Assessment of Flood Hazard Areas Using Analytical Hierarchy Process

Total Page:16

File Type:pdf, Size:1020Kb

Assessment of Flood Hazard Areas Using Analytical Hierarchy Process Available online at www.sciencedirect.com Available online at www.sciencedirect.com ScienceDirect AvailableProcedia online Engineering at www.sciencedirect.com 00 (2017) 000–000 2 Seejata et al./ Procedia Engineering 00 (2017) 000–000 Procedia Engineering 00 (2017) 000–000 www.elsevier.com/locate/procedia www.elsevier.com/locate/procedia ScienceDirect Flood hazard map is a tool for assessment of flood vulnerability to understand a level of susceptibility to being harmed [3]. In order to identify a degree of the susceptibility, flood hazard map can be constructed on the basis of Procedia Engineering 212 (2018) 340–347 physical and ecological systems in the environment of Geographic Information Systems (GIS). GIS is effective tool to determine the high risk of flood prone areas down to small hydrological basins. In addition, GIS has its capability 7th International Conference on Building Resilience; Using scientific knowledge to inform policy to manipulate multi-dimensional phenomena of natural hazards using spatial component [4]. 7thand International practice in disaster Conference risk reduction, on Building ICBR2017, Resilience; 27 Using – 29 November scientific knowledge2017, Bangkok, to inform Thailand policy The physical factors used in GIS needs to be associated with a procedure referred to as multi-criteria analysis and practice in disaster risk reduction, ICBR2017, 27 – 29 November 2017, Bangkok, Thailand (MCA) that weights the parameters logically. One of the methods to determine the relative importance of the factors is Analytical Hierarchy Process (AHP) [5, 6] that has been used in many applications [7, 8, 9] In this study, we aim Assessment of flood hazard areas using Analytical Hierarchy to model a flood hazard area using spatial multi-criteria index to understand the relative importance of the Process over the Lower Yom Basin, Sukhothai Province parameters used. Then, the produced flood hazard map is compared and discussed with an observed flood extent Process overa the Lowera Yom Basin, Sukhothaia Provincea from secondary data source. Kamonchat Seejataa, Aphittha Yodyinga, Tubtim Wongthadamb a, Nattapon Mahavika*, Sarintip Kamonchat Seejata , Aphittha Yodying , TubtimTantanee Wongthadamb , Nattapon Mahavik *, Sarintip Tantanee 2. Study area and data aDepartment of Natural Resources and Environment, Naresuan University, Phitsanulok, Thailand a Departmentb of Natural Resources and Environment, Naresuan University, Phitsanulok, Thailand Department of Civil Engineering, Naresuan University, Phitsanulok, Thailand bDepartment of Civil Engineering, Naresuan University, Phitsanulok, Thailand Abstract Abstract Flood hazard map is essential tool to assess susceptibility of flood prone area. The present study focuses on an assessment of floodFlood hazardhazard areasmap isin essential Sukhothai tool province to assess of susceptibilityThailand where of floodit has prone suffered area. from The floodpresent in studyevery focusesyear with on differentan assessment extents. of Spatifloodal hazard analysis areas in GIS in Sukhothaienvironment province has been of appliedThailand for where the estimation it has suffered of flood from risk floodzones in whichevery yearsix relevant with different physical extents. factors haveSpati albeen analysis selected in GIS namely, environment rainfall has amount, been applied slope, for elevation, the estimation river ofdensity, flood riskland zones use inand which soil sixpermeability. relevant physical The relative factors have been selected namely, rainfall amount, slope, elevation, river density, land use and soil permeability. The relative importance of physical factors has been compared in pairwise matrix to gain the weight values during the process of Analytical importance of physical factors has been compared in pairwise matrix to gain the weight values during the process of Analytical Hierarchy Process (AHP). The flood hazard zones have been mapped according to their weights. It has been found that Muang, Hierarchy Process (AHP). The flood hazard zones have been mapped according to their weights. It has been found that Muang, Kongkrailat, Khirimat and Sisamrong districts are identified as the high risk zones of flood. Kongkrailat, Khirimat and Sisamrong districts are