文章强烈地在在东方亚洲人和印度洋夏天季风之间的互联考察研究进步,在亚洲季风和 ElNino 南部的摆动(ENSO ) 活动之间,并且在季风, ENSO 并且在 Holocene 期间变化诺思大西洋气候之间。根据最近的年的研究,东方亚洲人和印度洋夏天季风的紧张变化显示出一种相反的关系,这被发现,它可以是仔细与在赤道的和平的 Oceanand 的 ENSO 的现象有关诺思大西洋在上的深海的形成的变化内部对轨道的时间规模年度。分别地,发生在约 4200 和 8200 一 BP 的 4k 和 8k 事件可能在 Holocene 期间在一系列严重 pa-leo-EI Nino 事件是二,强烈反映季风, ENSO 和北方的相互作用和影响大西洋气候。Inorder 将更好在赤道的太平洋和 pateoclimatecondition 的模拟研究与 hightime 决定在海表面温度的代理记录上理解在这些 paleoclimatic 现象,在在季风代理之间的分割和比较记录的亚洲季风上加强研究工作的科学家需要,和学习之间的关系。
The article emphatically reviews the research progress in interconnections between the East Asian and Indian Ocean summer monsoons, between the Asian monsoon and the El NiSo-Southern Oscillation (ENSO) activity, and between the monsoon, ENSO and the changing of the North Atlantic climate during the Holocene. According to the studies of recent years, it is found that the intensity variations of the East Asian and Indian Ocean summer monsoons show an opposite relationship, which may be closely related to the phenomena of ENSO in the equatorial Pacific Ocean and the variation of the deep-water formation of the North Atlantic Ocean on the interannual to orbital time scales. The 4k and 8k events occurring at around 4200 and 8200 a BP, respectively, might be the two in a series of severe paleo-El NiSo events during the Holocene, strongly reflecting the interactions and influences of the monsoons, ENSO and the North Atlantic climate. In order to better understand the relationships between these paleoclimatic phenomena, scientists need to strengthen the research work on the Asian monsoon division and the comparison between monsoon proxy records, and the study on the proxy record of sea surface temperature with high time-resolution in the equatorial Pacific Ocean and the simulation research of paleoclimate condition.