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100			_aLee, Wing-Man _951792
245			_aSummer monsoon–induced upwelling dominated coastal sea surface temperature variations in the northern South China Sea over the last two millennia/
260			_bSage, _c2019.
300			_aVol 29, issue 4, 2019 : (691-698 p.).
520			_aThe South China Sea (SCS), situated to the north of the Indo-Pacific Warm Pool (IPWP), is under the strong influence of the Asian monsoon system. However, coastal sea surface temperature (SST) records from the SCS, which are of vital importance to exploring ocean-atmosphere-land interactions behind the Asian monsoon system, remain scarce. Here, we use a sediment core collected at the coast of northern SCS to investigate alkenone-SST variations over the past two millennia. On multi-centennial timescale, SST changes in our record exhibit an opposite pattern to that of Northern Hemisphere temperature and solar irradiance, for example, relatively cool SST during the Medieval Warm Period (MWP) and warm conditions during the Little Ice Age (LIA). Together with alkenone content and existing records, we suggest that the regional SST changes result from a strengthening (weakening) of wind-driven coastal upwelling, associated with variability of the Asian summer monsoon intensity during the MWP (LIA).
650			_aalkenone, _951793
650			_a Asian summer monsoon, _951794
650			_acoastal upwelling, _951795
650			_a late-Holocene, _951310
650			_aSouth China Sea, _951796
650			_aU37K′-SST _951797
700			_aPoon, Kit-Chi _951798
700			_aKong, Deming _951799
700			_aSewell, Roderick J _951800
700			_aZong, Yongqiang _951801
700			_aZhang, Yancheng _951802
700			_aLiu, Zhonghui _951803
773	0		_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836
856			_uhttps://doi.org/10.1177/0959683618824715
942			_2ddc _cART
999			_c12819 _d12819