Water Masses Characteristics at the Western Pasific Equator on August 2018

  • Duaitd Kolibongso Department Marine Science, University of Papua

Abstract

The Western Pacific Equator waters are a meeting place for water masses coming from the Northern and Southern Hemispheres. This study aims to identify the characteristics of water masses formed in the waters of Northern Papua. The study of water mass characteristics in the northern waters of Papua was carried out based on reanalysis data from the World Ocean Atlas (WOA) in August 2018. There were 12 stations divided into 3 transects to be analyzed in this study, namely transect 1 and transect 2 which stretched north-south and transect 3 which stretches east-west. The analysis were performed by method of the core layer and was processed with Sofware Ocean Data View (ODV). The results showed in the waters of North Papua there was a meeting of 2 water masses from the North Pacific and South Pacific. The water masses characteristics in latitudes <5 oLU are affected by surface and intermediates of the South Pacific carried by the Papua New Guinea Coastal Current that flows along the northern coast of Papua New Guinea and into Papua waters and beyond into the waters of the Halmahera Sea. Whereas the mass of water in latitudes > 5 oLU is dominated by surface and intermediate water masses from the North Pacific carried by North Equatorial Counter Current.

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References

Atmadipoera, A.S, Y. Kuroda, Pariwono, J. I. 2004. Water mass variation in the upper layer of Halmahera eddy region observed from TRITON buoy. Techno ocean ’04 Conference. Kobe, Japan.

Fine, R.A., Lukas R., Bingham F., Warnar M, and Gammon R. 1994. The Western Equatorial Pasific: A water mass crossroad. Journal Geophysis. Res. 90: 25063-25080.

Kashino, Y. M., Aoyama., Kawano, T., Hendiarti, N., Syaefudin, Y., Anantasena, K., Muneyama, dan Watanabe, H. 1996. The Water masses between Mindanao and New Guinea. Journal of Geophysical Research. 101 (C5): 12.391 – 12. 400.

Kashino, Y., Ueki I., Kuroda Y., Purwandi A. 2007. Ocean variability North of New Guinea Derived from TRITON Buoy Data. Journal Oceanography, 63: 325-333.

Koch-Larrouy, A., G. Madec, B. Blanke, and R. Molcard. 2008. Water Mass transformation along the Indonesian Throughflow in an OGCM. Ocean Dynamics, 58(3-4): 289-309

Nurhayati, 2006. Distribusi Vertikal Suhu, Salinitas, dan Arus di Perairan Morotai, Maluku Utara. Oseanologi dan Limnologi di Indonesia, 40: 29-41.

Purwandana, A. 2013. Sebaran Medan Massa, Medan Tekanan dan Arus Geostropik di Perairan Utara Papua pada Bulan Desember 1991. Prosiding Seminar Nasional Fisika IV Tahun 2013, Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Negeri Semarang (UNNES). FB1-FB10

Radjawane, I. M dan Hadipoetranto, P. P. 2014. Karateristik massa air di percabangan Arus Lintas Indonesia perairan Sangihe Talaud menggunakan data Index Satal 2010. Jurnal ilmu dan Teknologi Kelautan Tropis. 6(2): 525-536.

Schlitzer, R. 2012. Ocean Data View. http://odv.awi.de. [Diakses tanggal: 30 Agustus 2019]

Wyrtki, K. 1961. Physical Oceanography of Southeast Asian Waters. Naga Report, Volume 2. The University of California Scripps Institusion of Oceanography: La Jolla California. United States of America. 225p.
How to Cite
KOLIBONGSO, Duaitd. Water Masses Characteristics at the Western Pasific Equator on August 2018. JURNAL SUMBERDAYA AKUATIK INDOPASIFIK, [S.l.], v. 4, n. 1, p. 43-52, may 2020. ISSN 2550-0929. Available at: <https://ejournalfpikunipa.ac.id/index.php/JSAI/article/view/77>. Date accessed: 12 july 2020. doi: https://doi.org/10.46252/jsai-fpik-unipa.2020.Vol.4.No.1.77.
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Keywords:
North Pasific Water Masses, South Pasific Water Masses, Western Pasific equator Water
Published
2020-05-24
Section
Research Articles