Spatio-temporal analysis of river morphological changes and erosion detection using very high resolution satellite image

9th IGRSM International Conference and Exhibition on Geospatial & Remote Sensing

地球科学;计算机科学

Mohamad, N.^1 ; Khanan, M.F.A.^1 ; Musliman, I.A.^1 ; Kadir, W.H.W.^1 ; Ahmad, A.^1 ; Rahman, M.Z.A.^1 ; Jamal, M.H.^2 ; Zabidi, M.^3 ; Suaib, N.M.^4 ; Zain, R.M.^4

Faculty of Geoinformation and Real Estate, Universiti Teknologi Malaysia, Johor Bahru

81310, Malaysia^1

Faculty of Civil Engineering, Universiti Teknologi Malaysia, Johor Bahru

81310, Malaysia^2

Faculty of Electrical Engineering, Universiti Teknologi Malaysia, Johor Bahru

81310, Malaysia^3

Faculty of Computer, Universiti Teknologi Malaysia, Johor Bahru

81310, Malaysia^4

关键词: Erosion detection;    Maximum likelihood classifications;    Morphological changes;    Riverbank erosion;    Spatiotemporal analysis;    Specific location;    Very high resolution;    Very high resolution satellite images;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/169/1/012020/pdf
DOI  :  10.1088/1755-1315/169/1/012020

学科分类：计算机科学（综合）

来源: IOP

【 摘 要 】

Spatio-temporal analysis of Kilim River using Very High-Resolution (VHR) satellite image between the years of 2005 and 2012 are vital to assess river morphological changes and erosion detection over the specific time duration. Therefore, this study utilizes remote sensing and Geographical Information System (GIS) capabilities to identify the channel migration and shifting as well as to calculate the rate of erosion and accretion. Classification of the river from Quickbird and WorldView-2 images is carry out using Maximum Likelihood Classification (MLC) technique whereas feature selection tool performs to extract river feature from the raw image. Subsequently, river feature been overlaid to identify the changes of riverbank pattern and to calculate the rate of riverbank erosion in terms of area. The result shows the total area of erosion is 27252.959 m2 and the total area of accretion is 6079.999 m2. A maximum erosion of 6993.102 m2 detected at Section E while maximum accretion of 681.026 m2 spotted at Section D. The rates of riverbank erosion are 3406.62 m2/year while the rates for accretion are 759.999 m2/years between 2005 and 2012. Hence, the output of this study enables Langkawi Development Authority (LADA) and other stakeholders to recognize the specific location, which severely affected by erosion and accretion as well as to spot the area experienced huge river channel shifting.