Wet and cold climate conditions recorded by coral geochemical proxies during the beginning of the first millennium CE in the northern South China Sea

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• 作者：Hangfang Xiao^a ; ^b ; Wenfeng Deng^a ; ^{wfdeng@gig.ac.cn} ; ^{wfdeng@gmail.com} ; Xuefei Chen^a ; ^b ; Gangjian Wei^a ; Ti Zeng^c ; Jian-xin Zhao^d
• 关键词：Eastern Han ; Three Kingdoms ; Western Jin ; Sea surface temperature ; Sea surface salinity ; South China Sea
• 刊名：Journal of Asian Earth Sciences
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：135
• 期：Complete
• 页码：25-34
• 全文大小：901 K
• 卷排序：135

文摘

The climate was cold and wet during 167–309 CE in the northern South China Sea. The cold SSTs were caused by the weak solar irradiance. The wet conditions were caused by the reduced northward shift of ITCZ/monsoon rainbelt. The interannual and interdecadal variability may be associated with ENSO and PDO.