Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models

A coupling of a 1-D flood routing model and quasi 2-D floodplain inundation model is applied for mapping spacetime flood extent. The routing model is formulated based on a non-linear storage-discharge relationship which is converted from an observed and synthetic rating curve. To draw the rating c...

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Main Authors: Kowit Boonrawd, Chatchai Jothityangkoon
Format: Article
Language:English
Published: Prince of Songkla University 2015-04-01
Series:Songklanakarin Journal of Science and Technology (SJST)
Subjects:
Online Access:http://rdo.psu.ac.th/sjstweb/journal/37-2/37-2-8.pdf
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spelling doaj-622bc49cc1e648048d908e44370e37a52020-11-25T01:12:49ZengPrince of Songkla UniversitySongklanakarin Journal of Science and Technology (SJST)0125-33952015-04-01372171181Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation modelsKowit Boonrawd0Chatchai Jothityangkoon1School of Civil Engineering, Institute of Engineering, Suranaree University of Technology, Mueang, Nakhon Ratchasima, 30000 Thailand.School of Civil Engineering, Institute of Engineering, Suranaree University of Technology, Mueang, Nakhon Ratchasima, 30000 Thailand.A coupling of a 1-D flood routing model and quasi 2-D floodplain inundation model is applied for mapping spacetime flood extent. The routing model is formulated based on a non-linear storage-discharge relationship which is converted from an observed and synthetic rating curve. To draw the rating curve, required parameters for each reaches are estimated from hydraulic properties, floodplain geometry and vegetation and building cover of compound channels. The shape of the floodplain is defined by using fitting exercise based on the reverse approach between past and simulated inundation flood extent, to solve the current problem of inadequate topographic input data for floodplain. Mapping of daily flood can be generated relying on flat water levels. The quasi 2-D raster model is tested and applied to generate more realistic water surface and is used to estimate flood extent. The model is applied to the floodplains of Chiang Mai, north of Thailand and used to estimate a time series of hourly flood maps. Extending from daily to hourly flood extent, mapping development provides more details of flood inundation extent and depth.http://rdo.psu.ac.th/sjstweb/journal/37-2/37-2-8.pdfUpper Ping Riverflood mapraster modelrating curve
collection DOAJ
language English
format Article
sources DOAJ
author Kowit Boonrawd
Chatchai Jothityangkoon
spellingShingle Kowit Boonrawd
Chatchai Jothityangkoon
Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models
Songklanakarin Journal of Science and Technology (SJST)
Upper Ping River
flood map
raster model
rating curve
author_facet Kowit Boonrawd
Chatchai Jothityangkoon
author_sort Kowit Boonrawd
title Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models
title_short Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models
title_full Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models
title_fullStr Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models
title_full_unstemmed Mapping temporal extent of Chiang Mai floods using coupled 1-D and quasi 2-D floodplain inundation models
title_sort mapping temporal extent of chiang mai floods using coupled 1-d and quasi 2-d floodplain inundation models
publisher Prince of Songkla University
series Songklanakarin Journal of Science and Technology (SJST)
issn 0125-3395
publishDate 2015-04-01
description A coupling of a 1-D flood routing model and quasi 2-D floodplain inundation model is applied for mapping spacetime flood extent. The routing model is formulated based on a non-linear storage-discharge relationship which is converted from an observed and synthetic rating curve. To draw the rating curve, required parameters for each reaches are estimated from hydraulic properties, floodplain geometry and vegetation and building cover of compound channels. The shape of the floodplain is defined by using fitting exercise based on the reverse approach between past and simulated inundation flood extent, to solve the current problem of inadequate topographic input data for floodplain. Mapping of daily flood can be generated relying on flat water levels. The quasi 2-D raster model is tested and applied to generate more realistic water surface and is used to estimate flood extent. The model is applied to the floodplains of Chiang Mai, north of Thailand and used to estimate a time series of hourly flood maps. Extending from daily to hourly flood extent, mapping development provides more details of flood inundation extent and depth.
topic Upper Ping River
flood map
raster model
rating curve
url http://rdo.psu.ac.th/sjstweb/journal/37-2/37-2-8.pdf
work_keys_str_mv AT kowitboonrawd mappingtemporalextentofchiangmaifloodsusingcoupled1dandquasi2dfloodplaininundationmodels
AT chatchaijothityangkoon mappingtemporalextentofchiangmaifloodsusingcoupled1dandquasi2dfloodplaininundationmodels
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