identified as the high risk zones of flood. © 2017 The Authors. Published by Elsevier Ltd. © 2017 The Authors. Published by Elsevier Ltd. Peer© 2018-review Theunder responsibilityAuthors. ofPublished the scientific bycommittee Elsevier of the 7thLtd. International Conference on Building Resilience. Peer-review under responsibility of the scientific committee of the 7th International Conference on Building Resilience. Peer-review under responsibility of the scientific committee of the 7th International Conference on Building Resilience. * Corresponding author: Email: [email protected] Tel*Corresponding: +66-55-962752 author : Email: [email protected] Tel: +66-55-962752 Keywords: Flood Hazard Map, Thailand, GIS Keywords: Flood Hazard Map, Thailand, GIS 1. Introduction 1. Introduction Flood is one of the natural disasters that cause a damage worldwide [1]. In 2011, Thailand has also suffered from Flood is one of the natural disasters that cause a damage worldwide [1]. In 2011, Thailand has also suffered from a massive flood event of their histories [2]. There were five tropical storms and three strong low-pressure systems a massive flood event of their histories [2]. There were five tropical storms and three strong low-pressure systems that occurred between June and October 2011. The Chao Phraya River basin (CPRB), the largest basin in Thailand, that occurred between June and October 2011. The Chao Phraya River basin (CPRB), the largest basin in Thailand, has been flooded causing more than 700 people killed. The estimation of total damage loss by the World Bank was Fig. 1. Study area has been flooded causing more than 700 people killed. The estimation of total damage loss by the World Bank was around 1.36 trillion baht. around 1.36 trillion baht. Sukhothai province, Northern Thailand, where is lower part of Yom river has been selected as study area because 1877-7058 © 2017 The Authors. Published by Elsevier Ltd. the present study area has suffered from every flood, even though the flood extent are different in each year. In Peer1877--review7058 © under 2017 responsibilityThe Authors. ofPublished the scientific by Elsevier committee Ltd. of the 7th International Conference on Building Resilience. Peer-review under responsibility of the scientific committee of the 7th International Conference on Building Resilience. addition, the present study area has not yet been constructed a permanent dam. This may be interested area to model of flood in GIS environment without complicate factor of dam. Sukhothai province covers an area of 6,596 sq. km and it consists of nine districts. The Yom river flows through from the north to southeast of the province that tributary rivers mainly flow to meet the Yom river from the right side of river bank in the central and lower part of the province. Moreover, the northern part of the province is mountainous area which restricts the flood plain 1877-7058 © 2018 The Authors. Published by Elsevier Ltd. compared to larger river flat plain over the central and southern part of the province. The largest of mountainous Peer-review under responsibility of the scientific committee of the 7th International Conference on Building Resilience 10.1016/j.proeng.2018.01.044 10.1016/j.proeng.2018.01.044 1877-7058 Available online at www.sciencedirect.com Available online at www.sciencedirect.com ScienceDirect Kamonchat Seejata et al. / Procedia Engineering 212 (2018) 340–347 341 Procedia Engineering 00 (2017) 000–000 2 Seejata et al./ Procedia Engineering 00 (2017) 000–000 Procedia Engineering 00 (2017) 000–000 www.elsevier.com/locate/procedia www.elsevier.com/locate/procedia Flood hazard map is a tool for assessment of flood vulnerability to understand a level of susceptibility to being harmed [3]. In order to identify a degree of the susceptibility, flood hazard map can be constructed on the basis of physical and ecological systems in the environment of Geographic Information Systems (GIS). GIS is effective tool to determine the high risk of flood prone areas down to small hydrological basins. In addition, GIS has its capability 7th International Conference on Building Resilience; Using scientific knowledge to inform policy to manipulate multi-dimensional phenomena of natural hazards using spatial component [4]. 