LIU Bingjin，HUANG Enqing，TIAN Jun. Precession forcing of the Holocene moisture transfer between tropical western Pacific and Indian Ocean[J]. Marine Geology & Quaternary Geology，2023，43(4)：56-70. DOI: 10.16562/j.cnki.0256-1492.2023042001
Citation: LIU Bingjin，HUANG Enqing，TIAN Jun. Precession forcing of the Holocene moisture transfer between tropical western Pacific and Indian Ocean[J]. Marine Geology & Quaternary Geology，2023，43(4)：56-70. DOI: 10.16562/j.cnki.0256-1492.2023042001
shu

Precession forcing of the Holocene moisture transfer between tropical western Pacific and Indian Ocean

  • State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China

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  • Received Date: April 19, 2023
  • Revised Date: May 25, 2023
  • Accepted Date: May 25, 2023
  • Available Online: June 13, 2023
    Graphical Abstract
    • Abstract
  • Precipitation, evaporation and moisture transport within the oceans are the main components of the global hydrological cycle. However, the evolution of the oceanic hydrological cycle over the Holocene remains a knowledge gap. In this study, through compiling paired planktonic foraminiferal δ18O and Mg/Ca sea surface temperature reconstructions from 98 locations in the tropical ocean, we calculate the fluctuation of sea surface δ18O and residual δ18O for the Holocene period. We notice a striking feature that the residual δ18O records of the tropical western Pacific and eastern Indian Ocean show a different change over the Holocene. The mean residual δ18O of the tropical western Pacific was about 0.2‰ heavier than that of the eastern Indian Ocean during the early-mid Holocene (11.5～6.0 kaBP), but they were almost identical over the late Holocene (2.0～0 kaBP). Combined with the transient climate simulations, we suggest that precession forcing is responsible for this different pattern through modulating a set of climate processes. The lower precession over the early Holocene drove a net atmospheric moisture transport from the western Pacific to the eastern Indian Ocean and lowered precipitation δ18O over the eastern Indian Ocean. Moreover, the strengthened South Asian monsoon delivered large amounts of diluted freshwater into the Bay of Bengal via river systems. All these three mechanisms contribute to a relatively negative excursion of residual δ18O in the eastern Indian Ocean. In contrast, the lower precession resulted in a decrease of net precipitation in the open western Pacific and a loss of freshwater via the atmospheric transport, thus generating heavier residual δ18O values. Through combining seawater δ18O reconstructions from a large spatial extent with the isotope-enabled simulations, this study has provided a reliable picture of the moisture transfer between different ocean basins and unveiled the underlying mechanisms regulated by precession.
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    • References (127)
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