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All Journal BULETIN OSEANOGRAFI MARINA Jurnal Mirai Management Phinisi Integration Review AL-ATHFAAL : JURNAL ILMIAH PENDIDIKAN ANAK USIA DINI BJRA (Bongaya Journal of Research in Accounting) Jurnal Eduscience (JES) Besaung : Jurnal Seni Desain dan Budaya Jurnal Sains Riset Jurnal Ilmiah Profesi Pendidikan Jurnal Chart Datum PINISI Discretion Review JEKPEND Jurnal Ekonomi dan Pendidikan Amina REMITTANCE: JURNAL AKUNTANSI KEUANGAN DAN PERBANKAN Annual Conference on Islamic Early Childhood Education Edunomia : Jurnal Ilmiah Pendidikan Ekonomi International Journal of Social Science, Educational, Economics, Agriculture Research, and Technology (IJSET) Shautuna: Jurnal Ilmiah Mahasiswa Perbandingan Mazhab Muhasabatuna: Jurnal Akuntansi Syariah Jurnal Ilmu Akuntansi dan Bisnis Syariah (AKSY) International Journal of Social Science, Education, Communication and Economics AKUNSIKA: Jurnal Akuntansi dan Keuangan Seminar Nasional Pengabdian Kepada Masyarakat Jurnal Maritim Malahayati JURNAL PARADIGMA: Journal of Sociology Research and Education Sabangka Abdimas Jurnal Pengabdian Masyarakat Sabangka Future Academia : The Journal of Multidisciplinary Research on Scientific and Advanced Celebes Journal of Community Services Jurnal Sistem Informasi, Akuntansi dan Manajemen J-CEKI As-Syirkah: Islamic Economic & Financial Journal
Muhammad Azis
Fakultas Ekonomi Universitas Negeri Makassar
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Journal : BULETIN OSEANOGRAFI MARINA

 1 
Karakteristik Struktur Lapisan Termoklin Di Laut Andaman Dalam 4 Monsun Selama 1 Tahun Rahmatullah, Amri; Asmoro, Nuki Widi; Azis, Muhammad; Pranowo, Widodo Setiyo; Setiyadi, Johar
Buletin Oseanografi Marina Vol 13, No 1 (2024): Buletin Oseanografi Marina
Publisher : Universitas Diponegoro

