Thermal Front Variability during the El Nino Southern Oscillation (ENSO) in the Banda Sea Using Remotely Sensed Data

Authors

  • Achmad Fachruddin Syah Study Program of Marine Science, University of Trunojoyo Madura, Jl. Raya Telang PO BOX 2 Kamal, Bangkalan,Madura, Indonesia
  • Siti Sholehah Study Program of Marine Science, University of Trunojoyo Madura, Jl. Raya Telang PO BOX 2 Kamal, Bangkalan,Madura, Indonesia

DOI:

https://doi.org/10.30564/jms.v3i2.2741

Abstract

The Banda Sea is one of the routes of global ocean currents that move from the Pacific Ocean to the Indian Ocean. This flow is known as Indonesian Through Flow (ITF). The Banda Sea is an area where warm and cold water masses meet, so it has the potential for a thermal front. This study aims to understand the variability of thermal front in the Banda Sea during the El Nino Southern Oscillation period. Southern Oscillation Index (SOI) and sea surface temperature (SST) data in 2010, 2012 and 2015 were used in this study. SOI data was obtained from http://www.bom.gov.au and SST data were obtained from http://oceancolor.gsfc.nasa.gov. The data were processed using ArcGIS 10.4 software and Ms. Office 2013. The results showed the La Nina period occurs in July - December 2010, the Normal period occurs in July - December 2012, and the El Nino period occurs in May - October 2015. In general, during La Nina, the mean SST has higher values than the other periods. On the other hand, the highest thermal front occurs during the El Niño period (10584), followed by the Normal period (7544) and the lowest during the La Niña period (5961), respectively.

Keywords:

El Nino, La Nina, Normal, Sea surface temperature

References

[1] Ratnawati, H. I., Hidayat, R., Bey, A., & June, T. Upwelling Di Laut Banda Dan Pesisir Selatan Jawa Serta Hubungannya Dengan ENSO Dan IOD. Jurnal Omni Akuatika, 2016, 12(3): 119-130.

[2] Sukresno, B., & Suniada, K, I. Observasi Pengaruh Enso Terhadap Produktifitas Primer Dan Potensi Perikanan Dengan Menggunakan Data Satelit Di Laut Banda. Globe, 2008, 10(2): 97-107.

[3] Yuggotomo, M. E., & Ihwan. 2014. Pengaruh Fenomena El Niño Southern Oscillation Dan Dipole Mode Terhadap Curah Hujan Di Kabupaten Ketapang. Jurnal Poitron, 2014, 4(2): 35-39.

[4] Suniada, K. I. Perbandingan Antara Informasi Suhu Permukaan Laut Dari Data Satelit Dengan Hasil Pemodelan Di WPP NKRI-716. Jurnal Bumi Lestari, 2016, 16(6): 32-37.

[5] Kunarso, Hadi, S., Ningsih, N., & Baskoro. 2011. Variabilitas Suhu Dan Klorofil A Di Daerah Upwelling Pada Variasi Kejadian ENSO Dan IOD Di Perairan Selatan Jawa Sampai Timor. Jurnal Ilmu Kelautan, 2011, 16(3): 171-180.

[6] Insanu, K, R., Handayani, H., Sukojo. Analisis Pemetaan Zona Penangkapan Ikan (Fishing Ground) Dengan Menggunakan Citra Satelit Tera Modis dan Parameter Oseanografi. Prosiding Seminar Nasional Managemen Teknologi XVII. Program Studi MMTITS. Surabaya.

[7] Jatisworo, D., & Murdimanto, A. Identifikasi Thermal Front di Selat Makassar dan Laut Banda. Prosiding Simposium Nasional Sains Geoinformasi III 2013. ISBN : 978-979-98521-4-4.

[8] Jatisworo, D. Kajian Spasial Dan Temporal Sebaran Front di Selatan Makassar Dan Laut Banda Terkait Variasi Musim. Tesis. Program Pasca Sarjana Penginderaan Jauh. Fakults Geografi. Universitas Gadjah Mada. Yogyakarta. 2017.

[9] Cayula, J.F., & Cornillon, P. Edge Detection Algorithm for SST Images. Journal of Atmospheric and Oceanic Technology, 1992, 9(1): 67-80.

[10] Cayula, J. F., & Cornillon, P. Multi-Image Edge Detection for SST Images. Journal of Atmospheric and Oceanic Technology, 1995, 12(4): 821-829.

[11] Besewni, Effendi, D. S., Agustineke, R., Nugroho, Nugroho, G. D., Susilo, A. W., & Suhadi (Eds.). Peta Keragaan Perikanan Tangkap di Wilayah Pengelolaan Perikanan. Republik Indonesia (WPP-RI). DirJen Perikanan Tangkap KKP RI, 2011, pp. iv+68.

