the simulated typhoon in the modified experiment has a bigger deepening rate after 30-h and is the same as the observation in the last 12-h. The roughness is leveled off when wind speed is greater than 30 m/s. The momentum exchange coefficient (CD) and enthalpy exchange coefficient (CK) are leveled off too, and CD is decreased more than CK when wind speed is greater than 30 m/s. More sensible heat flux and less latent heat flux are produced. -
Ensemble Forecast of a Typhoon Flood Event
AUGUST 2001 MACKEY AND KRISHNAMURTI 399 Ensemble Forecast of a Typhoon Flood Event BRIAN P. M ACKEY AND T. N . K RISHNAMURTI Department of Meteorology, The Florida State University, Tallahassee, Florida (Manuscript received 9 September 1999, in ®nal form 2 February 2001) ABSTRACT A high-resolution nested regional spectral model and an ensemble prediction system are combined to forecast the track, intensity, and ¯ooding precipitation arising from Typhoon Winnie of August 1997, which eventually reached supertyphoon status. The prediction of ¯oods is operationally challenging since rainfall distributions can have a high degree of spatial and temporal variability. Rare event probabilities, however, can be estimated more readily via ensemble forecasting. This technique is used to evaluate a typhoon ¯ood event in which rainfall amounts greater than 200 mm led to landslides and major ¯ooding of crops. Seven-member ensembles were generated using an EOF-based technique. An experiment was conducted with a regional model resolution of 0.58 latitude. A Mercator transform grid with a grid mesh size of approximately 55 km in the east±west and 48 km in the north±south was employed. The results indicated very accurate track and intensity forecasts for both the control and ensemble mean. Track position errors remained below 150 km through 72 h, while intensity errors were approximately5ms21 at landfall. Qualitatively, the overall 5-day precipitation patterns appeared realistic and compared favorably with the observed data, while, quantitatively, the correlation coef®cient was near 0.6. For stations near and north of where Winnie made landfall, ensemble-based predictions performed well. While the ensemble mean often underestimated the heaviest rainfall totals by approximately 25%±50%, the maximum values within the ensemble spread either exceeded or came within 10%±15% of the station totals. -
The Use of a Spectral Nudging Technique to Determine the Impact of Environmental Factors on the Track of Typhoon Megi (2010)
atmosphere Article The Use of a Spectral Nudging Technique to Determine the Impact of Environmental Factors on the Track of Typhoon Megi (2010) Xingliang Guo ID and Wei Zhong * Institute of Meteorology and Oceanography, National University of Defense Technology, Nanjing 211101, China; [email protected] * Correspondence: [email protected] Received: 3 October 2017; Accepted: 7 December 2017; Published: 20 December 2017 Abstract: Sensitivity tests based on a spectral nudging (SN) technique are conducted to analyze the effect of large-scale environmental factors on the movement of typhoon Megi (2010). The error of simulated typhoon track is effectively reduced using SN and the impact of dynamical factors is more significant than that of thermal factors. During the initial integration and deflection period of Megi (2010), the local steering flow of the whole and lower troposphere is corrected by a direct large-scale wind adjustment, which improves track simulation. However, environmental field nudging may weaken the impacts of terrain and typhoon system development in the landfall period, resulting in large simulated track errors. Comparison of the steering flow and inner structure of the typhoon reveals that the large-scale circulation influences the speed and direction of typhoon motion by: (1) adjusting the local steering flow and (2) modifying the environmental vertical wind shear to change the location and symmetry of the inner severe convection. Keywords: spectral nudging; typhoon track; environmental factors 1. Introduction Although the forecasting accuracy of typhoon tracks has been effectively improved in recent years through observations, numerical simulations, data assimilation and studies of the physical mechanisms affecting typhoon movement [1], the accurate prediction of abnormal typhoon tracks, including their continuous changes and abrupt deflection, is still not possible [2]. -
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. -
Impact of Tropical Intraseasonal Oscillation on the Tracks of Tropical Cyclones in the Western North Pacific
