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Organic Fluorescent Characteristics of Five Tributaries in Gaoping River Basin in Dry Season
International Proceedings of Chemical, Biological and Environmental Engineering, V0l. 101 (2017) DOI: 10.7763/IPCBEE. 2017. V101. 4 Organic Fluorescent Characteristics of Five Tributaries in Gaoping River Basin in Dry Season Guan-Ling Chen 1, Jing-Wen Cao 2, Chun-Yen Chiu 3, Lih-fu Chen 4, Wen-Liang Lai 5,* 1 Graduate School of Environmental Management, Master student, Tajen, Pingtung 907, Taiwan, ROC (E- mail: [email protected]) 2 Graduate School of Environmental Management, Assistant, Tajen University, Pingtung 907, Taiwan, ROC (E-mail: [email protected]) 3 Graduate School of Environmental Management, Associate Professor, Tajen University, Pingtung 907, Taiwan, ROC (E-mail: [email protected]) 4 College of Liberal Education, Shu-Te University, Associate Professor, Kaohsiung 82445, Taiwan, ROC (E- mail: [email protected]) 5 Graduate School of Environmental Management, Professor, Tajin University, Pingtung 907, Taiwan, ROC, (E-mail: [email protected]) *Corresponding author Abstract. In this research, fluorescence excitation emission spectrometry (Excitation emission fluorescent matrix, EEFM) and total organic carbon Analyzer were main instruments applied into evaluating the property and amount of natural organic matter in dry season for Gaoping River basin located in Southern Taiwan. Dissolved non-volatile organic carbon in water (non-purgeable dissolved organic carbon, NPDOC) was measured and SUVA, (UV254/NPDOC), BIX (Biological index, BIX) were compared in whole samples belonging to five segments. Results showed that NPDOC values of whole samplings in Gaoping River basin were less than the criteria of Source Water Standard of Drinking Water except for Jiouru bridges. SUVA values and BIX for whole samplings were less than 1, indicating that the source pollution in the Gaoping River Basin was mainly attributed to the human activity and microbial organic matter produced in the River. -
Forensic Investigation of Typhoon Morakot Disaster: Nansalu and Daniao Village Case Study
NCDR 102-T28 Forensic Investigation of Typhoon Morakot Disaster: Nansalu and Daniao Village Case Study HuiHsuan Yang, SuYing Chen, SungYing Chien , and WeiSen Li 2014.05 Contents CONTENTS ................................................................................................................... I TABLES. ....................................................................................................................... II FIGURES ..................................................................................................................... III ABSTRACT .................................................................................................................. IV I. INTRODUCTION ................................................................................................. 1 II. TYPHOON MORAKOT DISASTER ......................................................................... 2 III. REVIEWING POSSIBLE CAUSES OF MORAKOT IMPACTS: ..................................... 4 (I) METEOROLOGICAL FACTORS .............................................................................................. 4 (II) PHYSIOGRAPHIC FACTORS ................................................................................................ 4 (III) DISASTER MITIGATION ................................................................................................... 4 (IV) DISASTER RESPONSE ..................................................................................................... 6 IV. RESEARCH APPROACH ...................................................................................... -
From the Highest to the Deepest: the Gaoping River–Gaoping Submarine Canyon Dispersal System
Earth-Science Reviews 153 (2016) 274–300 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev From the highest to the deepest: The Gaoping River–Gaoping Submarine Canyon dispersal system James T. Liu a,⁎, Ray T. Hsu a, Jia-Jang Hung a,Yuan-PinChanga,Yu-HuaiWanga, Rebecca H. Rendle-Bühring b, Chon-Lin Lee c, Chih-An Huh d,RickJ.Yanga a Department of Oceanography, National Sun Yat-sen University, Kaohsiung 80424, Taiwan ROC b Department of Geosciences, University of Bremen, PO Box 330440, D-28334 Bremen, Germany c Department of Marine Environment, National Sun Yat-sen University, Kaohsiung 80424, Taiwan ROC d Institute of Earth Sciences, Academia Sinica, Taipei, 11529, Taiwan ROC article info abstract Article history: There are many different source-to-sink dispersal systems around the world, and the Gaoping River (GPR)– Received 2 September 2014 Gaoping Submarine Canyon (GPSC) provides an example especially as a canyon-captured system. The GPR, a Received in revised form 22 September 2015 small mountainous river having an average gradient of 1:150, and the GPSC, which links the river catchment Accepted 27 October 2015 to the deep-sea basin, represent two major topographic features around SW Taiwan. Together, they constitute Available online 30 October 2015 a terrestrial-to-marine dispersal system that has an overriding impact on the source-to-sink transport of sediment in this region. The GPSC extents from the mouth of the GPR through the shelf and slope and into the Keywords: Small mountainous river northeastern Manila Trench, a distance of about 260 km. -
