Analysis of the Impacts of Land Use Change on Hydrological Responses to Support Water and Food Security in the Tukad Unda Watershed

  • I Made Alit Widnyana Institut Sains dan Teknologi Nahdlatul Ulama Bali
  • Husnayaen Institut Sains dan Teknologi Nahdlatul Ulama Bali
  • Adrian Pratama Putra Institut Sains dan Teknologi Nahdlatul Ulama Bali
Keywords: land-use change, peak discharge, Snyder Synthetic Unit Hydrograph (SUH), effective rainfall, Tukad Unda Watershed.

Abstract

Land-use changes can affect the hydrological characteristics of a watershed by altering the ability of the land surface to infiltrate, retain, and convey rainfall. This study aims to analyze changes in peak flood discharge resulting from land-use changes in the Tukad Unda Watershed between 2014 and 2024 using the Snyder Synthetic Unit Hydrograph (SUH) method. The analysis included land-use change identification, runoff coefficient determination, design rainfall analysis, hourly rainfall distribution, effective rainfall estimation, and transformation of effective rainfall into flood hydrographs using the Snyder SUH method. The results showed that the watershed runoff coefficient increased from 0.38 in 2014 to 0.40 in 2024, indicating an increase in the proportion of rainfall contributing to direct runoff. The watershed covers an area of 2,315,048 ha or 231.50 km², with a main river length of 51.8 km and a distance from the outlet to the watershed centroid of 20.4 km. The Snyder SUH was used to characterize the watershed response and transform effective rainfall for return periods of 2, 5, 10, 25, 50, and 100 years. Land-use changes between 2014 and 2024 were also reflected in an increase in Composite Curve Number (CN) from 55.77 to 60.73 and Composite Imperviousness (IMP) from 4.8% to 6.2%. These changes resulted in higher effective rainfall in 2024 compared with 2014. The Snyder SUH modeling indicated an increase in peak discharge, particularly for the 100-year return period, from 55.03 m³/s in 2014 to approximately 119.00 m³/s in 2024. The results indicate that land-use changes in the Tukad Unda Watershed contribute to increased runoff and peak flood discharge. These findings highlight the importance of land-use management that maintains watershed infiltration and water-retention functions as part of efforts to reduce flood risk and support sustainable water resources management.

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References

Agusalim, M., & Nanda, A. R. (2018). Perbandingan Hidrograf Satuan Amatan Dan Hidrograf Satuan Sintesis (Das Maros Sub Das Maros Tompubulu). Teknik Hidro, 11(1), 1–11. https://doi.org/10.26618/th.v11i1.2435

Anam, S; Noerhayati, E; Rachmawati, A. (2020). Studi Pengembangan Jaringan Irigasi Sprinkler Berbasis Gravitasi di Desa Poncokusumo Kabupaten Malang. Universitas Islam Malang, 8(3), 162–173.

Andi Besse Rimba, Geetha Mohan, Saroj Kumar Chapagain, Andi Arumansawang, Carolyn Payus, Kensuke Fukushi, Husnayaen, Takahiro Osawa, R. A. (2021). Impact of population growth and land use and land cover (LULC) changes on water quality in tourism-dependent economies using a geographically weighted regression approach. Environmental Science and Pollution Research. https://doi.org/10.1007/s11356-020-12285-8

Andi Setiawan dan Edi Susanto. (2019). Penentuan Liku Kalibrasi Debit (Rating Curve) pada Musim Hujan di Daerah Aliran Sungai (DAS) Deli. Jurnal Ilmiah Rekayasa Pertanian Dan Biosistem, Vol. 7, No, 157–165.

Armston, J. D. (2009). Prediction and validation of foliage projective cover from Landsat-5 TM and Landsat-7 ETM+ imagery. Journal of Applied Remote Sensing, 3(1). https://doi.org/10.1117/1.3216031

Atharinafi, Z., & Wijaya, N. (2021). Land Use Change and Its Impacts on Surface Runoff in Rural Areas of the Upper Citarum Watershed ( Case Study : Cirasea Sub- watershed ). Journal of Regional and City Planning, 32(1), 36–55. https://doi.org/10.5614/jpwk.2021.32.1.3

Badan Standardisasi Nasional. (2016). SNI 2415:2016 Tata cara perhitungan debit banjir rencana.

Barid, B., & Afanda, B. O. (2022). Increasing peak flow of snyder synthetic hydrograph units in the serenan sub-watershed of Bengawan Solo Watershed. Jurnal ASTONJADRO, 2018, 616–626.

Bosmans, J. H. C., Beek, L. P. H. Van, Sutanudjaja, E. H., & Bierkens, M. F. P. (2017). Hydrological impacts of global land cover change and human water use. 2005, 5603–5626.

Bruijnzeel, L. A. (2004). Hydrological functions of tropical forests : not seeing the soil for the trees ? (Vol. 104). https://doi.org/10.1016/j.agee.2004.01.015

Faoziyah, U., Rosyaridho, M. F., & Panggabean, R. (2024). Unearthing Agricultural Land Use Dynamics in Indonesia : Between Food Security and Policy Interventions. Jurnal MDPI, 1–29.