7thand International practice in disaster Conference risk reduction, on Building ICBR2017, Resilience; 27 Using – 29 November scientific knowledge2017, Bangkok, to inform Thailand policy The physical factors used in GIS needs to be associated with a procedure referred to as multi-criteria analysis and practice in disaster risk reduction, ICBR2017, 27 – 29 November 2017, Bangkok, Thailand (MCA) that weights the parameters logically. One of the methods to determine the relative importance of the factors is Analytical Hierarchy Process (AHP) [5, 6] that has been used in many applications [7, 8, 9] In this study, we aim Assessment of flood hazard areas using Analytical Hierarchy to model a flood hazard area using spatial multi-criteria index to understand the relative importance of the Process over the Lower Yom Basin, Sukhothai Province parameters used. Then, the produced flood hazard map is compared and discussed with an observed flood extent Process overa the Lowera Yom Basin, Sukhothaia Provincea
Recommended publications
  • Japan International Cooperation Agency (Jica)
    Project for the Comprehensive Flood Management Plan Main Report for the Chao Phraya River Basin in the Kingdom of Thailand Chapter 9 Strategy of Master Plan Formulation CHAPTER 9 STRATEGY OF MASTER PLAN FORMULATION 9.1 Basic Approach to the Master Plan 9.1.1 Concept of Master Plan The Chao Phraya River Basin is composed of three (3) areas; namely, the Highlands, the Upper Central Plain and the Lower Central Plain. The characteristics of each area and its required measures have been examined to formulate the Master Plan of Flood Disaster Management for the Chao Phraya River Basin. The study area is outlined from flood disaster management aspects as follows: 1) The Highlands are the watersheds of the major tributaries of the Chao Phraya River Basin, which are the Ping, Wang, Yom and Nan rivers. The areas are covered by forest, but the forest area has been devastated and the degraded forest areas have been identified by the Royal Forest Department. For flood disaster management, restoration of the degraded forest areas and the improvement of forest management are required. 2) The Upper Central Plain is located at the Upper Nakhon Sawan and composed of the river basins of the Ping, Wang, Yom, Nan and Chao Phraya. During the 2011 flood in the Upper Central Plain the inundation started along the Yom River in late July and at Nakhon Sawan in early September. The areas are flat and have wide low-lying areas along the rivers, which have a functional role in natural flood retarding basin and partly habitual inundation areas in rainy season, but partly used as agricultural lands in dry season.
    [Show full text]
  • Did the Construction of the Bhumibol Dam Cause a Dramatic Reduction in Sediment Supply to the Chao Phraya River?
    water Article Did the Construction of the Bhumibol Dam Cause a Dramatic Reduction in Sediment Supply to the Chao Phraya River? Matharit Namsai 1,2, Warit Charoenlerkthawin 1,3, Supakorn Sirapojanakul 4, William C. Burnett 5 and Butsawan Bidorn 1,3,* 1 Department of Water Resources Engineering, Chulalongkorn University, Bangkok 10330, Thailand; [email protected] (M.N.); [email protected] (W.C.) 2 The Royal Irrigation Department, Bangkok 10300, Thailand 3 WISE Research Unit, Chulalongkorn University, Bangkok 10330, Thailand 4 Department of Civil Engineering, Rajamangala University of Technology Thanyaburi, Pathumthani 12110, Thailand; [email protected] 5 Department of Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL 32306, USA; [email protected] * Correspondence: [email protected]; Tel.: +66-2218-6455 Abstract: The Bhumibol Dam on Ping River, Thailand, was constructed in 1964 to provide water for irrigation, hydroelectric power generation, flood mitigation, fisheries, and saltwater intrusion control to the Great Chao Phraya River basin. Many studies, carried out near the basin outlet, have suggested that the dam impounds significant sediment, resulting in shoreline retreat of the Chao Phraya Delta. In this study, the impact of damming on the sediment regime is analyzed through the sediment variation along the Ping River. The results show that the Ping River drains a mountainous Citation: Namsai, M.; region, with sediment mainly transported in suspension in the upper and middle reaches. By contrast, Charoenlerkthawin, W.; sediment is mostly transported as bedload in the lower basin. Variation of long-term total sediment Sirapojanakul, S.; Burnett, W.C.; flux data suggests that, while the Bhumibol Dam does effectively trap sediment, there was only a Bidorn, B.
