DATA INSTANT Download

Buat teman-teman yang tertarik tuk neliti dan buat tulisan tentang kondisi oseanografi perairan Indonesia khususnya daerah Selat Makassar, Lifamatola, Lombok, Ombai dan Timor, saat ini data hasil kegiatan INSTANT sudah dapat didownload secara gratis.

Data-data yang tersedia berupa hasil mooring CTD (Salinitas dan temperatur) serta arus pada lokasi tersebut. Nah buat teman-teman yang mau download silahkan klik disini .

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Publikasi Pelayaran Kebangsaan 2008 bidang Biologi

Distribution of Phytoplankton at Sunda Strait

(1) Roni Koneri, (2) Rosi Faslah and (3) Sapto Pamungkas

(1) Biology Department Faculty of Mathematic and Natural Science University of Sam Ratu Langi Manado
(2) Biology Department Faculty of Mathematic and Natural Science University of Mataram
(3) Marine Science Department, Faculty of Fisheries and Marine Science University of Diponegoro, Semarang

ABSTRACT
Phytoplankton have important rule in marine ecosystem, information about distribution of phytoplankton biomass is very needed. The research on distribution of phytoplankton biomass in Sunda Strait was conducted during November 2008. Samples were taken from 10 stations using Kitahara net. Total phytoplankton abundance varied from 0.0193 ml/m³ - 0.2359 ml/m³. Phytoplankton Biomass graduated from maximum value at the near coastal area to the minimum at offshore. The higher concentration of phytoplankton observed at north part of Sunda Strait.

Keywords: distribution, biomass, phytoplankton, Sunda Strait.

Publikasi Pelayaran Kebangsaan 2008 bidang Fisika

Distribusi Temperatur, Salinitas dan Densitas Bulan November 2008 di Selat Sunda

Oleh

Heron Surbakti¹⁾ Elizabeth Vorandra²⁾ Tjiong Giok Pin ³⁾Eko Minarto⁴⁾ Muzilman Musli⁵⁾ Eka Saputra⁶⁾

ABSTRAK

Selat Sunda adalah salah satu pintu masuk massa air antara Samudera Hindia dan perairan Indonesia. Untuk mengetahui masukan massa air di Selat Sunda, dilakukan pengukuran parameter hidrooseanografi pada akhir November 2008 yang dilanjutkan dengan penggambaran pola sebaran temperatur dan salinitas. Pengaruh daratan terutama datang dari Pulau Jawa. Pada beberapa lokasi sepanjang pesisir Pulau Jawa terpantau pasokan air tawar dengan salinitas yang rendah (St.2) dan suplai panas dari darat (St.8). Pengaruh dari darat tidak hanya terlihat pada permukaan laut, tetapi sampai dengan kedalaman 25-30 m. Sedangkan dari sebaran melintang dan mendatar terlihat adanya masukan massa air Samudera Hindia yang memiliki salinitas lebih tinggi menuju Selat Sunda. Dalam tulisan ini juga digunakan data penelitian massa air bulan Juli 2001 sebagai perbandingan untuk kondisi musim Timur.

Kata Kunci : Selat Sunda, massa air, pengaruh darat, pengaruh Samudera Hindia.

ABSTRACT

Sunda Strait is one of the water mass passages from Indian Ocean to Indonesian waters. To study the through flow of Indian Ocean water masses through Sunda Strait and the affects of Java and Sumatera main lands to the strait, an oceanographic investigation was conducted in November 2008 using the RV Baruna Jaya VIII. The affects of Java main land was observed at several points along the Java coast where the less saline water recorded from the surface to the depth of 25-30 m at the northern part of the survey area and the high water temperature was recorded at the southern part. Analyzed the vertical distribution of temperature and salinity through the cross section at the middle of the strait it was shown that the Indian Ocean water entered the Sunda Strait. In this research, the value of Sunda Strait water mass in July 2001 also used as comparition for east monsson condition.

Key words: Sunda strait, water masses, main land affects, Indian Ocean

¹⁾ Universitas Sriwijaya ²⁾Institut Teknologi Bandung ³⁾Universitas Indonesia ⁴⁾Institut Teknologi Sepuluh November ⁵⁾Universitas Nasional ⁶⁾Universitas Syah Kuala

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6. Nonlinear Physical Oceanography: A Dynamical Systems Approach to the Large Scale OceanCirculation and El Nino (Atmospheric and Oceanographic Sciences Library)
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8. Tropical Cyclones: Climatology and Impacts in the South Pacific by James P Terry
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