Indian Ocean sea surface temperature stack

• Main Authors: Nuber, Sophie, Rae, James W B, Zhang, Xu, Andersen, Morten L, Dumont, Matthew, Mithan, T Huw, Sun, Yuchen, de Boer, Bas, Hall, Ian R, Barker, Stephen
• Format: Dataset
• Language: English
• Published: PANGAEA
• Subjects: 361-U1476; Abashiri; ABS; AGE; Calculated; CALYPSO; Calypso Corer; CD129; Charles Darwin; COMPCORE; Composite Core; Exp361; GeoB10038-4; Giant piston corer; GPC; Gravity corer (Kiel type); GS900963; IMAGES VII - WEPAMA; Indian Ocean; Japan; Joides Resolution; KAL; Kasten corer; Marion Dufresne (1972); Marion Dufresne (1995); MD012378; MD01-2378; MD104; MD122; MD65; MD90-963; MD96-2048; Monitoring station; MONS; oxygen isotope ratios; oxygen isotopes; PABESIA; PC; PEGASE; Percentile 95; Piston corer; planktic foraminifera; Reconstructed; Salinity; Temperature; sea surface salinity; Sea surface temperature; standard score; SEYMAMA/SHIVA; Indian; Planktonic foraminifera
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.955710

Indian Ocean surface circulation is an important part of the global ocean conveyor belt, and is connected via two important gateways including the Indonesian Throughflow, and the Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning circulation. Here we present a planktonic foraminifera-based stack of sea surface temperatures from the surface Indian Ocean. We find that Indian Ocean surface temperature (along with salinity) increases during glacial intensification. We link this phenomenon to dynamics in the Indonesian Archipelago.