Heat Transport Processes of the Indonesian Throughflow Along the Outflow Pathway in the Eastern Indian Ocean During the Last 160 Kyr

Author:

Ding Xuan12ORCID,Bassinot Franck3ORCID,Pang Xiaolei45,Kou Yingxin6,Zhou Liping47ORCID

Affiliation:

1. School of Ocean Sciences China University of Geosciences (Beijing) Beijing China

2. Key Laboratory of Polar Geology and Marine Mineral Resources (China University of Geosciences, Beijing) Ministry of Education Beijing China

3. LSCE (CEA/CNRS/UVSQ) Domaine du CNRS Gif‐sur‐Yvette France

4. Institute of Ocean Research Peking University Beijing China

5. School of Earth and Space Sciences Peking University Beijing China

6. Research School of Earth Sciences Australian National University Canberra ACT Australia

7. Key Laboratory for Earth Surface Processes Department of Geography Peking University Beijing China

Abstract

AbstractAs the only low‐latitude connection along the return branch of the Great Conveyor Belt, the Indonesian Throughflow (ITF) plays an important role in the large‐scale ocean–atmosphere interaction in the tropical region. However, the heat transport processes of the ITF along the outflow pathway in the eastern Indian Ocean over the recent geologic period is still debated. In this study, by using Mg/Ca ratios of the surface‐dwelling and thermocline‐dwelling planktonic foraminifera Globigerinoides ruber and Pulleniatina obliquiloculata, we reconstruct sea surface temperature and thermocline water temperature (TWT), and thermocline structure at two sites in the main outflow path of the ITF in the eastern Indian Ocean for the last 160 Kyr, and compare these new data with those from two cores in the central Indo‐Pacific Warm Pool. Our results show that, on the orbital time scale, the thermocline structure changes above the equatorial 90°E Ridge mimic those of the eastern Timor Sea, indicating that the ITF vertical structure remained unchanged during its penetration into the Indian Ocean. The TWT in the equatorial western Pacific and eastern Indian Ocean presents similar change trend, suggesting that the ITF is likely to be an important route for thermocline water transport into the Indian Ocean. However, the vertical structure of the ITF varied through time, reflecting the effects of sea level and orbitally‐driven monsoonal activity. This impacted heat transport processes, resulting in changes in the surface water temperature along the outflow pathway in the eastern Indian Ocean.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

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