Simulated ocean circulation and its variability in the Northern Banda Sea from CROCO model

¹ Graduate Magister program in Marine Sciences, Faculty of Fisheries and Marine Sciences, IPB University, 16680, Bogor, Indonesia
² Marine Science and Technology Department, Faculty of Fisheries and Marine Sciences, IPB University, 16680, Bogor, Indonesia
³ Marine Science Program, Faculty of Mathematics and Natural Sciences, Tanjungpura University, 78124, Pontianak, West Kalimantan, Indonesia
⁴ Research Center for Oceanography, National Research and Innovation Agency, 10340, Central Jakarta, DKI Jakarta, Indonesia
⁵ Marine Science Department, Faculty of Fisheries and Marine Science, Pattimura University, 97233, Ambon, Maluku, Indonesia

^* Corresponding author: amanda.dompeipen@gmail.com

Abstract

A simulation of 1/24º resolution 3-dimension regional ocean circulation of CROCO was successfully performed from 2015 to 2022 (8 years), covering the ENSO year in El Niño 2015 and La Niña 2022 in the northern Banda Sea (NBS). The model and data comparison of sea surface temperature/height reproduced the observed satellite datasets well, with correlation coefficients above 0.9. It is shown that the mean circulation in the NBS is fed by two inflows from western Buru and the Manipa Strait, resulting in a meandering eastward mean circulation with warmer water accumulated in the eastern NBS, associated with high current variance south of Buru and along the Manipa Strait. Seasonal variations in the oceanographic parameters were dominant in the study area. For example, during the southeast (northwest) monsoon period, the seawater temperature is minimum (maximum) and the salinity is maximum (minimum). Furthermore, the interannual timescale ENSO and IOD significantly modulated seawater temperature and salinity variation, particularly at the thermocline layer (110 m). Much cooler and saltier water is associated with El Niño 2015 and a positive IOD, in contrast to warmer and fresher water during La Niña 2022 and a negative IOD.