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Identification of flash flood hazard zones in mountainous small watershed of Aceh Besar Regency, Aceh Province, Indonesia
Azmeria, Hadihardaja I.K.b, Vadiya R.a
a Department of Civil Engineering, Syiah Kuala University, Banda Aceh, Aceh Province, 23111, Indonesia
b Faculty of Civil and Environmental Engineering, Institute of Technology Bandung (ITB), Bandung, West Java Province, 40132, Indonesia
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]© 2016 National Authority for Remote Sensing and Space Sciences.Flash-floods develop at space and time scales that conventional observation systems were not able to monitor for rainfall, stream flow and sediment discharge. This condition resulted in greater casualties and tremendous economic losses. One of the regions in Indonesia affected by the flash floods was Aceh Besar Regency. It was located in Krueng Teungku watershed. The flash floods were recurring events, which occurred in 1987 and 2000. The disaster reocurred on January 2, 2013 at 19:30 P.M. with the huge impact. This study aimed to analyze the factors affecting flash flood hazards and to obtain flash flood hazard zones at the Krueng Teungku watershed. The method used in this study was weighted overlay technique through Geographic Information System (GIS). The result revealed the information about the flash flood hazard zones at Krueng Teungku watershed as the model for the early warning. Through the development of this model, flood forecasting capabilities in the watershed without measuring devices can be improved. This paper provided the review of factors that affect the incidence of flash flooding, including the factors of peak discharge, slope, watershed shape, stream gradient, damming, drainage density, erosion, slope stability and reservoir volume. The information factors were expected as a contribution for research agencies and government (Aceh Disaster Management Agency) to guide the disaster risk reduction (DRR) activities of flash floods.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Disaster management,Disaster risk reductions,Flash flood,Hazard zones,Information factor,Observation systems,Overlay techniques,Sediment discharge[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]Disaster management,Flash flood,Hazard zones,Krueng Teungku watershed[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1016/j.ejrs.2015.11.001[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]