BASIN MODELING IN BOYONG-CODE RIVER USING openLISEM AND PCRASTER

Flashflood becomes destructing and deadly hazard through its overwhelming discharge with rapid run-off velocity. It forms as a large quantity of water body that comes in sudden and collide everything on its way. One exposed target of flashfloods deadly hazard is riparian settlements in densely popul...

وصف كامل

محفوظ في:
التفاصيل البيبلوغرافية
المؤلفون الرئيسيون: , Shakti Rahadiansyah, , Prof. Dr.rer.nat Junun Sartohadi, M.Sc.
التنسيق: Theses and Dissertations NonPeerReviewed
منشور في: [Yogyakarta] : Universitas Gadjah Mada 2014
الموضوعات:
ETD
الوصول للمادة أونلاين:https://repository.ugm.ac.id/131056/
http://etd.ugm.ac.id/index.php?mod=penelitian_detail&sub=PenelitianDetail&act=view&typ=html&buku_id=71497
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الوصف
الملخص:Flashflood becomes destructing and deadly hazard through its overwhelming discharge with rapid run-off velocity. It forms as a large quantity of water body that comes in sudden and collide everything on its way. One exposed target of flashfloods deadly hazard is riparian settlements in densely populated city. The research proposal aims to build a model for a retention basin in the Boyong-Code Watershed. In order to mitigate the impact of flashflood in The City of Yogyakarta and other towns down valley, modeling of flashflood is undertaken by using PCRaster and LISEM. The result of the research is shows the modeling result of multiple scenarios. It can be concluded that rebuilding appropriate sabo dams after volcanic eruption is the highest impact in reducing flashflood peak discharge (reduction down to 16.46% of total occurred flashflood peak discharge). Furthermore the application of retention basin in Boyong-Code River can reduce flashfloods peak discharge down to 11.86%. Retention basin application with its economical low cost and positive ecological approach can be considered as securing infrastructure against flashfloods if non expensive cost approach is wished. The statistic test result shows that the model is valid to be run. Total map error projection of 10% is achieved by multiple statistical parameters of MA%E = 6.71% and ground check binomial probability value = 91.14%. In calibration process, factor of porosity = 0.68 is used as it derived from the lowest ranging average of 0.58 and 0.78.