Assessing Typhoon-Induced Canopy Damage Using Vegetation Indices in the Fushan Experimental Forest, Taiwan
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Integrating Spatial, Temporal, and Size Probabilities for the Annual Landslide Hazard Maps in the Shihmen Watershed, Taiwan
Open Access Nat. Hazards Earth Syst. Sci., 13, 2353–2367, 2013 Natural Hazards www.nat-hazards-earth-syst-sci.net/13/2353/2013/ doi:10.5194/nhess-13-2353-2013 and Earth System © Author(s) 2013. CC Attribution 3.0 License. Sciences Integrating spatial, temporal, and size probabilities for the annual landslide hazard maps in the Shihmen watershed, Taiwan C. Y. Wu and S. C. Chen Department of Soil and Water Conservation, National Chung-Hsing University, Taichung 40227, Taiwan Correspondence to: S. C. Chen ([email protected]) Received: 23 February 2013 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 19 March 2013 Revised: 13 August 2013 – Accepted: 13 August 2013 – Published: 25 September 2013 Abstract. Landslide spatial, temporal, and size probabilities susceptible to landslides, and heavy rainfall during typhoons were used to perform a landslide hazard assessment in this or storms have indeed caused large landslides of loosened study. Eleven intrinsic geomorphological, and two extrinsic soil (Wu and Chen, 2009). Furthermore, climate change en- rainfall factors were evaluated as landslide susceptibility re- larges bare land areas, thereby increasing the frequency of lated factors as they related to the success rate curves, land- landslides in Taiwan (Chen and Huang, 2010). Because of slide ratio plots, frequency distributions of landslide and non- the uncertainties associated with natural disasters, risk man- landslide groups, as well as probability–probability plots. agement is necessary to minimize losses (Chen et al., 2010). Data on landslides caused by Typhoon Aere in the Shihmen In view of the growing emphasis on risk management in dis- watershed were selected to train the susceptibility model. -
Dependence of Probabilistic Quantitative Precipitation Forecast Performance on Typhoon Characteristics and Forecast Track Error in Taiwan
APRIL 2020 T E N G E T A L . 585 Dependence of Probabilistic Quantitative Precipitation Forecast Performance on Typhoon Characteristics and Forecast Track Error in Taiwan HSU-FENG TENG AND JAMES M. DONE National Center for Atmospheric Research, Boulder, Colorado CHENG-SHANG LEE Department of Atmospheric Sciences, National Taiwan University, Taipei, Taiwan YING-HWA KUO National Center for Atmospheric Research, and University Corporation for Atmospheric Research, Boulder, Colorado (Manuscript received 15 August 2019, in final form 7 January 2020) ABSTRACT This study investigates the probabilistic quantitative precipitation forecast (PQPF) performance of ty- phoons that affected Taiwan during 2011–16. In this period, a total of 19 typhoons with a land warning issued by the Central Weather Bureau (CWB) are analyzed. The PQPF is calculated using the ensemble precipi- tation forecast data from the Taiwan Cooperative Precipitation Ensemble Forecast Experiment (TAPEX), and the verification data, verification thresholds, and typhoon characteristics are obtained from the CWB. The overall PQPF performance of TAPEX has an acceptable reliability and discrimination ability, and the higher probability error is distributed at the mountainous area of Taiwan. The PQPF performance is significantly influenced by typhoon characteristics (e.g., typhoon tracks, sizes, and forward speeds). The PQPFs for westward-moving, large, or slow typhoons have higher reliability and discrimination ability, and lower- probability error than those for northward-moving, small, or fast typhoons, except for similar reliability between fast and slow typhoons. Because northward-moving or small typhoons have larger forecast track error, and their PQPF performance is sensitive to the accuracy of the forecast track, a higher probability error occurs than that for westward-moving or large typhoons. -
Understanding Disaster Risk ~ Lessons from 2009 Typhoon Morakot, Southern Taiwan
