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Monitoring Coastal Line Changes Using the Digital Shoreline Analysis System (DSAS) Method in the Coastal Area of Mekkatta Village, Mejene Regency

Jurnal IPTEKS Pemanfaatan Sumberdaya Perikanan · Vol. 10 No. 2 (2023) · hlm. 107–118

DOI
10.20956/jipsp.v10i2.32060
ISSN
2614-5014, 2355-729X
Terbit
2023-12-13
Penerbit
Hasanuddin University
Bahasa
en
Lisensi
creativecommons.org/licenses/by/4.0

Abstrak

Analysis of coastline changes in Mekkata Village from 2013 to 2023 was conducted using the baseline of the nearest coastline to the mainland. This baseline was used as a reference point for transects measuring changes. The shoreline encompasses the coastline during the research period. Net Shoreline Movement (NSM) was employed to differentiate between erosion and accretion in the study area, showing an average shoreline change value of -9.72 meters towards the mainland, indicating predominant erosion. According to DSAS, it is observed that the coastline of Mekkata Village experienced erosion along 41 transects, while 31 transects exhibited accretion, highlighting significant changes. The most notable erosion area was identified along transects 60, 61, and 62, indicating consistent land reduction. Meanwhile, the most accretion-prone transects were 11, 12, and 13, signifying substantial land addition. The predominant erosion process is suspected to be influenced by the gentle slope of the coastal area and the composition of sand material. Human activities such as deforestation and river mouths also contribute to erosion. The absence of coastal protection structures allows direct waves and currents to impact the shore, potentially causing erosion. Meanwhile, accretion areas around river mouths indicate the formation of emergent land or deltas.

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  • Universitas Muhammadiyah Mamuju
  • Universitas Halu Oleo
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Rekan penulisOrganisasiArtikel bersama
Muhammad YusufUniversitas Halu Oleo1
Haryanto AsriAfiliasi tidak diketahui1
Muhammad YusufUniversitas Muhammadiyah Mamuju1
Muhammad YusufUniversitas Muhammadiyah Mamuju1
NurlianaUniversitas Muhammadiyah Mamuju1
Widya UtamiUniversitas Muhammadiyah Mamuju1
Hardianty NurUniversitas Muhammadiyah Mamuju1

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Sumber metadata: OAI-PMH (metadata jurnal) https://journal.unhas.ac.id/index.php/iptekspsp/oai, pertama di-harvest 5 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en">Monitoring Coastal Line Changes Using the Digital Shoreline Analysis System (DSAS) Method in the Coastal Area of Mekkatta Village, Mejene Regency</dc:title>
	<dc:creator xml:lang="en">Asri, Haryanto </dc:creator>
	<dc:creator xml:lang="en">Novitasari, Femiliani</dc:creator>
	<dc:subject xml:lang="en">Coastline</dc:subject>
	<dc:subject xml:lang="en">, Coastal Geomorphological Changes</dc:subject>
	<dc:subject xml:lang="en">DSAS</dc:subject>
	<dc:subject xml:lang="en">Erosion and Accretion</dc:subject>
	<dc:subject xml:lang="en">NSM</dc:subject>
	<dc:description xml:lang="en">Analysis of coastline changes in Mekkata Village from 2013 to 2023 was conducted using the baseline of the nearest coastline to the mainland. This baseline was used as a reference point for transects measuring changes. The shoreline encompasses the coastline during the research period. Net Shoreline Movement (NSM) was employed to differentiate between erosion and accretion in the study area, showing an average shoreline change value of -9.72 meters towards the mainland, indicating predominant erosion. According to DSAS, it is observed that the coastline of Mekkata Village experienced erosion along 41 transects, while 31 transects exhibited accretion, highlighting significant changes. The most notable erosion area was identified along transects 60, 61, and 62, indicating consistent land reduction. Meanwhile, the most accretion-prone transects were 11, 12, and 13, signifying substantial land addition. The predominant erosion process is suspected to be influenced by the gentle slope of the coastal area and the composition of sand material. Human activities such as deforestation and river mouths also contribute to erosion. The absence of coastal protection structures allows direct waves and currents to impact the shore, potentially causing erosion. Meanwhile, accretion areas around river mouths indicate the formation of emergent land or deltas.</dc:description>
	<dc:publisher xml:lang="en">Hasanuddin University</dc:publisher>
	<dc:date>2023-12-13</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:type xml:lang="en">Research article</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://journal.unhas.ac.id/index.php/iptekspsp/article/view/32060</dc:identifier>
	<dc:identifier>10.20956/jipsp.v10i2.32060</dc:identifier>
	<dc:source xml:lang="en">Jurnal IPTEKS Pemanfaatan Sumberdaya Perikanan; Vol. 10 No. 2 (2023); 107 - 118</dc:source>
	<dc:source>2614-5014</dc:source>
	<dc:source>2355-729X</dc:source>
	<dc:source>10.20956/jipsp.v10i2</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://journal.unhas.ac.id/index.php/iptekspsp/article/view/32060/11013</dc:relation>
	<dc:relation>10.20956/jipsp.v10i2.32060.g11013</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2023 Jurnal IPTEKS Pemanfaatan Sumberdaya Perikanan</dc:rights>
	<dc:rights xml:lang="en">https://creativecommons.org/licenses/by/4.0</dc:rights>
</oai_dc:dc>