    [Show full text]
  • EN Himantura Chaophraya
    First published : November 2005 by Office of Natural Resources and Environmental Policy and Planning (ONEP), Thailand. ISBN : 974–9929–87–X This publication is financially supported by ONEP and may be reproduced in whole or in part and in any form for educational or non–profit purposes without special permission from ONEP, providing that acknowledgment of the source is made. No use of this publication may be made for resale or for any other commercial purposes. Citation : Vidthayanon C., 2005. Thailand Red Data : Fishes. Office of Natural Resources and Environmental Policy and Planning, Bangkok, Thailand. 108 p. Author : Chavalit Vidthayanon (D. Sc.) Education : D. Sc. of Aquatic Bioscience Tokyo University of Fisheries Position : Senior Freshwater Specialist WWF Thailand Field of Work : l Research for supporting participatory conservation of wetlands in the Mekong basin and northern Thailand. l 15 years’ experience developing and researching aquatic biodiversity, both marine and freshwater. Available from : Biological Diversity Division Office of Natural Resources and Environmental Policy and Planning Ministry of Natural Resources and Environment 60/1 Rama VI Rd. Bangkok 10400 THAILAND Telephone (66) 2265 6638–39 Facsimile (66) 2265 6638 Website: http://chm-thai.onep.go.th E-mail: [email protected] Designed & Printed : Integrated Promotion Technology Co., Ltd. Telephone (66) 2585 2076, 2586 0837 Facsimile (66) 2913 7763 2 1. Mae Hong Son 20. Nakhon Sawan 39. Udon Thani 58. Chachoengsao 2. Chiang Mai 21. Uthai Thani 40. Sakon Nakhon 59. Chon Buri 3. Chiang Rai 22. Chai Nat 41. Nong Khai 60. Rayong 4. Lamphun 23. Suphan Buri 42. Nakhon Phanom 61.
    [Show full text]
  • An Application of Hec-Ras Model and Geographic Information System on Flood Maps Analysis: Case Study of Upper Yom River
    The 40th Asian Conference on Remote Sensing (ACRS 2019) October 14-18, 2019 / Daejeon Convention Center(DCC), Daejeon, Korea TuF2-2 AN APPLICATION OF HEC-RAS MODEL AND GEOGRAPHIC INFORMATION SYSTEM ON FLOOD MAPS ANALYSIS: CASE STUDY OF UPPER YOM RIVER Sutthipat Wannapoch* (1), Sarintip Tantanee (1), Sombat Chuenchooklin (1), Kamonchat Seejata (1), Weerayuth Pratoomchai (2) 1 Department of Civil Engineering, Naresuan University, Phitsanulok, Thailand. 2 Department of Engineering, King Mongkut's University of Technology Thonburi, Bangkok, Thailand. *Presenting author: Sutthipat Wannapoch; E-mail: [email protected] Corresponding author: Sarintip Tantanee; E-mail: [email protected] KEYWORDS: HEC-RAS, Geographic Information System, Flood Hazard, Flood Vulnerability, Upper Yom River. ABSTRACT: Most important disaster in Thailand is the flood, which frequently occurs and causes widespread losses in both properties and lives. Yom river basin is one of the basin in Thailand which is a narrow stream without regulated dam in upstream. Therefore, during rainy season, these area often suffer from flood. Phrae province where locate in a flood-prone area of upper Yom river basin have faced with flood almost every year. To manage the disaster situations, the approaches to assess the flood susceptible areas and the extent of disaster impact are the challenging tasks. This study aimed to develop flood hazard map, flood vulnerability map, and flood risk map along Yom river in Phrae province by using hydrological model of HEC-RAS and a set of procedures of HEC-GeoRAS for processing geospatial data in Geographic Information System (GIS). The model was calibrated using the rainfall observation data during flood seasons from 2007 to 2016.