Understanding disaster risk ~ Lessons from 2009 Typhoon Morakot, Southern Taiwan Wen–Chi Lai, Chjeng-Lun Shieh Disaster Prevention Research Center, National Cheng-Kung University 1. Introduction 08/10 Rainfall 08/07 Rainfall started & stopped gradually typhoon speed decrease rapidly 08/06 Typhoon Warning for Inland 08/03 Typhoon 08/05 Typhoon Morakot warning for formed territorial sea 08/08 00:00 Heavy rainfall started 08/08 12:00 ~24:00 Rainfall center moved to south Taiwan, which triggered serious geo-hazards and floodings Data from “http://weather.unisys.com/” 1. Introduction There 4 days before the typhoon landing and forecasting as weakly one for norther Taiwan. Emergency headquarters all located in Taipei and few raining around the landing area. The induced strong rainfalls after typhoon leaving around southern Taiwan until Aug. 10. The damages out of experiences crush the operation system, made serious impacts. Path of the center of Typhoon Morakot 1. Introduction Largest precipitation was 2,884 mm Long duration (91 hours) Hard to collect the information High intensity (123 mm/hour) Large depth (3,000 mm-91 hour) Broad extent (1/4 of Taiwan) The scale and type of the disaster increasing with the frequent appearance of extreme weather Large-scale landslide and compound disaster become a new challenge • Area:202 ha Depth:84 meter Volume: 24 million m3 2.1 Root Cause and disaster risk drivers 3000 Landslide Landslide (Shallow, Soil) (Deep, Bedrock) Landslide dam break Flood Debris flow Landslide dam form Alisan Station ) 2000 -
On the Extreme Rainfall of Typhoon Morakot (2009)
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, D05104, doi:10.1029/2010JD015092, 2011 On the extreme rainfall of Typhoon Morakot (2009) Fang‐Ching Chien1 and Hung‐Chi Kuo2 Received 21 September 2010; revised 17 December 2010; accepted 4 January 2011; published 4 March 2011. [1] Typhoon Morakot (2009), a devastating tropical cyclone (TC) that made landfall in Taiwan from 7 to 9 August 2009, produced the highest recorded rainfall in southern Taiwan in the past 50 years. This study examines the factors that contributed to the heavy rainfall. It is found that the amount of rainfall in Taiwan was nearly proportional to the reciprocal of TC translation speed rather than the TC intensity. Morakot’s landfall on Taiwan occurred concurrently with the cyclonic phase of the intraseasonal oscillation, which enhanced the background southwesterly monsoonal flow. The extreme rainfall was caused by the very slow movement of Morakot both in the landfall and in the postlandfall periods and the continuous formation of mesoscale convection with the moisture supply from the southwesterly flow. A composite study of 19 TCs with similar track to Morakot shows that the uniquely slow translation speed of Morakot was closely related to the northwestward‐extending Pacific subtropical high (PSH) and the broad low‐pressure systems (associated with Typhoon Etau and Typhoon Goni) surrounding Morakot. Specifically, it was caused by the weakening steering flow at high levels that primarily resulted from the weakening PSH, an approaching short‐wave trough, and the northwestward‐tilting Etau. After TC landfall, the circulation of Goni merged with the southwesterly flow, resulting in a moisture conveyer belt that transported moisture‐laden air toward the east‐northeast. -
Shear Banding
2020-1065 IJOI http://www.ijoi-online.org/ THE MAJOR CAUSE OF BRIDGE COLLAPSES ACROSS ROCK RIVERBEDS: SHEAR BANDING Tse-Shan Hsu Professor, Department of Civil Engineering, Feng-Chia University President, Institute of Mitigation for Earthquake Shear Banding Disasters Taiwan, R.O.C. [email protected] Po Yen Chuang Ph.D Program in Civil and Hydraulic Engineering Feng-Chia University, Taiwan, R.O.C. Kuan-Tang Shen Secretary-General, Institute of Mitigation for Earthquake Shear Banding Disasters Taiwan, R.O.C. Fu-Kuo Huang Associate Professor, Department of Water Resources and Environmental Engineering Tamkang University, Taiwan, R.O.C. Abstract Current performance design codes require that bridges be designed that they will not col- lapse within their design life. However, in the past twenty five years, a large number of bridges have collapsed in Taiwan, with their actual service life far shorter than their de- sign life. This study explores the major cause of the collapse of many these bridges. The