英文節慶網站建置 英文 主辦單位基本資料(公開資訊) Project Title Liu-Dui Blessing Pole-Firecrackers Beating Series Activities Title of Organization: Person Responsible
中英文節慶網站建置 英文 主辦單位基本資料(公開資訊) Project Title Liu-dui Blessing Pole-firecrackers Beating Series Activities Title of Organization: Person Responsible: Organization Pingtung County Director Tzeng Mei-ling, Hakka Responsible Government affairs Department Address No.527, Zi-you Rd. Ping-tung City Person to CHEN YA-CHENG, 08-7324015 Ext. 3924 Contact Cellphone: 0917-353-921 Fax.number 08- 7346304 E-mai address [email protected] 【節慶重點介紹】 The Origin of Activities Celebrations and worships are important customs of folk beliefs, ancestors of Liu-dui hakka region live mainly on farming, there had been romance among them, therefore, all the festival activities are closely connect to their farming phases and paces. Following the development and progress of modern society, aiming to preserve traditional cultures and promote local human cultural thinking and local social development, organizations in Liu-dui region have recently popularized many cultural activities, rebuild a new face of Liu-dui Hakka Culture, combine tradition and folk beliefs, and stimulate the love and passion of people around Liu-dui regions. The activity “Liu-dui Pole-firecrackers Beating ” was originated at the Wu-gou-suei area of Wan-luan township, and it was highly praised and chosen as “One of the 12 Major Festivals of Hakka Village” since 2009. For modeling local brand image, our series activities are based on the following concepts: 1 a. Go back to the original place, Wu-gou-suei, preserve our traditional culture, to model the brand image of local festivals. b. The activity combines the features of Liu-dui Hakka Culture, showing significant index. c. -
Hotspot Analysis of Taiwanese Breeding Birds to Determine Gaps In
Wu et al. Zoological Studies 2013, 52:29 http://www.zoologicalstudies.com/content/52/1/29 RESEARCH Open Access Hotspot analysis of Taiwanese breeding birds to determine gaps in the protected area network Tsai-Yu Wu1, Bruno A Walther2,3, Yi-Hsiu Chen1, Ruey-Shing Lin4 and Pei-Fen Lee1,5* Abstract Background: Although Taiwan is an important hotspot of avian endemism, efforts to use available distributional information for conservation analyses are so far incomplete. For the first time, we present a hotspot analysis of Taiwanese breeding birds with sufficient sampling coverage for distribution modeling. Furthermore, we improved previous modeling efforts by combining several of the most reliable modeling techniques to build an ensemble model for each species. These species maps were added together to generate hotspot maps using the following criteria: total species richness, endemic species richness, threatened species richness, and rare species richness. We then proceeded to use these hotspot maps to determine the 5% most species-rich grid cells (1) within the entire island of Taiwan and (2) within the entire island of Taiwan but outside of protected areas. Results: Almost all of the species richness and hotspot analyses revealed that mountainous regions of Taiwan hold most of Taiwan's avian biodiversity. The only substantial unprotected region which was consistently highlighted as an important avian hotspot is a large area of unprotected mountains in Taiwan's northeast (mountain regions around Nan-ao) which should become a high priority for future fieldwork and conservation efforts. In contrast, other unprotected areas of high conservation value were just spatial extensions of areas already protected in the central and southern mountains. -
FULLTEXT01.Pdf
1 Table of Contents Abstract ................................................................................................................................................... 3 Introduction ............................................................................................................................................. 4 Background .......................................................................................................................................... 5 River-Sea System ............................................................................................................................. 6 Annual changes in sediment delivery .............................................................................................. 7 Methods .................................................................................................................................................. 9 Marine coring ...................................................................................................................................... 9 Core sampling .................................................................................................................................... 10 Loss on Ignition .................................................................................................................................. 10 Freeze drying ..................................................................................................................................... 10 Grain Size .......................................................................................................................................... -