Vol.20 No.1 JOURNAL OF TROPICAL METEOROLOGY March 2014 Article ID: 1006-8775(2014) 01-0026-09 IMPACT OF TROPICAL INTRASEASONAL OSCILLATION ON THE TRACKS OF TROPICAL CYCLONES IN THE WESTERN NORTH PACIFIC 1 2 TAO Li (陶 丽) , LI Shuang-jun (李双君) (1. Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, Nanjing 210044 China; 2. Wuhan Central Meteorological Observatory, Wuhan 430074 China) Abstract: In this work, an index of tropical 20-90 d oscillation (intra-seasonal oscillation; ISO) in the western North Pacific (WNP) was determined via the combined empirical orthogonal function (EOF) method using daily outgoing longwave radiation (OLR) field data from the National Oceanic and Atmospheric Administration (NOAA), daily wind field data (at 850 hPa) from the European Centre for Medium-Range Weather Forecasts (ECMWF) and referencing the Madden-Julian oscillation (MJO) index proposed by Wheeler and Hendon. An in-depth investigation was conducted to examine the impact of the ISO on changes in tropical cyclone (TC) tracks in the WNP during different ISO phases. The research results indicate that during the easterly phase of the ISO, under the impact of the northeastern airflow of anti-cyclonic ISO circulation, the easterly airflow south of the western Pacific subtropical high is relatively weak, and TCs generated in the subtropical high tend to change their tracks east of 140°E; during the westerly phase, there is a relatively high probability that TCs change their tracks west of 140°E. This work also analyzed the ISO flow field situation in cases of typhoons and determined that the track of a tropical cyclone will experience a sudden right turn when the center of the ISO cyclonic (anti-cyclonic) circulation coincides with that of the cyclone. -
Assimilation of GBVTD-Retrieved Winds from Single-Doppler Radar for Short-Term Forecasting of Super Typhoon Saomai (0608) at Landfall
Assimilation of GBVTD-Retrieved Winds from Single-Doppler Radar for Short-Term Forecasting of Super Typhoon Saomai (0608) at Landfall Kun Zhao1, 2, Ming Xue2,3 and Wen-Chau Lee4 1Key Laboratory for Mesoscale Severe Weather/MOE and School of Atmospheric Sciences, Nanjing University, Nanjing, 210093, China 2Center for Analysis and Prediction of Storms and 3School of Meteorology University of Oklahoma, Norman Oklahoma 73072 4Earth Observing Laboratory, National Center for Atmospheric Research*, Boulder, CO 80307 July, 2010 Revised and resubmitted in April 2011 Quarterly Journal of Royal Meteorological Society Corresponding author address: Ming Xue Center for Analysis and Prediction of Storms University of Oklahoma, 120 David L. Boren Blvd, Norman OK 73072 [email protected] *The National Center for Atmospheric Research is sponsored by the National Science Foundation. Abstract A single-Doppler wind retrieval method called the Ground-Based Velocity-Track Display technique (GBVTD) has been developed in recent years to retrieve horizontal circulations of tropical cyclones. The technique is able to retrieve axisymmetric tangential and radial winds, asymmetric tangential winds for wavenumbers 1 through 3, and along-beam mean winds in tropical cyclones. It has been successfully applied to tropical cyclone monitoring and warning. This study explores, for the first time, the assimilation of GBVTD-retrieved winds into a tropical cyclone prediction model, and examines its impact relative to that of directly assimilated radial velocity data. Super Typhoon Saomai (2006), the most intense landfalling typhoon ever recorded in China, is chosen as the test case, and data from the coastal operational radar at Wenzhou, China are used. The ARPS 3DVAR system is used to assimilate either the radial velocity data directly or the GBVTD-retrieved winds, at 30-min intervals for 2 hours. -
Sea Level Rise and Implications for Low-Lying Islands, Coasts and Communities
Sea Level Rise and Implications for Low-Lying Islands, SPM4 Coasts and Communities Coordinating Lead Authors: Michael Oppenheimer (USA), Bruce C. Glavovic (New Zealand/South Africa) Lead Authors: Jochen Hinkel (Germany), Roderik van de Wal (Netherlands), Alexandre K. Magnan (France), Amro Abd-Elgawad (Egypt), Rongshuo Cai (China), Miguel Cifuentes-Jara (Costa Rica), Robert M. DeConto (USA), Tuhin Ghosh (India), John Hay (Cook Islands), Federico Isla (Argentina), Ben Marzeion (Germany), Benoit Meyssignac (France), Zita Sebesvari (Hungary/Germany) Contributing Authors: Robbert Biesbroek (Netherlands), Maya K. Buchanan (USA), Ricardo Safra de Campos (UK), Gonéri Le Cozannet (France), Catia Domingues (Australia), Sönke Dangendorf (Germany), Petra Döll (Germany), Virginie K.E. Duvat (France), Tamsin Edwards (UK), Alexey Ekaykin (Russian Federation), Donald Forbes (Canada), James Ford (UK), Miguel D. Fortes (Philippines), Thomas Frederikse (Netherlands), Jean-Pierre Gattuso (France), Robert Kopp (USA), Erwin Lambert (Netherlands), Judy Lawrence (New Zealand), Andrew Mackintosh (New Zealand), Angélique Melet (France), Elizabeth McLeod (USA), Mark Merrifield (USA), Siddharth Narayan (US), Robert J. Nicholls (UK), Fabrice Renaud (UK), Jonathan Simm (UK), AJ Smit (South Africa), Catherine Sutherland (South Africa), Nguyen Minh Tu (Vietnam), Jon Woodruff (USA), Poh Poh Wong (Singapore), Siyuan Xian (USA) Review Editors: Ayako Abe-Ouchi (Japan), Kapil Gupta (India), Joy Pereira (Malaysia) Chapter Scientist: Maya K. Buchanan (USA) This chapter should be cited as: Oppenheimer, M., B.C. Glavovic , J. Hinkel, R. van de Wal, A.K. Magnan, A. Abd-Elgawad, R. Cai, M. Cifuentes-Jara, R.M. DeConto, T. Ghosh, J. Hay, F. Isla, B. Marzeion, B. Meyssignac, and Z. Sebesvari, 2019: Sea Level Rise and Implications for Low-Lying Islands, Coasts and Communities. -
Sea Level Rise and Implications for Low Lying Islands, Coasts And
SECOND ORDER DRAFT Chapter 4 IPCC SR Ocean and Cryosphere 1 2 Chapter 4: Sea Level Rise and Implications for Low Lying Islands, Coasts and Communities 3 4 Coordinating Lead Authors: Michael Oppenheimer (USA), Bruce Glavovic (New Zealand) 5 6 Lead Authors: Amro Abd-Elgawad (Egypt), Rongshuo Cai (China), Miguel Cifuentes-Jara (Costa Rica), 7 Rob Deconto (USA), Tuhin Ghosh (India), John Hay (Cook Islands), Jochen Hinkel (Germany), Federico 8 Isla (Argentina), Alexandre K. Magnan (France), Ben Marzeion (Germany), Benoit Meyssignac (France), 9 Zita Sebesvari (Hungary), AJ Smit (South Africa), Roderik van de Wal (Netherlands) 10 11 Contributing Authors: Maya Buchanan (USA), Gonéri Le Cozannet (France), Catia Domingues 12 (Australia), Petra Döll (Germany), Virginie K.E. Duvat (France), Tamsin Edwards (UK), Alexey Ekaykin 13 (Russian Federation), Miguel D. Fortes (Philippines), Thomas Frederikse (Netherlands), Jean-Pierre Gattuso 14 (France), Robert Kopp (USA), Erwin Lambert (Netherlands), Andrew Mackintosh (New Zealand), 15 Angélique Melet (France), Elizabeth McLeod (USA), Mark Merrifield (USA), Siddharth Narayan (US), 16 Robert J. Nicholls (UK), Fabrice Renaud (UK), Jonathan Simm (UK), Jon Woodruff (USA), Poh Poh Wong 17 (Singapore), Siyuan Xian (USA) 18 19 Review Editors: Ayako Abe-Ouchi (Japan), Kapil Gupta (India), Joy Pereira (Malaysia) 20 21 Chapter Scientist: Maya Buchanan (USA) 22 23 Date of Draft: 16 November 2018 24 25 Notes: TSU Compiled Version 26 27 28 Table of Contents 29 30 Executive Summary ......................................................................................................................................... 2 31 4.1 Purpose, Scope, and Structure of the Chapter ...................................................................................... 6 32 4.1.1 Themes of this Chapter ................................................................................................................... 6 33 4.1.2 Advances in this Chapter Beyond AR5 and SR1.5 ........................................................................ -
Causes of the Unusual Coastal Flooding Generated by Typhoon Winnie on the West Coast of Korea
Natural Hazards 29: 485–500, 2003. 485 © 2003 Kluwer Academic Publishers. Printed in the Netherlands. Causes of the Unusual Coastal Flooding Generated by Typhoon Winnie on the West Coast of Korea I.-J. MOON1,I.S.OH2,T.MURTY3 and Y.-H. YOUN4 1University of Rhode Island, Graduate School of Oceanography, Narragansett, RI 02882, U.S.A. (E-mail: [email protected]); 2Seoul National University, Department of Oceanography and Research Institute of Oceanography, Seoul 151-742, Korea; 3W. F. Baird & Associates, Coastal Engineers Ltd., Ottawa, Canada; 4Korea Meteorological Administration, Meteorological Research Institute, Seoul 151-742, Korea (Received: 30 October 2000; accepted: 11 February 2002) Abstract. On 19 August 1997 Typhoon Winnie brought unusually strong and extensive coastal flooding from storm surges to the west coast of Korea, which was far enough from the typhoon’s center to lack significant local wind and pressure forcing. Sea levels at some tidal stations broke 36-year records and resulted in property damages of $18,000,000. This study investigated the causes of the unusual high sea levels by using an Astronomical-Meteorological Index (AMI) and a coupled ocean wave-circulation model developed by the present authors. The AMI analysis and the numerical simulation of the surge event showed that the major cause of the high sea levels was not the standard inverse barometric effect supplemented by water piling up along the coast by the wind field of the typhoon as is usual for a typical storm surge, but rather an enhanced tidal forcing from the perigean spring tide and water transported into the Yellow Sea by the currents generated by the typhoon.