results of the study reveal the following. (1) Because riverbeds can be divided into high shear strength rock riverbeds and low shear strength soil riverbeds, the main cause of bridge collapse on a high shear strength rock riverbed is the shear band effect inducing local brittle fracture of the rock, and the main cause on a low shear strength soil riverbed is scouring, but current bridge design specifications only fortify against the scouring of low shear strength soil riverbeds. (2) Since Taiwan is mountainous, most of the collapsed bridges cross high shear strength rock riverbeds in mountainous areas and, therefore, the major cause of collapse of bridges in Taiwan is that their design does not consider the 180 The International Journal of Organizational Innovation Volume 13 Number 1, July 2020 2020-1065 IJOI http://www.ijoi-online.org/ shear band effect. -
Utlizing Multi-Scale Remote Sensing Technology for Evalutaing Sediment Disaster in the Catchment Area
2012 International Conference on Earth Science and Remote Sensing (ESRS 2012) Utlizing Multi-scale Remote Sensing Technology for Evalutaing Sediment Disaster in the Catchment Area Chun-Kai Chen1, Cheng-Yang Hsiao 2, Bor-Shiun Lin 2, Chin-Tung Cheng2 1 2 Disaster Prevention Technology Research Center, Sinotech Engineering Consultants, INC., Taipei, Taiwan, 1 [email protected] Keywords: Multi-scale remote sensing, change process of landslides , 3D Web-GIS. Abstract.This study combines multi-scale remote sensing imagery and intelligence gathering to investigate water catchment area environment. Temporal telemetry information combined with object-oriented technology is used to create a semi-automated algorithm for identifying landslide location and area. Through this process, landslide changes on a watershed scale are explored. This study also demonstrates the use of air-borne LiDAR technology for conservation treatment project effectiveness evaluation. 1. Introduction With rapid advances in satellite remote sensing, image processing and data storage in recent years, remote sensing images have provided new methods for performing photogramtric surveys, landuse monitoring and natural disaster reconnaissance. Natural disaster reconnaissance objectives can include identifying changes in the natural environment, land topography, public facilities, or transportation structures. Remote sensing data, processed with image analysis techniques can serve as a tool for environmental assessments and contribute to environmental protection and conservation work. Using multi-scale remote sensing tools for fast, automated surveys and can break through access features not accessible by field reconnaissance survey such as the wide area of the landslide. Satellite remote sensing technology has been in use for a long time and has a wide range of shooting features. -
Lessons Learned from Lessons Learned From
Workshop on the Framework of LongLong--TermTerm Capacity Building for Disaster Risk Reduction in APEC Lessons Learned from Typhoon Morakot Dr. Hsu, Ming-Hsi Deputy Director, National Science & Technology Center for Disaster Reduction Professor, National Taiwan University Chinese Taipei 2 I Introduction II Damage and Losses III Lesson Learned IV Conclusions 3 I Introduction 4 Introduction • Before the end of June, we face a challenge of the drought problem . In the southern island, it did no rain in 60 consecutive days . The water storages in main reservoirs decreased to a lower stage fihifor operations at that time Shihmen Reservoir : 69 million tons (33%) Zengwen Reservoir : 126 million tons (21%) Nanhua Reservoir : 28 million tons (24%) . We expect Typhoon Morakot bringing rainfall to quench the dhdrought. • The Typhoon Morakot affected northern island on Aug. 7-9, but it results the worst flood in 50 years at southern island 5 Course of Typhoon Aug 5-6: Moved fast toward Chinese Taipei. Aug. 7 : Slowed down and out skirt touched the island. Aug. 8 : Made landfall at 00:00; Center left the island at 14:00 at very slow pace. Aug. 9 : Gradually moved toward China. 6 Doppler Radar Image • UilUnsymmetrical structure of rain clouds aroundtd typh oon •The typhoon rain cloud The Central Ridge interacted with suppl ying extra Eye moisture by southwest monsoon result large amount of rainfall in the south of the island. 7 Southwest Monsoon Interacted with Morakot by Supplying Extra Moisture Morakot Chinese Taipei 8 Accumulated Rainfall of Typhoon -
