Email this article 
Hide
Show all
Spatial Analysis of the River Line and Land Cover Changes in the Kampar River Estuary: The Influence of the Bono Tidal Bore Phenomenon
Aprizon Putra(1*), Ulung Jantama Wisha(2), Gunardi Kusumah(3)(1) Research Institute for Coastal Resources and Vulnerability Padang-Painan km 16 Padang-West Sumatra 25245, Indonesia
(2) Research Institute for Coastal Resources and Vulnerability Padang-Painan km 16 Padang-West Sumatra 25245, Indonesia
(3) Research Institute for Coastal Resources and Vulnerability Padang-Painan km 16 Padang-West Sumatra 25245, Indonesia
(*) Corresponding Author
Abstract
The Kampar River estuary is well known for a tidal-bore phenomenon called ‘Bono waves’. The emergence of Bono waves has a significant influence on the estuary system of Kampar River. Scoured materials, resulting from the hydraulic jump of the tidal bore, are carried into the middle of the river. These materials are then deposited when the velocity of the river decreases as a result of the collision of the tidal current from the sea and the river flow. The aim of this was to determine the area of erosion and sedimentation with respect to the river line and perform land-cover change analysis for the area around the Kampar River estuary for the years of 1990, 2007, 2010 and 2016. The method employed was the supervised maximum likelihood (SML) classifications, which uses an overlay technique to yield alternate information on the river line and land-cover changes in the form of time-series data. The largest erosion occurred during 1990–2007, for which the average change reached 2.36 ha/year. The smallest erosion occurred during 2010–2016, when the change reached 0.41 ha/year. The largest land-cover change was found during 1990–2016, which occurred in the land for agriculture/plantations (11.57 ha/year), building/settlement (48.11 ha/year) and scrubland (30.88 ha/year). The other types of land cover, such as bare land and sediment deposition, varied every single year. The changes to the river line are caused by land-cover changes, and the Bono waves that lead to erosion and sedimentation that is not stable in the middle of the river and downstream.
Keywords
References
Agency for Research and Development (ARD) of Natural Resources Conservation Technology (NRCT). (2013). Forestry Profile 33 Province, 632. (In Indonesian) Retrieved from http://balitek-ksda.or.id/2014/02/profil-kehu-tanan-33-provinsi/.
Anna, A.N., Kaeksi, R.W and Astuti, W.A. (2010). The Analysis of Hydrological Characteristics Parameter as The Effect of Landuse Changing Using Landsat Imagery From 1997 to 2002 in Sukoharjo District. Forum Geografi, Vol. 24, No. 1, pp. 57 – 72.
Berrios, P.H. (2004). Spatial Analysis of The Differences Between Forest Land Use and Forest Cover Using GIS and RS. A case study in Telake Watershed, Pasir district, East Kalimantan. MSc Thesis. The Netherlands: ITC.
Cenci, L., Disperati, L., Persichillo, M.G., Oliveira, E.R., Alves, F.L and Phillips, M. (2017). Integrating remote sensing and GIS techniques for monitoring and modeling shoreline evolution to support coastal risk management. J. GIScience & Remote Sensing. Vol 0, No. 0, pp. 1–21.
Chanson, H. (2001). Flow Field in A Tidal Bore: A physical Model. Proc. 29th IAHR Congress, Beijing, Theme E, Tsinghua University. Beijing. pp. 365 – 373.
Danoedoro, P. (2012). Introduction to Digital Remote Sensing. Yogyakarta: C.V Andi Offset. (In Indonesian)
Darwish, K., Smith, S. E., Torab, M., Monsef, H and Hussein, O. (2016). Geomorphological Changes along the Nile Delta Coastline between 1945 and 2015 Detected Using Satellite Remote Sensing and GIS. Journal of Coastal Research, pp. 786 – 794.
Department of Binamarga and Water Resources (DBWR) of Pelalawan Regency. (2010). Final Report DED Kampar River Retaining Cliff Teluk Meranti Village Pelalawan Regency, Riau. (In Indonesian)
Edison, E., Mubarak and Bathara, L. (2009). Characteristics and Sediment Potential in Kampar River Estuary. J. Aquatic science. Vol. 7, No. 2, pp. 11 – 22.
Goslee, S.C. (2011. Analyzing Remote Sensing Data in R: The Landsat Package. J. Statistical Software. Vol. 43, No. 4, pp. 1 – 23.
Harjadi, B. (2009). Monitoring and Evaluation of Watershed With Remote Sensing and Geography Information System. Forum Geografi. Vol. 23, No.2, pp. 139 – 152.