    [Show full text]
  • Sukhothai Wat Si Chum Uttaradit • Phitsanulok • Phetchabun Contents Sukhothai 10 Uttaradit 30 Phitsanulok 36 Phetchabun 44
    Sukhothai Wat Si Chum Uttaradit • Phitsanulok • Phetchabun Contents Sukhothai 10 Uttaradit 30 Phitsanulok 36 Phetchabun 44 10 11 Sukhothai is located on the lower edge of the northern region, with the provincial capital situated some 450 km. north of Bangkok and some 350 km. south of Chiang Mai. The province covers 6,596 sq. km. and is above all noted as the centre of the old Thai kingdom of Sukhothai, with major historical remains at Sukhothai and Si Satchanalai. Its main natural attraction is Khao Luang mountain park. The provincial capital, sometimes called New Sukhothai, is a small town lying on the Yom River whose main business is serving tourists who visit the nearby Sukhothai Historical Park. City Attractions Phra Mae Ya Shrine Situated in front of the City Hall, the Shrine houses the Phra Mae Ya figure, in ancient queen’s dress, said to have been made by King Ramkhamhaeng as a dedication to his late mother Nang Sueang. Sangkhalok Museum The Museum displays Sangkhalok (Sawankhalok) ceramics of the kind produced in old Sukhothai and ceramics produced in the old Lanna Kingdom (now northern Thailand). Located 1 km. from town on the Phitsanulok Road; open daily 8 a.m.- 5 p.m.; admission : 100 baht adults, 20 baht children. Fish Museum Located in Rama IV Park on the Phitsanulok Road, the Museum displays a variety of freshwater fish mentioned in Thai literature. Open daily except Tuesdays 9 a.m.-5 p.m., admission free. Wat Si Chum Phra Mae Ya Shrine Sukhothai The province covers 6,596 sq. km.
    [Show full text]
  • The Interpretation of Si Satchanalai
    THE INTERPRETATION OF SI SATCHANALAI By MR. Jaroonsak JARUDHIRANART A Thesis Submitted in Partial Fulfillment of the Requirements for Doctor of Philosophy (Architectural Heritage Management and Tourism) International Program Graduate School, Silpakorn University Academic Year 2017 Copyright of Graduate School, Silpakorn University - โดย นายจรูญศกั ด์ิ จารุธีรนาท วทิ ยานิพนธ์น้ีเป็นส่วนหน่ึงของการศึกษาตามหลกั สูตรปรัชญาดุษฎีบณั ฑิต สาขาวิชาArchitectural Heritage Management and Tourism Plan 2.2 บัณฑิตวิทยาลัย มหาวิทยาลัยศิลปากร ปีการศึกษา 2560 ลิขสิทธ์ิของบณั ฑิตวทิ ยาลยั มหาวิทยาลัยศิลปากร THE INTERPRETATION OF SI SATCHANALAI By MR. Jaroonsak JARUDHIRANART A Thesis Submitted in Partial Fulfillment of the Requirements for Doctor of Philosophy (Architectural Heritage Management and Tourism) International Program Graduate School, Silpakorn University Academic Year 2017 Copyright of Graduate School, Silpakorn University 4 Title THE INTERPRETATION OF SI SATCHANALAI By Jaroonsak JARUDHIRANART Field of Study (Architectural Heritage Management and Tourism) International Program Advisor Supot Chittasutthiyan Graduate School Silpakorn University in Partial Fulfillment of the Requirements for the Doctor of Philosophy Dean of graduate school (Associate Professor Jurairat Nunthanid, Ph.D.) Approved by Chair person ( Kreangkrai Kirdsiri , Ph.D.) Advisor ( Supot Chittasutthiyan , Ph.D.) External Examiner (Professor Emeritus ORNSIRI PANIN ) D ABST RACT 53056954 : Major (Architectural Heritage Management and Tourism) International Program Keyword : Si
    [Show full text]
  • Characteristics of the 2011 Chao Phraya River Flood in Central Thailand