Rethinking Indigenous People's Drinking Practices in Taiwan
Durham E-Theses Passage to Rights: Rethinking Indigenous People's Drinking Practices in Taiwan WU, YI-CHENG How to cite: WU, YI-CHENG (2021) Passage to Rights: Rethinking Indigenous People's Drinking Practices in Taiwan , Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/13958/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 Passage to Rights: Rethinking Indigenous People’s Drinking Practices in Taiwan Yi-Cheng Wu Thesis Submitted for the Degree of Doctor of Philosophy Social Sciences and Health Department of Anthropology Durham University Abstract This thesis aims to explicate the meaning of indigenous people’s drinking practices and their relation to indigenous people’s contemporary living situations in settler-colonial Taiwan. ‘Problematic’ alcohol use has been co-opted into the diagnostic categories of mental disorders; meanwhile, the perception that indigenous people have a high prevalence of drinking nowadays means that government agencies continue to make efforts to reduce such ‘problems’. -
Indigenous Knowledge and Endogenous Actions for Building Tribal Resilience After Typhoon Soudelor in Northern Taiwan
sustainability Article Indigenous Knowledge and Endogenous Actions for Building Tribal Resilience after Typhoon Soudelor in Northern Taiwan Su-Hsin Lee 1 and Yin-Jen Chen 2,* 1 Department of Geography, National Taiwan Normal University, 162, Section 1, Heping E. Rd., Taipei City 10610, Taiwan; [email protected] 2 Graduate Institute of Earth Science, Chinese Culture University, 55, Hwa-Kang Road, Yang-Ming-Shan, Taipei City 11114, Taiwan * Correspondence: [email protected] Abstract: Indigenous peoples often face significant vulnerabilities to climate risks, yet the capacity of a social-ecological system (SES) to resilience is abstracted from indigenous and local knowledge. This research explored how the Tayal people in the Wulai tribes located in typhoon disaster areas along Nanshi River used indigenous knowledge as tribal resilience. It applied empirical analysis from secondary data on disaster relief and in-depth interviews, demonstrating how indigenous people’s endogenous actions helped during post-disaster reconstructing. With the intertwined concepts of indigenous knowledge, SESs, and tribes’ cooperation, the result presented the endogenous actions for tribal resilience. In addition, indigenous knowledge is instigated by the Qutux Niqan of mutual assistance and symbiosis among the Wulai tribes, and there is a need to build joint cooperation through local residence, indigenous people living outside of their tribes, and religious or social groups. The findings of tribal resilience after a typhoon disaster of co-production in the Wulai, Lahaw, and Fushan tribes include the importance of historical context, how indigenous people turn to their local knowledge rather than just only participating in disaster relief, and how they produce indigenous tourism for indigenous knowledge inheritance. -
Fordebris Flow Triggering Characteristics and Occurrence Probability After Extreme Rainfalls: Case Study in the Chenyulan Watershed, Taiwan
forDebris flow triggering characteristics and occurrence probability after extreme rainfalls: case study in the Chenyulan watershed, Taiwan Jinn-Chyi Chen1, Jiang- Guo Jiang1, Wen-Shun Huang2, Yuan-Fan Tsai3 5 1Department of Environmental and Hazards-Resistant Design, Huafan University, Taipei 22301, Taiwan 2 Ecological Soil and Water Conservation Research Center, National Cheng Kung University, Tainan 70101, Taiwan 3Department of Social and Regional Development, National Taipei University of Education, Taipei 10671, Taiwan 10 Correspondence to: Jinn-Chyi Chen ([email protected]) ABSTRACT. Rainfall and other extreme events often trigger debris flows in Taiwan. This study examines the debris flow triggering characteristics and probability of debris flow occurrence after extreme rainfalls. The Chenyulan watershed, central Taiwan, which has suffered from the Chi-Chi 15 earthquake and extreme rainfalls, was