IIOSC - 2025

IIOSC - 2025

International Indian Ocean Science Conference - 2025

Celebrating 10 years of the Second International Indian Ocean Expedition

01-05 December 2025
INCOIS, Hyderabad, India.

Summary of Abstract Submission



Abstract Submission No.ABS-02-0151
Title of AbstractAustral Autumn Surface CO2 in the Western Indian Ocean and Relationship with the Indian Ocean Dipole (IOD)
AuthorsSo-Yun Kim*, Sang-Hwa Choi, Dong-Jin Kang, Hyoun-Woo Kang
OrganisationKorea Institute of Ocean Science & Technology (KIOST)
Address385 Haeyang-ro
Yeongdo-gu, Busan, Korea, Rep.
Pincode: 49111
E-mail: soyun3369@kiost.ac.kr
CountryKorea, Rep.
PresentationPoster
AbstractThe Indian Ocean plays a crucial role in global carbon cycling, yet the seasonal and climate-driven variability in air-sea CO2 exchange remains poorly understood. We investigated surface fugacity of CO2 (fCO2sea) and associated CO2 air-sea fluxes in the western Indian Ocean during austral autumn (April-June) in 2019, 2023, 2024, and 2025. The western Indian Ocean generally acted as a CO2 sink, except in the northern region (<10° S; Seychelles-Chagos Thermocline Ridge, SCTR) during negative Indian Ocean Dipole (nIOD) years, with fluxes ranging from 0.2 to 0.7 mol m-2 yr-1. Thermal effects on fCO2sea were strongest in 2025 (the warmest year), while non-thermal effects dominated in the SCTR region. During nIOD years (2023, 2025), enhanced subsurface upwelling in the SCTR region increased surface CO2 concentrations, producing positive non-thermal effect anomalies, higher fCO2sea, and weaker CO2 uptake. In contrast, during positive IOD years (2019, 2024), suppressed upwelling generated negative non-thermal anomalies, lower fCO2sea, and stronger CO2 uptake. These results highlight the relationship between IOD phases and CO2 dynamics in the SCTR region.
Are you part of IIOE-2 endorsed projectyes
Endorsed Project NumberIIOE2-EP51
Keywordssurface fCO2, CO2 flux, western Indian Ocean, SCTR, IOD
For Awardsno