    Hydrological Research Letters 6, 41–46 (2012) Published online in J-STAGE (www.jstage.jst.go.jp/browse/HRL). DOI: 10.3178/HRL.6.41 Characteristics of the 2011 Chao Phraya River flood in Central Thailand Daisuke Komori1, Shinichirou Nakamura2, Masashi Kiguchi1, Asako Nishijima3, Dai Yamazaki1, Satoshi Suzuki1, Akiyuki Kawasaki1, Kazuo Oki1 and Taikan Oki1 1Institute of Industrial Science, The University of Tokyo, Japan 2“Wisdom of Water” (Suntory) Corporate Sponsored Research Program Organization for Interdisciplinary Research Projects, The University of Tokyo, Japan 3Japan Weather Association, Japan Abstract: Social Development Board, 2012). Many floods have been experienced in the past in the Chao Phraya River watershed, A massive flood, the maximum ever recorded in and floods on the same scale as the 2011 flood are expected Thailand, struck the Chao Phraya River in 2011. The total to occur in the future. In developing proper assessments and rainfall during the 2011 rainy season was 1,439 mm, which flood control measures to prepare for the next flood disaster, was 143% of the average rainy season rainfall during the it is important to develop a solid understanding of the actual period 1982–2002. Although the gigantic Bhumipol and situation surrounding this flood, and get to the root causes Sirikit dams stored approximately 10 billion m3 by early of the flood damage. October, the total flood volume was estimated to be 15 3 billion m . This flood caused tremendous damage, including OVERVIEW OF THE CHAO PHRAYA RIVER 813 dead nationwide, seven industrial estates, and 804 companies with inundation damage, and total losses estimated at 1.36 trillion baht (approximately 3.5 trillion Figure 1 shows a diagram of the Chao Phraya River yen).
    [Show full text]
  • Difficult Encounters Around “Monkey Cheeks”: Farmers' Interests and the Design of Flood Retention Areas in Thailand
    Received: 20 September 2018 Revised: 1 April 2019 Accepted: 6 May 2019 DOI: 10.1111/jfr3.12543 ORIGINAL ARTICLE Difficult encounters around “monkey cheeks”: Farmers' interests and the design of flood retention areas in Thailand Thanaporn Trakuldit1 | Nicolas Faysse1,2 1School of Environment, Resources and Development, Asian Institute of Abstract Technology, Bangkok, Thailand Flood retention areas are being increasingly promoted for flood risk management. 2Cirad, G-Eau Research Unit, Montpellier People living in these areas will accept them if their interests are taken into University, Montpellier, France account. The present study analyses the extent to which farmers' interests were Correspondence taken into account in two flood retention projects in Thailand. A feasibility study Nicolas Faysse, Asian Institute of was conducted in preparation for the first project which included public participa- Technology, Bangkok, Thailand. tion. The second project was a pilot project implemented in the same zone at a Email: [email protected] small scale. Participants in the public participation process and farmers living in Funding information proposed flood retention areas were interviewed for the purpose of the present Agence Nationale de la Recherche (French National Agency for Research) study. Agreement could have been reached between the farmers and the public agencies concerning the flood retention areas. However, the participation process did not enable frank discussion about the conditions under which farmers would accept the project. The second project was designed without public participation and offered very little compensation to farmers. In countries marked by power imbalances in water resources management, public agencies may impose flood retention areas, but the absence of agreements with farmers can reduce the effec- tiveness of the measure.
