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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Prince of Songkla University
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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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1725164857555156992 |