[12] Hanintyo R., Hadianti S., Mahardhika R. M. P., & Islamy, F. Sebaran Musiman Kejadian Thermal Front Berdasarkan Citra Aqua-MODIS Di WPP-RI 714, 715 Dan 716 Seminar Nasional Penginderaan Jauh 2015.

[13] Kurnianingsih, T., Sasmito, B., & Prasetyo, Y. Analisis Sebaran Suhu Permukaan Laut, Klorofil-A, Dan Angin Terhadap Fenomena Upwelling Di Perairan Pulau Buru Dan Seram, Jurnal Geodesi Undip, 2017, 6(1), pp. 238-248.

[14] Oktaviani, A., Jumarang., & Ihwan. Kajian Elevasi Muka Air Laut Di Perairan Indonesia Pada Konsisi El Nino Dan La Nina. Jurnal Prisma Fisika, 2014, 2(1) : 06-10.

[15] Silvia. Analisis Daerah Penangkapan Ikan Cakalang (Katsuwonus Pelamis) Berdasarkan Suhu Permukaan Laut Dan Sebaran Klorofil-A Di Perairan Mentawai, Sumatera Barat. Bogor: IPB. 2009.

[16] Kumar, K. K., Kleeman, R., Cane, M.A., & Rajagopalan, B. Epochal changes in Indian monsoon-ENSO precursors. Geo Res Lett, 199, 26:75-78.

[17] Waileruny, W., Wiyono, E., Wisudo., Purbayanto., & Nurani. Musim Dan Daerah Penangkapan Ikan Cakalang Di Laut Banda Dan Sekitarnya Provinsi Maluku. Jurnal Teknologi Perikanan Dan Kelautan. 2014, 5(1): 41-54.

[18] Ahmad, Ayu, L., Syamsuddin, L., Purba, Noir, P. Kondisi Thermal Front Ditinjau Dari El Nino, Dan Arlindo Di Perairan Selatan Jawa Timur Dan Bali Pada Muson Timur. Jurnal Perikanan Dan Kelautan. 2017, 8 (1), 186-191.

[19] Zulmy, M. Pengaruh Monsun Dan El Nino Southern Oscillation (ENSO) Terhadap Variabilitas Thermal Front Di Perairan Laut Jawa.Skripsi. Universitas Diponegoro Semarang. 2017.

[20] Sukresno, B., Jatisworo, D., Kusuma, D, W. Analisis Multilayer Variabilitas Upwelling Di Perairan Selatan Jawa. Balai Riset Dan Observasi Laut. Bali. 2018, Hal 1-13.

[21] Maulidiyah, H. Ihwan, A. Jumarang. Penentuan Kejadian El Nino Dan La Nina Berdasarkan Nilai Southern Oscillation Indeks. Positron, 2012, 2(2): 6-14.

[22] Natalia, E, Kunarso, H. & Rifai. Variabilitas Suhu Permukaan Laut Dan Klorofil-A Kaitannya Dengan El Nino Southern Oscillation (Enso) Dan Indian Ocean Dipole (Iod) Pada Periode Upwelling 2010- 2014 Di Lautan Hindia (Perairan Cilacap). Jurnal Oseanografi. 2015, 4(4): 661-669.

[23] Aji, M. A. S. 2012. Pendugaan Periode Penyuburan Di Perairan Laut Banda Menggunakan Citra Satelit Seawifs Dan Citra Satelit NOAA. Skripsi. Departemen Ilmu Dan Teknologi Kelautan Fakultas Perikanan Dan Ilmu Kelautan. Institut Pertanian Bogor. Bogor, 2012.

Downloads

Issue

Vol. 3 , Iss. 2 (April 2021)

Article Type

Articles

License

Copyright and Licensing

The authors shall retain the copyright of their work but allow the Publisher to publish, copy, distribute, and convey the work.

Journal of Marine Science publishes accepted manuscripts under Creative Commons Attribution-NonCommercial 4.0 International License (CC BY-NC 4.0). Authors who submit their papers for publication by Journal of Marine Science agree to have the CC BY-NC 4.0 license applied to their work, and that anyone is allowed to reuse the article or part of it free of charge for non-commercial use. As long as you follow the license terms and original source is properly cited, anyone may copy, redistribute the material in any medium or format, remix, transform, and build upon the material.

License Policy for Reuse of Third-Party Materials

If a manuscript submitted to the journal contains the materials which are held in copyright by a third-party, authors are responsible for obtaining permissions from the copyright holder to reuse or republish any previously published figures, illustrations, charts, tables, photographs, and text excerpts, etc. When submitting a manuscript, official written proof of permission must be provided and clearly stated in the cover letter.
The editorial office of the journal has the right to reject/retract articles that reuse third-party materials without permission.

Journal Policies on Data Sharing

We encourage authors to share articles published in our journal to other data platforms, but only if it is noted that it has been published in this journal.