Seasonal Water Mass Transformation in the Eastern Indian Ocean from In Situ Observations

• Published in: Atmosphere Vol. 15; no. 1; p. 1
• Main Authors: Purba, Noir P., Akhir, Mohd Fadzil, Pranowo, Widodo S., Subiyanto, Zainol, Zuraini
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-01-2024
• Subjects: Analysis; Atmospheric circulation; Atmospheric dynamics; Coastal zone; Datasets; Deep layer; Deep water; eastern boundary currents; Fresh water; Freshwater; Genetic transformation; Indonesian Throughflow; Indonesian throughflow water; Inland water environment; Mixed layer; Monsoons; Ocean currents; Oceans; ocean–atmosphere interactions; Physical properties; Rivers; Salinity; Salinity effects; Sea level; Southwest monsoon; Surface water; thermocline layers; Velocity; Vertical profiles; Water circulation; Water column; Water currents; Water depth; Water mass transformation; Water masses; Wind; Indian Ocean; Australia; United Kingdom; Banda Sea; South Pacific; Timor Sea; Western Australia Australia; Indonesia
• ISSN: 2073-4433; 2073-4433
• DOI: 10.3390/atmos15010001

The Eastern Indian Ocean (EIO) is one of the eastern boundary areas, which control currents circulation and atmospheric dynamics. This research mainly aimed to identify and analyze the water mass transformation in the EIO. The investigated physical properties of the ocean are the temperature, salinity, seasonal temperature–salinity, and water column stability. An extensive amount of in situ data measurements from 1950 to 2018 was downloaded from the global datasets inventory. The visualization and analysis of the data were defined in monthly spatial and vertical profiles. The result showed the mixed layer is shallower during the northwest monsoon relative to the southwest monsoon. The surface water in the EIO is documented to be warmer due to the interaction with the atmosphere. Furthermore, low-salinity surface water around the Java Seas area is caused by a mixing with fresh water from the eastern Indonesia rivers. The data also confirmed that, at latitude 16° S, the maximum salinity occurred at a depth between 150 and 350 m. There are ten types of water masses found in the EIO, which originate from several regions, including the Indonesia Seas, Pacific Ocean, Indian Ocean, and Antarctic. During the northwest and southeast monsoons, a stable layer is found at a depth of 40 to 150 m and 80 to 150 m, respectively. For further research, it is recommended to focus on the coastal region, particularly the Timor Sea and Northwestern Australia, to investigate the dynamics between the Indonesian Throughflow, Holloway Currents, and Leeuwin Currents. Additionally, deep water observations below 800 m are crucial for a comprehensive understanding of the oceanographic variability in the deep layers of the EIO.