Numerical Analysis of Shoreline Changes along the Coast Batu Hiu-Bojong Salawe, Pangandaran Regency, West Java Province, Indonesia

Authors

  • Subiyanto Subiyanto Department of Marine Science, Faculty Fishery and Marine Science, Universitas Padjadjaran, Sumedang 45363, Indonesia
  • Yuyun Hidayat Department of Statistic, Faculty of Mathematics and Natural Sciences, Universitas Padjadjaran, Sumedang 45363, Indonesia
  • Saeful Anwari Department of Marine Science, Faculty Fishery and Marine Science, Universitas Padjadjaran, Sumedang 45363, Indonesia
  • Mustafa Mamat Faculty of Informatics and Computing, Universiti Sultan Zainal Abidin, 21300 Kuala Terengganu, Terengganu, Malaysia
  • Mohammad Fadli Ahmad Faculty Ocean Engineering Technology and Informatics, Universiti Malaysia Terengganu, 21300 Kuala Terengganu, Terengganu, Malaysia
  • Novan Tofany Research Center for Computing, National Research and Innovation Agency (BRIN), Soekarno Science and Technology Zone, Cibinong 16911, Indonesia
  • Sudradjat Supian Department of Mathematic, Faculty of Mathematics and Natural Sciences, Sumedang 45363, Indonesia

DOI:

https://doi.org/10.37934/araset.42.2.5871

Keywords:

Abrasion, Accretion, Batu Hiu-Bojong Salawe, DSAS, Shoreline change

Abstract

Shoreline change poses a significant challenge in coastal regions, leading to issues such as abrasion, soil erosion, and the loss of valuable land. This problem is prevalent in various areas of Pangandaran, particularly in the Batu Hiu-Bojong Salawe coastal region of Pangandaran Regency, West Java, Indonesia. The objective of this study is to analyse and quantify the distance and rate of shoreline changes occurring over a decade (2010-2019) in the Batu Hiu-Bojong Salawe coastal area. Utilizing ArcMap software and the Digital Shoreline Analysis System (DSAS), this research aims to provide insights into the coastal dynamics, drawing analytical points from comparable studies for a comprehensive understanding. Batu Hiu's western coast faces substantial erosion (29.70m, LLR 3.10 m/year, EPR 3.22 m/year), while the east experiences accretion (52.76m, LLR/EPR 5.49 m/year, 5.72 m/year). Coastal dynamics, influenced by rocky structures, lead to sedimentation and erosion. Bojong Salawe Beach sees noteworthy accretion (83.01m, LRR/EPR 8.88 m/year, 9.00 m/year), with a maximum at transect 85 (134.5m, LRR 14.27 m/year, EPR 14.58 m/year). Erosion at transects 104 and 107 averages 30.47m, with LLR/EPR rates of 3.41 m/year and 3.3 m/year. The Cijulang River estuary contributes to coastal stability, resulting in significant accretion. This information is vital for coastal management, offering insights to address erosion and accretion impacts in Batu Hiu and Bojong Salawe coastal areas.

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Author Biographies

Subiyanto Subiyanto, Department of Marine Science, Faculty Fishery and Marine Science, Universitas Padjadjaran, Sumedang 45363, Indonesia

subiyanto@unpad.ac.id

Yuyun Hidayat, Department of Statistic, Faculty of Mathematics and Natural Sciences, Universitas Padjadjaran, Sumedang 45363, Indonesia

yuyun.hidayat@unpad.ac.id

Saeful Anwari, Department of Marine Science, Faculty Fishery and Marine Science, Universitas Padjadjaran, Sumedang 45363, Indonesia

saeful.anwari58@gmail.com

Mustafa Mamat, Faculty of Informatics and Computing, Universiti Sultan Zainal Abidin, 21300 Kuala Terengganu, Terengganu, Malaysia

must@unisza.edu.my

Mohammad Fadli Ahmad, Faculty Ocean Engineering Technology and Informatics, Universiti Malaysia Terengganu, 21300 Kuala Terengganu, Terengganu, Malaysia

fadhli@umt.edu.my

Novan Tofany, Research Center for Computing, National Research and Innovation Agency (BRIN), Soekarno Science and Technology Zone, Cibinong 16911, Indonesia

novan.tofany@brin.go.id

Sudradjat Supian, Department of Mathematic, Faculty of Mathematics and Natural Sciences, Sumedang 45363, Indonesia

sudradjat@unpad.ac.id

Published

2024-04-03

Issue

Section

Articles