Modeling flood characteristics in the Krueng Keureuto river basin in North Aceh regency using the Jams/J2000 application

Abstract

Abstract Significant land use changes in the Krueng Keureuto River basin exacerbate flooding annually. Despite intensive flood studies, there’s no mapped information on past and future flood inundation. Flood discharge parameters rely on empirical formulas, overlooking climate factors and flood event data, crucial in flood analysis due to climate change. To comprehensively understand flood characteristics, this research employs the JAMS/J2000 application on climatological data (2010-2020), land use, soil type, and geological maps. Using HRU-Web, Hydrologic Response Units (HRUs) are derived for J2000 modeling, producing four runoff components: overland flow, interflow, fast groundwater, and slow groundwater. Notably, the highest overland flow, or flood runoff, was 23.21 mm on December 26, 2014, with 40.69 mm/day rainfall. Interflow peaked at 6.72 mm on October 8, 2011, with 18.10 mm/day rainfall. Fast groundwater reached 1.28 mm on November 30, 2019, with 13.18 mm/day rainfall, and slow groundwater peaked at 1.04 mm on November 13, 2020, with 48.87 mm/day rainfall. This study provides comprehensive insights into the complex dynamics of flood characteristics in the Krueng Keureuto River basin.