Application of High-Resolution Radar Rain Data to the Predictive Analysis of Landslide Susceptibility Under Climate Change in the Laonong Watershed, Taiwan
remote sensing Article Application of High-Resolution Radar Rain Data to the Predictive Analysis of Landslide Susceptibility under Climate Change in the Laonong Watershed, Taiwan Chun-Wei Tseng 1,2 , Cheng-En Song 3, Su-Fen Wang 3, Yi-Chin Chen 3 , Jien-Yi Tu 3 , Ci-Jian Yang 4 and Chih-Wei Chuang 5,* 1 Department of Civil Engineering, National Taipei University of Technology, Taipei 10608, Taiwan; [email protected] 2 Division of Watershed Management, Taiwan Forestry Research Institute, Taipei 100051, Taiwan 3 Department of Geography, National Changhua University of Education, Changhua 50074, Taiwan; [email protected] (C.-E.S.); [email protected] (S.-F.W.); [email protected] (Y.-C.C.); [email protected] (J.-Y.T.) 4 Department of Geography, National Taiwan University, Taipei 10617, Taiwan; [email protected] 5 Department of Soil and Water Conservation, National Pingtung University of Science and Technology, Pingtung 912301, Taiwan * Correspondence: [email protected]; Tel.: +886-8-7703202 (ext. 7366) Received: 22 October 2020; Accepted: 23 November 2020; Published: 25 November 2020 Abstract: Extreme rainfall has caused severe road damage and landslide disasters in mountainous areas. Rainfall forecasting derived from remote sensing data has been widely adopted for disaster prevention and early warning as a trend in recent years. By integrating high-resolution radar rain data, for example, the QPESUMS (quantitative precipitation estimation and segregation using multiple sensors) system provides a great opportunity to establish the extreme climate-based landslide susceptibility model, which would be helpful in the prevention of hillslope disasters under climate change. -
Channel Planform Dynamics Monitoring and Channel Stability Assessment in Two Sediment-Rich Rivers in Taiwan
Article Channel Planform Dynamics Monitoring and Channel Stability Assessment in Two Sediment-Rich Rivers in Taiwan Cheng-Wei Kuo 1,*, Chi-Farn Chen 2, Su-Chin Chen 1, Tun-Chi Yang 3 and Chun-Wei Chen 2 1 Department of Soil and Water Conservation, National Chung Hsing University, 145 Xingda Rd., South Dist., Taichung, 402, Taiwan; [email protected] (S.-C.C.) 2 Center for Space and Remote Sensing Research, National Central University, 300 Jhongda Rd., Jhongli Dist., Taoyuan, 32001, Taiwan; [email protected] (C.-F.C.); [email protected] (C.- W.C.) 3 Water Administration Division, Water Resources Agency, Ministry of Economic Affairs, 501,Sec. 2, Liming Rd., Nantun Dist., Taichung 408, Taiwan; [email protected] (T.-C.Y.) * Correspondence: [email protected]; Tel.: +886-4-22840238; Fax: +886-22853967 Academic Editor: Peggy A. Johnson Received: 30 November 2016; Accepted: 25 January 2017; Published: 30 January 2017 Abstract: Recurrent flood events induced by typhoons are powerful agents to modify channel morphology in Taiwan’s rivers. Frequent channel migrations reflect highly sensitive valley floors and increase the risk to infrastructure and residents along rivers. Therefore, monitoring channel planforms is essential for analyzing channel stability as well as improving river management. This study analyzed annual channel changes along two sediment-rich rivers, the Zhuoshui River and the Gaoping River, from 2008 to 2015 based on satellite images of FORMOSAT-2. Channel areas were digitized from mid-catchment to river mouth (~90 km). Channel stability for reaches was assessed through analyzing the changes of river indices including braid index, active channel width, and channel activity. -
A River Discharge Model for Coastal Taiwan During Typhoon Morakot
Multidisciplinary Simulation, Estimation, and Assimilation Systems Reports in Ocean Science and Engineering MSEAS-13 A River Discharge Model for Coastal Taiwan during Typhoon Morakot by Christopher Mirabito Patrick J. Haley, Jr. Pierre F.J. Lermusiaux Wayne G. Leslie Department of Mechanical Engineering Massachusetts Institute of Technology Cambridge, Massachusetts August 2012 A River Discharge Model for Coastal Taiwan during Typhoon Morakot∗ C. Mirabitoy P. J. Haley, Jr. P. F. J. Lermusiaux W. G. Leslie Abstract In the coastal waters of Taiwan, freshwater discharge from rivers can be an important source of uncer- tainty in regional ocean simulations. This effect becomes especially acute during extreme storm events, such as typhoons. In particular, record-breaking discharge caused by Typhoon Morakot (August 6{10, 2009) was observed to significantly affect near-shore temperature and salinity during the Intensive Ob- servation Period-09 (IOP09) of the Quantifying, Predicting and Exploiting Uncertainty (QPE) research initiative. In this report, a river discharge model is developed to account for the sudden large influx of freshwater during and after the typhoon. The discharge model is then evaluated by comparison with the discharge time series for the Zhu´oshuˇı(Á4) and G¯aop´ıng(高O) Rivers and by its utilization as forcing in ocean simulations. The parameters of the discharge and river forcing models and their effects on ocean simulations are discussed. The reanalysis ocean simulations with river forcing are shown to capture several of the independently observed features in the evolution of the coastal salinity field as well as the magnitude of the freshening of the ocean caused by runoff from Typhoon Morakot. -
