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Effect of Extreme ENSO and IOD on the Variability of Chlorophyll-a and Sea Surface Temperature in the North and South of Central Java Province

ILMU KELAUTAN: Indonesian Journal of Marine Sciences · Vol. 28 No. 1 (2023) · hlm. 1–11

DOI
10.14710/ik.ijms.28.1.1-11
ISSN
2406-7598, 0853-7291
Terbit
2023-03-15
Penerbit
Marine Science Department Diponegoro University
Bahasa
eng
Lisensi
creativecommons.org/licenses/by-sa/4.0

Abstrak

Chlorophyll-a (chl-a) and Sea Surface Temperature (SST) are important indicators of air-sea interaction and primary productivity. It has been widely known that the variability of chl-a and SST in the waters of Central Java Province (CJP) is influenced by the monsoonal cycle. Previous studies did not clearly describe the variability of chl-a and SST when compared to other cycles. This present study investigated the variability of chl-a and SST influenced by monsoonal cycles, IOD, and ENSO in both CJP waters. Our analysis is based on satellite observations and uses daily data to compile climatological data. The analysis found differences between the variability of chl-a and SST during the monsoonal cycle and ENSO-IOD extreme conditions. During the monsoonal cycle, the maximum (minimum) chl-a (SST) in northern CJP is 0.7 mg.L-1 (28.5ºC) is observed in the West Monsoon, and in the southern CJP is 1.5 mg.L-1 (25.5ºC) is observed in the East Monsoon. In addition, the analysis reveals that the ENSO and IOD extremes do not clearly alter the variability of chl-a and SST in the northern CJP. However, ENSO and IOD extremes have clearly altered the variability of chl-a and SST in the southern CJP. The highest impact to variability of chl-a and SST occurred during IOD+ extreme (2019), where the range of value chl-a (SST) in south CJP is 0,35–4,57 mg.L-1 (23,29 – 30,49ºC). The value of chl-a (SST) is greater than 4 mg.L-1 (less than 24ºC) are observed in the east monsoon. It is caused by the intensity of lifting the mass of water from deeper waters to the sea surface, which possibly supplies the nutrients in the surface waters. The result of the investigation showed that the increasing of chl-a and decreasing of SST in the northern CJP dominant by monsoonal cycle and southern CJP dominant by monsoonal cycle and ENSO – IOD.

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  • Diponegoro University
  • Bandung Institute of Technology
  • University of Maryland, College Park
  • Navamindradhiraj University
  • National Research and Innovation Agency
  • Sebelas Maret University
  • Australian Antarctic Division
  • Afiliasi tidak diketahui
  • Organisasi berbeda
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Tampilkan sebagai tabel
Rekan penulisOrganisasiArtikel bersama
Lilik MaslukahDiponegoro University4
Elis IndrayantiDiponegoro University4
Muhammad ZainuriDiponegoro University4
Denny Nugroho SugiantoDiponegoro University4
Parichat WetchayontNavamindradhiraj University3
Widodo Setiyo PranowoNational Research and Innovation Agency3
Sugeng WidadaDiponegoro University2
Baskoro RochaddiDiponegoro University2
Aris IsmantoDiponegoro University2
Nining Sari NingsihBandung Institute of Technology2
Safwan HadiBandung Institute of Technology2
Indra Budi PrasetyawanDiponegoro University2
Rikha WidiaratihDiponegoro University2
Agus TriantoDiponegoro University2
Diah Permata WijayantiDiponegoro University2
Radisya N NissaDiponegoro University2
DestioDiponegoro University2
Daenk HimawaDiponegoro University2
Anis Yasmin SabilaDiponegoro University1
Agus SupangatAfiliasi tidak diketahui1
Wiweka WiwekaAfiliasi tidak diketahui1
Purwanto PurwantoSebelas Maret University1
Galuh PermatasariDiponegoro University1
Warsito AtmodjoDiponegoro University1
Muhammad Shulhan JihadiDiponegoro University1
Virginia L. Andrews-GoffAustralian Antarctic Division1
Esti RudianaDiponegoro University1
Nirwani NirwaniDiponegoro University1
Subagiyo SubagiyoDiponegoro University1
Ria Azizah TnDiponegoro University1
Retno HartatiDiponegoro University1
Ita WidowatiDiponegoro University1
Ali RidloDiponegoro University1
Endang SupriyantiniDiponegoro University1