    [Show full text]
  • The Local Observed Trends and Variability in Rainfall Indices Over the Past Century of the Yom River Basin, Thailand
    J. Korean Soc. Hazard Mitig. ISSN 1738-2424(Print) Vol. 18, No. 4 (Jun. 2018), pp.41~55 ISSN 2287-6723(Online) https://doi.org/10.9798/KOSHAM.2018.18.4.41 www.kosham.or.kr 기후변화방재 The Local Observed Trends and Variability in Rainfall Indices Over the Past Century of the Yom River Basin, Thailand Ruetaitip Mama*, Kwansue Jung**, Butsawan Bidorn***, Matharit Namsai**** and Meiyan Feng***** Abstract A changing rainfall pattern can directly affect the frequency of occurrence of extreme event such as floods and droughts. These extreme events will cause future political conflicts, especially those dealing with water supply and flood management. The purpose of this study is to examine the variability of rainfall in the Yom River basin, Thailand, during the past 90 years (1921–2015). Based on rainfall data from 13 hydrological stations, long-term trends inrainfall and various rainfall-related extreme events, which consist of the annual total precipitation (PRCPTOT), consecutive dry days (CDD), consecutive wet days (CWD), number of heavy rainfall days (R10), number of very heavy rainfall days (R20), daily maximum rainfall (Rmax1), five-day maximum rainfall (Rmax5), and annual total rainy day (Rday) in the Yom River basin, were analyzed using the Mann-Kendall method with 95% confident level. The results suggest that for the PRCPTOT, Rmax1, and Rmax5 indices have experienced a significant increase trend in the western part of basin area. In addition, the decreasing trend was observed over 55% of basin considering for the CDD indices. Meanwhile, the CWD was found an increasing trend approximately 77% of the basin area except in the lower Yom River basin.
    [Show full text]
  • Zootaxa, Checklist of Catfishes, Recent and Fossil
    ZOOTAXA 1418 Checklist of catfishes, recent and fossil (Osteichthyes: Siluriformes), and catalogue of siluriform primary types CARL J. FERRARIS, JR. Magnolia Press Auckland, New Zealand CARL J. FERRARIS, JR. Checklist of catfishes, recent and fossil (Osteichthyes: Siluriformes), and catalogue of siluriform primary types (Zootaxa 1418) 628 pp.; 30 cm. 8 March 2007 ISBN 978-1-86977-058-7 (hardback) ISBN 978-1-86977-059-4 (Online edition) FIRST PUBLISHED IN 2007 BY Magnolia Press P.O. Box 41-383 Auckland 1346 New Zealand e-mail: [email protected] http://www.mapress.com/zootaxa/ © 2007 Magnolia Press All rights reserved. No part of this publication may be reproduced, stored, transmitted or disseminated, in any form, or by any means, without prior written permission from the publisher, to whom all requests to reproduce copyright material should be directed in writing. This authorization does not extend to any other kind of copying, by any means, in any form, and for any purpose other than private research use. ISSN 1175-5326 (Print edition) ISSN 1175-5334 (Online edition) 2 · Zootaxa 1418 © 2007 Magnolia Press FERRARIS Zootaxa 1418: 1–628 (2007) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2007 · Magnolia Press ISSN 1175-5334 (online edition) Checklist of catfishes, recent and fossil (Osteichthyes: Siluriformes), and catalogue of siluriform primary types CARL J. FERRARIS, JR. 2944 NE Couch Street, Portland, Oregon, 97232, U.S.A. E-mail: [email protected] Research Associate, National Museum of Natural History, Smithsonian Institution, Washington Research Associate, American Museum of Natural History, New York Research Associate and Honorary Fellow, California Academy of Sciences, San Francisco Table of contents Abstract ....................................................................................................................................................................................................
