Automatic Detection of Decadal Shoreline Change on Northern Coastal of Gresik, East Java _ Indonesia

5th Geoinformation Science Symposium 2017

地球科学;计算机科学

Fuad, M.A.Z.^1,2 ; Fais D A, M.^1

Faculty of Fisheries and Marine Science, Brawijaya University, Jl. Veteran-Malang, 65145, Indonesia^1

Marine Resources Exploration and Management Research Group (MEXMA), Brawijaya University, Indonesia^2

关键词: Area of interest;    Automatic Detection;    DSAS;    Landsat imagery;    Man-made structures;    Multi-temporal satellite images;    Shoreline change;    Shoreline change analysis;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/98/1/012001/pdf
DOI  :  10.1088/1755-1315/98/1/012001

学科分类：计算机科学（综合）

来源: IOP

【 摘 要 】

The Coastal zone is a dynamic region that has high environmental and economic values. This present research focuses on the analyzing the rate of shoreline change using multi-temporal Landsat Imagery and Digital Shoreline Analysis Systems (DSAS) along the northern part of Gresik coastal area, East Java Indonesia. Five village were selected for analysis; Campurejo, Dalegan, Prupuh, Ngemboh, and Banyuurip. Erosion and Accretion were observed and detected on Multi-temporal satellite Images along the area of interest from 1972 - 2016. Landsat Images were radiometrically and geometrically corrected before using for analysis. Coastline delineation for each Landsat image was performed by MNDWI method before digitized for quantitative shoreline change analysis. DSAS was performed for quantitative analysis of Net Shoreline Movement (NSM) and End Point Rate (EPR). The results indicate that in the study area accretion and abrasion was occurred, but overall abrasion was dominated than accretion. The remarkable shoreline changes were observed in the entire region. The highest abrasion area was occurred in Ngemboh village. From 1972 to 2016, coastline was retreat 242.56 meter to the land and the rate of movement was -5.54m/yr. In contrast, Campurejo area was relatively stable due to the introduction of manmade structure, i.e. Jetty and Groin. The Shoreline movement and the rate of movement in this area were -6.11m and -0.12 m/yr respectively. The research represents an important step in understanding the dynamics of coastal area in this area. By identification and analysis of coastline evolution, the stake holder could perform a scenario for reducing the risk of coastal erosion and minimize the social and economic lost.