Study Explains Dynamics of Interannual Eddy Kinetic Energy Variability in Sulawesi Sea
Mesoscale eddies are essential for the distribution of thermohaline and biochemical properties, and act as a bridge for the energy cascade between large-scale circulation and submesoscale dynamical processes. The Sulawesi Sea is the primary entrance for the western path of the Indonesian Throughflow and the most active region of mesoscale eddies in the Indonesian seas. However, the interannual evolution of eddy kinetic energy (EKE) in the Sulawesi Sea (an indicator of eddy activity intensity) is still unclear.
Recently, the research team led by Prof. YIN Baoshu from the Institute of Oceanology of the Chinese Academy of Sciences (IOCAS) and Prof. FENG Ming from CSIRO Oceans & Atmosphere have made new progress in the study of the dynamics of interannual EKE variability in the Sulawesi Sea.
This study was published in Journal Geophysical Research: Oceans.
Based on the outputs of Ocean Forecasting Australia Model version 3, it is found that the prominent interannual EKE variability in the Sulawesi Sea is modulated by the Mindanao Current (MC) intrusion. The barotropic instability of cyclonic loop current in the Sulawesi Sea, regulating by the fluctuation of upstream MC intrusion transport (MCIT), is responsible for the interannual EKE variations.
The paths of two western boundary currents, namely MC and New Guinea Coastal Current and Undercurrent (NGCC/NGCUC), are the primary driving forces to modulate the MC intrusion. During high-EKE periods, the MCIT increases 0.60 Sv (1 Sv≡106 m3s-1) when the NGCC/NGCUC weakens and the MC retroflection extends to south of 5°N, which strengthens the barotropic energy conversion from mean kinetic energy to EKE in the Sulawesi Sea. During low-EKE periods, the fact that the NGCC/NGCUC is intensified and the MC retroflection retreats to a northernmost path, leading to a decrease of 0.58 Sv in MCIT and thus a low EKE level in the Sulawesi Sea.
"In addition, cyclonic and anticyclonic mesoscale eddies to east of the Sulawesi Sea in the western Pacific can facilitate and suppress the MC intrusion, respectively," said HAO Zhanjiu, first author of the study.
"Our study highlights the significance of the nonlinear dynamics of western boundary currents in modulating eddy activities in the formation region of the Indonesian Throughflow," said Prof. XU Zhenhua, one of the corresponding authors.
This work was supported by the Strategic Priority Research Program of Chinese Academy of Sciences and the National Natural Science Foundation of China, etc.
Schematic of the dynamics responsible for the interannual EKE variability in the Sulawesi Sea.
Hao, Z., Xu, Z.*, Feng, M.*, Zhang, P., & Yin, B. (2022). Dynamics of interannual eddy kinetic energy variability in the Sulawesi Sea revealed by OFAM3. Journal of Geophysical Research: Oceans, 127, e2022JC018815.
(Text by HAO Zhanjiu)
Media Contact:
ZHANG Yiyi
Institute of Oceanology
E-mail: zhangyiyi@qdio.ac.cn
(Editor: ZHANG Yiyi)
