Didik Purwantoro
Department of Civil Engineering and Planning, Faculty of Engineering, Universitas Negeri Yogyakarta, Yogyakarta 55281, Indonesia

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Sediment Transport Modeling at the Bogowonto River Bend Using HEC RAS 6.6 Didik Purwantoro; Mawiti Infantri Yekti; Rossita Yuli Ratnaningsih; Nanda Nur Rofi’ah; Farah Mayra
INERSIA lnformasi dan Ekspose Hasil Riset Teknik Sipil dan Arsitektur Vol. 21 No. 2 (2025): December
Publisher : Universitas Negeri Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21831/inersia.v21i2.91818

Abstract

River bend erosion is a major concern for river engineers because it affects channel stability and navigation safety. Erosion along the outer bank and deposition along the inner bank are the primary processes responsible for the meandering pattern of rivers. This study investigates the effect of discharge variations on scour depth in a meandering reach of the Bogowonto River using numerical modeling with HEC-RAS 6.6. Simulations were carried out for six discharge scenarios corresponding to return periods of 2,5, 10, 20, 50, and 100 years (Q2, Q5, Q10, Q20, Q50, and Q100). The historical rainfall data collected from 2002 to 2021. Limantara Unit Hydrograph used for rainfall-runoff modelling. The HEC-RAS simulation results of the 2-year return period (Q2) reveal that sedimentation occurs at five points along the Bogowonto River bend in Purworejo District. In particular the greatest accumulation occurred at the apex of the bend (STA 17), where the bed sediment thickness reached 4.175 m at the Q100 discharge. The simulation results show a uniform sedimentation pattern across the entire bend cross-section, likely due to model limitations that prevent detailed representation of cross-flow patterns.
Long-Term Rainfall Variability and Seasonal Shifts in Relation to Pranatamangsa in the Rongkop Karst Region, Indonesia Qonaah Rizqi Fajriani; Suwartanti Nayono; Satoto Endar Nayono; Didik Purwantoro
INERSIA lnformasi dan Ekspose Hasil Riset Teknik Sipil dan Arsitektur Vol. 22 No. 1 (2026): May
Publisher : Universitas Negeri Yogyakarta

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.21831/inersia.v22i1.95431

Abstract

Climate change has altered rainfall characteristics and seasonal patterns. This matter affects mostly rainfed agricultural systems in karst regions. This study aims to analyze rainfall characteristics, extreme rainfall events, seasonal shifts, and the reliability of traditional seasonal knowledge (pranata mangsa) in the Rongkop karst area, Indonesia. The dataset used in this study are long-term daily rainfall data from Rongkop stations for the period 1986–2021. The rainfall data then convert to dasarian (10-day) temporal resolution. The daily rainfall was classified into intensity categories, while seasonal onset was determined based on rainfall thresholds. Trend analysis was conducted using the Mann–Kendall test and Sen’s slope estimator. The results indicate that Rongkop has moderate annual rainfall, with an average of 2012 mm, and no significant trend in total rainfall. However, there is a significant increase in the frequency of heavy rainfall events (>50 mm/day), indicating a shift towards higher rainfall intensity. Seasonal analysis shows variability in the onset of the rainy season between late August and late December, and the dry season between early February and mid-May. Seasonal duration also varies significantly, with extended dry spells and increased rainfall during the dry season. The results indicate increasing inconsistencies between traditional and observed rainfall patterns, with very high rainfall occurring during the dry season and very low rainfall during the wet season. The onset of the wet and dry seasons also exhibits significant variability beyond the expected seasonal boundaries. These findings suggest that although traditional seasonal forecasts (pranatamangsa) still reflect general climate patterns, their reliability for agricultural planning has declined due to increasing rainfall variability, extreme events, and large-scale climate phenomena such as El Niño and La Niña, particularly in rainfed karst areas. Therefore, integrating traditional seasonal knowledge with modern climatological analysis is crucial to support adaptive agricultural management, particularly in karst areas.