Herdiaprila, T., & Hartati, E. (2023). Penentuan Koefisien Limpasan Rata-Rata (Cr) Tata Guna Lahan Kelurahan Sukamiskin Kecamatan Arcamanik Kota Bandung. VIII–2.

Indarto, I., & Herlinda, N. D. (2020). Aplikasi Metode Pemisahan Aliran Dasar Berbasis Grafis Digital: Studi Pendahuluan Di Wilayah DAS Brantas. Jurnal Sumber Daya Air, 16(1), 11–22.

Indriyani, M., & Amalia, R. S. (2022). Analisa Debit Puncak Menggunakan Pendekatan Metode Hidrograf Satuan Sintetis ( HSS ) Snyder dan HEC-HMS ( Peak Discharge Analysis Using Synthetic Unit Hydrograph Method ( HSS ) Snyder and HEC-HMS Approach ). 6, 48–57.

Iresh, A. D. S., Dilthara, G. W. A. S., & Sugeeshwara, S. P. C. (2024). Estimation of Catchment Parameters of Snyder ’ s Synthetic Method for Water Resources Planning and Flood Management in Sri Lanka. ENGINEER.

Kahffi, A., & Lipu, S. (2021). Analisis Hidrograf DAS Poso dengan Metode Hidrograf Satuan Sintetis Snyder dan Hidrograf Satuan Sintetis Soil Conversation Service (SCS). Civil Engineering Journal on Research and Development, 121–128. https://doi.org/10.22487/renstra.v2i2.334

Kayitesi, N. M., Guzha, A. C., & Mariethoz, G. (2022). Impacts of land use land cover change and climate change on river hydro-morphology- a review of research studies in tropical regions. Journal of Hydrology, 615(PA), 128702. https://doi.org/10.1016/j.jhydrol.2022.128702

Koneti, S., Sunkara, S. L., & Roy, P. S. (2018). Hydrological Modeling with Respect to Impact of Land-Use and Land-Cover Change on the Runoff Dynamics in Godavari River Basin Using the HEC-HMS Model. https://doi.org/10.3390/ijgi7060206

Kristianto, A. B., Nyoman, N. I., Sila, D. I. G. B., & Yekti, M. I. (2019). Comparative Model of Measured Unit Hydrograph ( Case Study of Tukad Pakerisan Watershed ). 7(1), 21–31.

Permatasari, R. (2017). Pengaruh Perubahan Penggunaan Lahan terhadap Rezim Hidrologi DAS ( Studi Kasus : DAS Komering ). 24(1), 91–98. https://doi.org/10.5614/jts.2017.24.1.11

Putri, D. A. I., Widiarti, W. Y., & Halik, G. (2020). DAMPAK PERUBAHAN TATA GUNA LAHAN TERHADAP DEBIT PUNCAK DI SUB DAS TALANG KABUPATEN JEMBER. 16(1), 30–38.

Suprayogi, I., Trimaijon, & M. (2014). Model Prediksi Liku Kalibrasi Menggunakan Pendekatan Jaringan Saraf Tiruan (ZST) (Studi Kasus : Sub DAS Siak Hulu). Jurnal Online Mahasiswa Fakultas Teknik Universitas Riau, 1(1), 1–18.

Watershed, L., & Çalı, A. (2025). Exploring Hydrological Response to Land Use / Land Cover Change Using the SWAT + Model in the Iznik.

Wijaya, O. T., Yudianto, D., Fitriana, F., & Sanjaya, S. (2024). PREDIKSI DAMPAK PERUBAHAN TATAGUNA LAHAN TERHADAP DEBIT LIMPASAN , STUDI KASUS : GEREJA RANCASARI PREDICTION OF LAND USE CHANGE IMPACT ON RUNOFF , CASE STUDY : RANCASARI. Jurnal Sumber Daya Air, 20(2), 87–98.

Yuli Yani, P. R., Saidah, H., & Wirahman, L. (2021). Pola Distribusi Hujan Jam-Jaman Di Stasiun Hujan Jurang Sate Dan Stasiun Hujan Lingkok Lime Pada Wilayah Lombok Tengah. Spektrum Sipil, 8(1), 41–54.

Zulfa, G. F., Purnaditya, N. P., Wigati, R., Subekti, S., & Priyambodho, B. A. (2023). Prediction of Snyder Synthetic Unit Hydrograph Coefficient for Cidurian Watershed. Jurnal Teknik Sipil, 12(2), 271. https://doi.org/10.36055/fondasi.v12i2.22046

Published
2026-11-09
How to Cite
[1]
Widnyana, I.M.A., Husnayaen and Putra, A.P. 2026. Analysis of the Impacts of Land Use Change on Hydrological Responses to Support Water and Food Security in the Tukad Unda Watershed. Jurnal Ilmiah Kanderang Tingang. 17, 2 (Nov. 2026), 355-369. DOI:https://doi.org/10.37304/jikt.v17i2.461.