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Sumber metadata: OAI-PMH (metadata jurnal) http://ejournal.undip.ac.id/index.php/ijms/oai, pertama di-harvest 8 Nov 2026, terakhir terlihat 8 Nov 2026.
Metadata asli (oai_dc)
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	<dc:title xml:lang="en-US">Effect of Extreme ENSO and IOD on the Variability of Chlorophyll-a and Sea Surface Temperature in the North and South of Central Java Province</dc:title>
	<dc:creator>Kunarso, Kunarso</dc:creator>
	<dc:creator>Ismunarti, Dwi Haryo</dc:creator>
	<dc:creator>Rifai, Azis</dc:creator>
	<dc:creator>Munandar, Bayu</dc:creator>
	<dc:creator>Wirasatriya, Anindya</dc:creator>
	<dc:creator>Susanto, Raden Dwi</dc:creator>
	<dc:subject xml:lang="en-US">Chlorophyll-a; SST; ENSO; IOD; Central Java</dc:subject>
	<dc:description xml:lang="en-US">Chlorophyll-a (chl-a) and Sea Surface Temperature (SST) are important indicators of air-sea interaction and primary productivity. It has been widely known that the variability of chl-a and SST in the waters of Central Java Province (CJP) is influenced by the monsoonal cycle. Previous studies did not clearly describe the variability of chl-a and SST when compared to other cycles. This present study investigated the variability of chl-a and SST influenced by monsoonal cycles, IOD, and ENSO in both CJP waters. Our analysis is based on satellite observations and uses daily data to compile climatological data. The analysis found differences between the variability of chl-a and SST during the monsoonal cycle and ENSO-IOD extreme conditions. During the monsoonal cycle, the maximum (minimum) chl-a (SST) in northern CJP is 0.7 mg.L-1 (28.5ºC) is observed in the West Monsoon, and in the southern CJP is 1.5 mg.L-1 (25.5ºC) is observed in the East Monsoon. In addition, the analysis reveals that the ENSO and IOD extremes do not clearly alter the variability of chl-a and SST in the northern CJP. However, ENSO and IOD extremes have clearly altered the variability of chl-a and SST in the southern CJP. The highest impact to variability of chl-a and SST occurred during IOD+ extreme (2019), where the range of value chl-a (SST) in south CJP is 0,35–4,57 mg.L-1 (23,29 – 30,49ºC). The value of chl-a (SST) is greater than 4 mg.L-1 (less than 24ºC) are observed in the east monsoon. It is caused by the intensity of lifting the mass of water from deeper waters to the sea surface, which possibly supplies the nutrients in the surface waters. The result of the investigation showed that the increasing of chl-a and decreasing of SST in the northern CJP dominant by monsoonal cycle and southern CJP dominant by monsoonal cycle and ENSO – IOD. </dc:description>
	<dc:publisher xml:lang="en-US">Marine Science Department Diponegoro University</dc:publisher>
	<dc:date>2023-03-15</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
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	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://ejournal.undip.ac.id/index.php/ijms/article/view/50064</dc:identifier>
	<dc:identifier>10.14710/ik.ijms.28.1.1-11</dc:identifier>
	<dc:source xml:lang="en-US">ILMU KELAUTAN: Indonesian Journal of Marine Sciences; Vol 28, No 1 (2023): Ilmu Kelautan; 1-11</dc:source>
	<dc:source>2406-7598</dc:source>
	<dc:source>0853-7291</dc:source>
	<dc:language>eng</dc:language>
	<dc:relation>https://ejournal.undip.ac.id/index.php/ijms/article/view/50064/pdf</dc:relation>
	<dc:rights xml:lang="en-US">Copyright (c) 2023 ILMU KELAUTAN: Indonesian Journal of Marine Sciences</dc:rights>
	<dc:rights xml:lang="en-US">https://creativecommons.org/licenses/by-sa/4.0</dc:rights>
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