Harjadi, B. (2010). Land Cover Analysis in Grindulu Catchment Area Using Remote Sensing and Geographic Information System. Forum Geografi. Vol. 24, No.1, pp. 85 – 91.
Jaya, L. M. G. (2013). Changes in Land Cover Analysis in The Gulf Coast Kendari Using High Resolution Satellite Image (Period: 2003 – 2009). Forum Geografi. Vol. 27, No. 2, pp. 179 – 188.
Kaliraj, S., Chandrasekar, N and Ramachandran, K.K. (2017). Mapping of coastal landforms and volumetric change analysis in the south west coast of Kanyakumari, South India using remote sensing and GIS techniques. The Egyptian Journal of Remote Sensing and Space Science, Vol. 20, No.2, pp. 265–282.
Leh, M., Bajwa, S and Chaubey, I. (2013). Impact of land use change on erosion risk: an integrated remote sensing, geographic information system and modeling methodology. Land Degradation & Development, Vol. 24, No. 5, pp. 409–421.
Mubarak, Sulaiman, A and Efriyeldi. (2017). Environmental Effect of Tidal Bore Propagation in Kampar River. MATEC Web of Conferences 103, 04015.
Pierik, H. J., Cohen, K. M and Stouthamer, E. (2016). A new GIS approach for reconstructing and mapping dynamic late Holocene coastal plain palaeogeography. J. Geomorphology, Vol. 270 (Supplement C), pp. 55–70.
Putra, A.,Husrin, S and Ridwan, N.N.H (2014). Shoreline Changes Analysis in Bali`s Northeast Coast Using Remote Sensing Dataset (Case Study USAT Liberty Ship Site Location, Tulamben). Proceedings of the National Marine Seminar. pp. 143 – 159.
Putra, A., Husrin S and Kelvin, J. (2015). Identification of Changes Area of Greenbelt in Pangandaran Regency, West Java Using Landsat. J. Akuatika. Vol.4, No. 1, pp. 59 – 67.
Rahmawan, G.A., Wisha, U.J and Husrin, S. (2017). Bathymetry and tidal analysis in the estuary of Kampar: generating the propagation of tidal wave “Undular Bore Bono”. J. Ilmiah Geomatika, Vol. 22, No. 2, pp. 57 – 64.
Richards, J. A. (1999). Remote Sensing Digital Imagery Analysis, Berlin: Springer-Verlag.
Rozali, R., Mubarak, M and Irvina, N. (2016). Patterns of Distribution Total Suspended Solid (TSS) in River Estuary Kampar Pelalawan. Student Online Journal Faculty of Fisheries and Marine Science Riau University. Vol. 3, No. 2, pp 1 – 8.
Seenath, A., Wilson, M and Miller, K. (2016). Hydrodynamic versus GIS modelling for coastal flood vulnerability assessment: Which is better for guiding coastal management?. Ocean & Coastal Management, Vol. 120 (Supplement C), pp 99–109.
Setiady, D. (2010). Estimated Potential Reserves of Sea Sand which exists in Muara Kampar Waters of Riau islands. Buletin Sumber Daya Geologi. Vol. 5, No. 1, pp 20– 25.
Suryantoro, A. (2003). The Easiness of Interpretation of SPOT XS Imagery and TM Landsat to Identify Object of The Cover of Urban Area. Forum Geografi. Vol. 17, No. 1, pp. 96 – 105.
Susanti, P.D and Miardini, A. (2017). The impact of Land Use Change on Water Pollution Index of Kali Madiun Sub-watershed. Forum Geografi. Vol. 31, No.1, pp. 128 – 137.
Valjarević, A., Živković, D., Valjarević, D., Stevanović, V and Golijanin, J. (2014). GIS Analysis of Land Cover Changes on the Territory of the Prokuplje Municipality. The Scientific World Journal, Vol. 2014, Article ID 805072, 8 pages.
Winarso, G., Syarif, B and Judijanto. (2001). The Potential Application of Remote Sensing Data for Coastal Study. Singapura: Proceeding on 22nd Asian Conference on Remote Sensing, CRISP NUS and Asian Association on Remote Sensing.
Wisha, U. J and Maslukah, L. (2017). Nutrient Condition of Kampar Big River Estuary: Distribution of N and P Concentrations Drifted by Tidal Bore “Bono”. Indonesian Journal of Marine Science. Vol. 22, No.3, pp 137–146.
Yulistyanto, B. (2009). The Phenomenon of Bono Rising Wave in Kampar River Estuary. J. Dinamika Teknil Sipil, SI. 9, pp 19–26.
Article Metrics
Abstract view(s): 1156 time(s)PDF: 459 time(s) HTML: 875 time(s)
Refbacks
- There are currently no refbacks.
