East Asian Winter Monsoon Variations and Their Links to Arctic Sea Ice During the Last Millennium, Inferred From Sea Surface Temperatures in the Okinawa Trough

@article{Li2018EastAW,
  title={East Asian Winter Monsoon Variations and Their Links to Arctic Sea Ice During the Last Millennium, Inferred From Sea Surface Temperatures in the Okinawa Trough},
  author={Dongling Li and Tiegang Li and Hui Jiang and Svante Bj{\"o}rck and Marit‐Solveig Seidenkrantz and Meixun Zhao and Longbin Sha and K. L. Knudsen},
  journal={Paleoceanography and Paleoclimatology},
  year={2018},
  volume={33},
  pages={61 - 75}
}
The East Asian winter monsoon (EAWM) significantly impacts living conditions in a large part of Asia, and therefore, it is important to understand its major driving mechanisms. Winter sea surface temperature (SSTW) and circulation in the southern Okinawa Trough are today both primarily controlled by the EAWM. Here we present a new SSTW reconstruction for the last millennium based on a diatom record from sediment core MD05‐2908, from the continental slope of the southern Okinawa Trough off… 

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TLDR
The results of the total organic carbon (TOC) and stable organic carbon isotope (δ13C) in sediment samples from core XH-2 in the Xianghu area in Zhejiang Province have revealed the evolution of sedimentary environmental and climatic changes during the breeding–prosperity–decline period of the Kuahuqiao culture.

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