Kaohsiung Locates in the South-West Area of Taiwan, Long and Narrow on a South-North Axis
Kaohsiung locates in the south-west area of Taiwan, long and narrow on a south-north axis. It is full of sunshine all year long and the weather is delightful. The area of Kaohsiung reaches 2946 km2. The Taiwan Strait is to the west and KaoPing River and Pingtung County are to the south, naturally forms the bay of Kaohsiung. Plentiful landforms enable Kaohsiung to have a distinctive city landscape with mountains, sea, rivers, and harbor, also develop its multi-ethnic culture. Rich historic culture, natural resources of mountain and sea, and the enthusiasm of people make Kaohsiung become one and only south big city. Kaohsiung has continuous supply of vitality and becomes a genuine maritime tourism capital. Kaohsiung Passionate Livable City 首爾 3 hours and 15 minutes 北京 Seoul 東京 Beijing 釜山 Tokyo 2 hours and 35 minutes Busan 3 hours and 21 minutes 大阪 2 hours and 30 minutes Osaka 上海 2 hours and 40 minutes Shanghai 2 hours and 10 minutes 台北 About Kaohsiung City Taipei Geographic Characteristics of Kaohsiung 1 hour The 2,946 km2 Kaohsiung City is a vertical strip of land in 1 hour and 15 minutes Southwestern Taiwan, bordering on the Jianan Plain, Pingtung Plain, 香港 高雄 Taiwan Strait and Bashi Channel to the north, east, west and south, Hong Kong Kaohsiung respectively. The City provides a strategically located pathway from Northeast Asia to the South Pacific, with natural qualities befitting a good commercial harbor as well an emerging cosmopolis. Transportation-wise, the Kaohsiung International Airport offers direct links to various Asian cities and Taiwan Taoyuan International Airport, from which flights to destinations worldwide depart. -
Ready for a Journey to Explore Taiwan's Indigenous Tribes ? Let’S Go !
Did you know ? Taiwan is home to groups of Austronesian indigenous people who have lived on this island for over 8,000 years. Did you know ? Taiwan has sixteen officially recognized indigenous peoples, who each have their own native languages and culture. Did you know ? Alongside famous tourist magnets like Taroko Gorge, Alishan, Sun Moon Lake, and Kenting, you may also explore and experience the traditional lifestyles of aboriginal tribes around the island. Ready for a journey to explore Taiwan's indigenous tribes ? Let’s go ! uhtan’e ho mimimiyo in the Tsou language means "Come, from one village to another." 2 3 . . Distribution of Taiwan's Indigenous Peoples Distribution of Taiwan's Indigenous Peoples Amis Or Pangcah. They live on plains around Mt. Chilai in northern Hualien, south to the coastal plains and the hilly Distribution of Indigenous Peoples in Taiwan areas of Taitung and the Hengchun Peninsula. They have a total population of about 177,000, which is the largest Taiwanese indigenous peoples were the first among Taiwan’s indigenous peoples. settlers on this island. They have diverse Atayal Distributed in the northern part of Taiwan’s Central cultural backgrounds and languages. Mountain Range, including the area from north of Puli to Their population is approximately Hualien. They have a total population of approximately 540,000 (only 2.3% of Taiwan’s total). 81,000. Most indigenous groups live Scattered on both sides of the southern Central Mountain around the Central Mountain Paiwan Range - from north to Mt. Dawu, south to Hengchun, west Range, in the East Rift Valley to Fangliao, and east to Taimali in Taitung. -
Attribution of Streamflow Variations in Southern Taiwan
water Article Attribution of Streamflow Variations in Southern Taiwan Jyun Tsao, Cheng-Haw Lee and Hsin-Fu Yeh * Department of Resources Engineering, National Cheng Kung University, Tainan 701, Taiwan; [email protected] (J.T.); [email protected] (C.-H.L.) * Correspondence: [email protected]; Tel.: +886-6-275-7575 Received: 11 July 2020; Accepted: 29 August 2020; Published: 2 September 2020 Abstract: Climate change and anthropogenic activity are the main factors impacting the hydrological environment. For sustainable water utilization, identifying the impact contribution of these two factors on the streamflow variations is an important topic in recent research. In this study, seven river basins in southern Taiwan were selected as the study area to evaluate the annual streamflow from 1980 to 2017. The decomposition and elasticity methods based on the Budyko hypothesis were applied to quantify the contribution of climate and anthropogenic factors to the streamflow variations. In addition, the normalized difference vegetation index (NDVI) was used to represent the actual situation of land cover and verify the parameters in the Budyko equation. The two quantitative methods consistently demonstrated that the streamflow variations from pre- to post-period occurred due to the climate factor. The elasticity coefficient of variables demonstrated that the streamflow change is more sensitive to precipitation and this influence reduces from pre- to post-period as the streamflow increase. In the NDVI variations, except for the Yanshui and the Linbain rivers, the Budyko equation parameters changed consistently with NDVI. The present study provides effective results on the contribution of streamflow variations in southern Taiwan to serve as a reference for future water management.