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.14710/buloma.v13i1.54877

Abstract

Suhu air laut menjadi salah satu parameter penting dalam bidang oseanografi. Salah satunya adalah termoklin, yaitu lapisan perairan dengan perubahan suhu yang cepat diantara lapisan yang berbeda. Karakteristik laut Andaman banyak yang belum diulas terutama pengaruh periodisitas monsun terhadap struktur lapisan termoklin. Penelitian ini menggunakan metode penelitian kuantitatif deskriptif dengan data model dari Copernicus. Tujuan penelitian ini untuk mengidentifikasi dan menganalisis karakteristik struktur lapisan termoklin di laut Andaman. Hasil pengolahan data menunjukkan lapisan termoklin dalam 4 monsun secara menyeluruh. Sebaran batas atas termoklin berada pada kisaran kedalaman 13,47-109,73 m dan suhu antara 29,87-20.36˚C. Sebaran batas bawah berada pada kisaran kedalaman antara 130,67-155,85 m dan suhu antara 23,85-16,83˚C. Karena didominasi pengaruh monsun sehingga batas atas termoklin terdangkal ditemukan pada monsun Peralihan I dan batas bawah paling dalam pada monsun Timur dan Peralihan II.  Struktur lapisan termoklin berada pada rentang ketebalan termoklin dari 17,4-80,28 m dan rata-rata ketebalan termoklin sebesar 47,18 m. Ketebalan maksimum ditemukan pada monsun Peralihan I dengan ketebalan hingga 80,28 m. Peningkatan ketebalan termoklin pada Monsun Peralihan I terjadi akibat pengaruh angin, SPL yang meningkat  dan masuknya Equatorial Jet yang membawa arus lebih hangat dan East Indian Current (EIC) yang berputar tetap searah jarum jam di Utara Laut Andaman.The sea temperature is one of the important parameters in oceanography. One of them is the thermocline, which is a layer of water with rapid temperature changes between different layers. Many characteristics of the Andaman Sea have not been reviewed, especially the effect of monsoon periodicity on the structure of the thermocline layer. This research uses descriptive quantitative research methods with model data from Copernicus.  This study aims to identify and analyze the characteristics of thermocline layer structure in the Andaman Sea. The results of data processing show the thermocline layer in 4 monsoons as a whole. The distribution of the upper boundary of the thermocline is in the range of 13.47-109.73 m depth and temperature between 29.87-20.36˚C. The lower boundary distribution is in the range of depths between 130.67-155.85 m and temperatures between 23.85-16.83˚C. Due to the dominant influence of monsoon, the shallowest upper thermocline was found in the first monsoon and the deepest lower thermocline in the second monsoon.  The thermocline layer structure ranges in thermocline thickness from 17.4-80.28 m, with an average thermocline thickness of 47.18 m. The maximum thickness is found in the Transitional I monsoon with a thickness of up to 80.28 m. The increase in thermocline thickness in Monsoon Transitional I occurs due to the influence of winds, increased SPL and the entry of the Equatorial Jet which brings warmer currents and the East Indian Current (EIC) which rotates clockwise in the North of the Andaman Sea.
Co-Authors Abadi, Ridfan Rivaldy Abd. Rasyid Syamsuri Abduh, Amirullah Abdul Karim Adiaksa, Harvan Aldayanti, Nur Alhieza, Nur Amartika, Christine Delia Anwar Ramli Anwar, Azwar Armayadi, Yoga Ashar, Muhammad Ashar, Muhammad Ashari, Elza Rahayu Asmoro, Nuki Widi Asrida Asrida, Asrida Azis, Fajriani Azisah, Nur Cahaya, Muthia Nur Dedi Harianto Dedi Kurniawan Desi, Natsar Dewi, Sasmita Dunakhir, Samirah Dwi Utami Fadillah, Rifai Fajar Arwadi Fathirah, Dian Fijrianti, Alda Hadrianti, Siska Hamzah, Hajrah Hamzah, Linduaji Hariany Idris Hasanah , Niswatun Hasyim, Sitti Hajerah Hermawati Hermawati, Hermawati Hidayah, Hafidz Muhammad Hidayah, Khairul Idris, Fardini Inanna, Inanna Kamaludin Kamija, Kamija l Imam Fatoni, Khoirol Lubis, Fahrul Ramadhan M. Ridwan Tikollah Masnawaty Muchtar, Nur Fadilah Muhammad Jafar, Muhammad Muhammad Kholis, Muhammad Muhammad Rakib Mukhammad Idrus Munawarah, Nita Madinatul Musari, Ila Musfira Muslem Muslem, Muslem Muthaharah, Fitria muttaqinah, Andi Ratu Muwahid, Fadli Muzaroddin, Ihrof Najamuddin Najamuddin, Najamuddin Ningsih, Nur Rubiati Nisah , Khairun Nur Afiah, Nur Nuraisyiah Nuraisyiah, Nuraisyiah Nurzalsabilah Pamungkas, Putra Purnama Sari Putra, Muh Ardiansyah Putri, Deby Octafiani Qayyum, Abd. Rahman Qomariah, Bunga Nur Rahmatullah, Amri Rasul, Imra Ukhriana Ratu Winda, Gusrianti Razak, Nur Rahmatika Rijal, Abdul Ritonga, Almiftahul Jannah Rosnaini Daga Rusdi, Nur Risma S, Masnawaty Sabaruddin Sahade Salfauqi Nurman, Salfauqi Samsinar Samsinar Samsinar Sangkala, Masnawaty Saputra, Rifki Setiyadi, Johar Siregar, Barly Harly Sri Utami Sulastri Devi Lestari. S Syahputri, Ardita Syahruddin, Nilam Cahya Thamrin Tahir Tikurede, Meli Tuti Supatminingsih Waliyullah, Akbar Widodo S Pranowo Yoshita, Rika Yusdiana, Yusdiana Yusuf, Dian Madinah