    [Show full text]
  • Effects of Dam Construction in the Wang River on Sediment Regimes in the Chao Phraya River Basin
    water Article Effects of Dam Construction in the Wang River on Sediment Regimes in the Chao Phraya River Basin Warit Charoenlerkthawin 1,2, Matharit Namsai 1,3, Komkrit Bidorn 2, Chaipant Rukvichai 1, Balamurugan Panneerselvam 4 and Butsawan Bidorn 1,2,* 1 Department of Water Resources Engineering, Chulalongkorn University, Bangkok 10330, Thailand; [email protected] (W.C.); [email protected] (M.N.); [email protected] (C.R.) 2 WISE Research Unit, Chulalongkorn University, Bangkok 10330, Thailand; [email protected] 3 The Royal Irrigation Department, Bangkok 10300, Thailand 4 Department of Civil Engineering, M. Kumarasamy College of Engineering, Karur, Tamilnadu 639113, India; [email protected] * Correspondence: [email protected] Abstract: The Wang River is one of the major tributaries of the Chao Phraya River (CPR) system in Thailand as the key riverine sediment source supplying the Chao Phraya Delta that has experienced severe shoreline retreat in the past six decades. Historical and observed river flow and sediment data measured during 1929–2019 were used to assess the variation in total sediment load along the Wang River and evaluate the effects of three major dam constructions on sediment supplied from the Wang River to the CPR. Results indicated that sediment loads increased toward downstream. Variation in long-term total sediment load (TSL) along the river suggested that construction of the Citation: Charoenlerkthawin, W.; Kiew Lom Dam in 1972 did not cause a reduction in sediment yield in the Wang River Basin because Namsai, M.; Bidorn, K.; Rukvichai, C.; it impounded less than 20% of the average annual runoff, while the Mae Chang and Kiew Koh Ma Panneerselvam, B.; Bidorn, B.
    [Show full text]
  • Sukhothai 7 Amphoe Khiri Mat 23 Amphoe Sawankhalok 28 Amphoe Si Satchanalai 29 Amphoe Thung Saliam 37 Amphoe Ban Dan Lan Hoi 40
    Contents How to get there 5 Attractions ! Amphoe Mueang Sukhothai 7 Amphoe Khiri Mat 23 Amphoe Sawankhalok 28 Amphoe Si Satchanalai 29 Amphoe Thung Saliam 37 Amphoe Ban Dan Lan Hoi 40 Events and Festivals 40 Interesting Activities 43 Cycling 43 Homestay!! 44 Local Products and Souvenirs 44 Souvenir Shops 48 Example of Tour Programmes 51 Facilities in Sukhothai 58 Accommodation 58 Restaurants 63 Car Rental 64 Useful Calls 64 !"#$%&'()*'++&&&" ",%-,%%&&&%.-/&01 4 Mini Light and Sound Presentation Sukhothai Night SUKHOTHAI !"#$%&'()*'++&&&- ",%-,%%&&&%.-"&01 5 Sukhothai was the !rst kingdom of Thailand established some 700 years ago. The province is located on the lower edge of the northern region, 427 kilometres north of Bangkok, and covers some 6,596 square kilometres. Established in around 1237-1257, Sukhothai literally means “Dawn of Happiness.” Phokhun Si Intharathit was the founder of the Phra Ruang Dynasty, Sukhothai’s !rst Dynasty. For 120 years as the capital of Thailand, Sukhothai was ruled by many kings. In this connection, the most dynamic monarch being King Ramkhamhaeng the Great, who created the Thai alphabet, laid the foundation for politics, monarchy, and religion, as well as, expanded its boundary of in"uence. Though the golden era of Sukhothai no more existed, tourists should bear in mind that respect and admiration for the renowned ruined twin cities of Sukhothai and Si Satchanalai is valued. Sukhothai is administratively divided into 9 districts (Amphoe); namely, Amphoe Mueang Sukhothai, Amphoe Kong Krailat, Amphoe Khiri Mat, Amphoe Thung Saliam, Amphoe Ban Dan Lan Hoi, Amphoe Si Satchanalai, Amphoe Si Samrong, Amphoe Sawankhalok, and Amphoe Si Nakhon.
    [Show full text]