selected as a study area. The rainfall index (RI) was used to analyze the return period and characteristics of debris flow occurrence after extreme rainfalls. The characteristics of debris flow occurrence included the variation in critical RI, threshold of RI for debris flow triggering, and recovery period, the time required for the lowered threshold to return to the original threshold. The variations in critical RI after extreme rainfall and the recovery period associated with RI 20 are presented. The critical RI threshold was reduced in the years following an extreme rainfall event. The reduction in RI as well as recovery period were influenced by the RI. Reduced RI values showed an increasing trend over time, and it gradually returned to the initial RI. The empirical relationship between the probability of debris flow occurrence (P) and corresponding return period (T) of the rainfall characteristics for areas affected by extreme rainfalls and affected by the Chi-Chi earthquake were 25 developed. -
East & Southeast Asia: Typhoon Aere and Typhoon
EAST & SOUTHEAST ASIA: TYPHOON AERE AND 26 August 2004 TYPHOON CHABA 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 181 countries. In Brief This Information Bulletin (no. 01/2004) is being issued for information only. The Federation is not seeking funding or other assistance from donors for this operation at this time. For further information specifically related to this operation please contact: in Geneva: Asia and Pacific Department; phone +41 22 730 4222; fax+41 22 733 0395 All International Federation assistance seeks to adhere to the Code of Conduct and is committed to the Humanitarian Charter and Minimum Standards in Disaster Response in delivering assistance to the most vulnerable. For support to or for further information concerning Federation programmes or operations in this or other countries, or for a full description of the national society profile, please access the Federation’s website at http://www.ifrc.org The Situation Over the past 48 hours over a million people have had to be evacuated as two powerful typhoons, Typhoon Aere and Typhoon Chaba have been adversely affecting parts of East Asia and the Philippines. East Asia Some 516,000 people were evacuated earlier this week in response to the approach of Typhoon Aere which struck Taiwan with winds measuring as high as 165 kilometres per hour on Tuesday 24 August, triggering flooding and landslides throughout central and northern Taiwan. Thousands of homes were damaged in northern Taiwan, and thousands of people in the mountainous area of Hsinchu were stranded due to blocked roads. -
Member Report
MEMBER REPORT ESCAP/WMO Typhoon Committee 42nd Session 25–29 January 2010 Singapore People’s Republic of China 1 CONTENTS I. Overview of tropical cyclones which have affected/impacted Member’s area since the last Typhoon Committee Session II. Summary of progress in Key Result Areas 1. Progress on Key Result Area 1 2. Progress on Key Result Area 2 3. Progress on Key Result Area 3 4. Progress on Key Result Area 4 5. Progress on Key Result Area 5 6. Progress on Key Result Area 6 7. Progress on Key Result Area 7 III. Resource Mobilization Activities IV. Update of Members’ Working Groups representatives 2 I. Overview of tropical cyclones which have affected/impacted Member’s area in 2009 In 2009, totally 9 tropical cyclones landed on China. They were severe tropical storm Linfa (0903), tropical storm Nangka (0904) and Soudelor (0905), Typhoon Molave (0906), tropical storm Goni (0907), typhoon Morakot (0908), tropical storm Mujigae (0913), typhoon Koppu (0915) and super typhoon Parma (0917) respectively. 1. Meteorological Assessment (highlighting forecasting issues/impacts) (1) LINFA (0903) LINFA formed as a tropical depression over South China Sea at 06:00 UTC 17 June 2009. It developed into a tropical storm and a severe tropical storm at 06:00 UTC 18 June and 03:00 UTC 20 June respectively. LINFA started to move northwards. As it was gradually approaching to the coast of the Fujian province, its intensity was greatly reduced to be a tropical storm category. LINFA landed on Jinjiang of the Fujian province, China at 12:30 UTC 21 June with the maximum wind at 23m/s near its centre.