Possible reverse trend in Asian summer monsoon strength during the late Holocene

被引:27
作者
Zhao, Cheng [1 ]
Chang, Yuan-Pin [2 ]
Chen, Min-Te [3 ]
Liu, Zhonghui [1 ]
机构
[1] Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China
[2] Natl Sun Yat Sen Univ, Inst Marine Geol & Chem, Kaohsiung 80424, Taiwan
[3] Natl Taiwan Ocean Univ, Inst Appl Geosci, Keelung, Taiwan
关键词
Asian summer monsoon; Late Holocene; Temperature changes; Summer insolation; INTERTROPICAL CONVERGENCE ZONE; SURFACE-TEMPERATURE VARIABILITY; GREENLAND ICE-CORE; NORTH-ATLANTIC; HIGH-RESOLUTION; CLIMATE-CHANGE; PACIFIC; OCEAN; PRECIPITATION; RAINFALL;
D O I
10.1016/j.jseaes.2012.09.028
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Holocene climate change is characterized as generally cooling in high latitudes and drying in tropical and Asian summer monsoonal regions, following the gradual decrease in northern hemisphere summer insolation over the last 12,000 years. However, some recent high-resolution, well-dated monsoon reconstructions seem to suggest an abnormal increase in Asian summer monsoon strength during the late Holocene, against the generally weakening Holocene trend. Here, we synthesize marine and terrestrial moisture records from Asian monsoonal regions that span most of the Holocene period. Late Holocene strengthening of Asian summer monsoon identified from a wealth of the synthesized monsoon records appears to be a robust feature, which warrants further consideration of its possible causes. The possible reverse trend in Asian summer monsoon strength preceding insolation minima seems to have also occurred during previous interglacial periods, based on speleothem records. We further show a similar late Holocene reverse trend in tropical hydrological changes, suggesting that the Asian summer monsoon behavior might be internally linked to the movement of the average position of the ITCZ and ENSO variability during the late Holocene. On the other hand, we suggest that even though several Holocene temperature records indeed show a reverse trend in the late Holocene, the overall evidence for a link between the late Holocene reverse trend in Asian summer monsoon and global temperature changes is insufficient. The reverse trend in Asian summer monsoon during the late Holocene is difficult to be explained with the traditional boreal insolation-driven view. We suggest that this phenomenon might be linked to austral summer insolation changes and/or greenhouse gas increase. However, we caution that additional paleoclimate reconstructions and model simulations are needed to systematically study the spatial pattern and understand underlying mechanism of the late Holocene reverse trend in Asian summer monsoon strength. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:102 / 112
页数:11
相关论文
共 66 条
[1]   Glacial-Interglacial Indian Summer Monsoon Dynamics [J].
An Zhisheng ;
Clemens, Steven C. ;
Shen, Ji ;
Qiang, Xiaoke ;
Jin, Zhangdong ;
Sun, Youbin ;
Prell, Warren L. ;
Luo, Jingjia ;
Wang, Sumin ;
Xu, Hai ;
Cai, Yanjun ;
Zhou, Weijian ;
Liu, Xiaodong ;
Liu, Weiguo ;
Shi, Zhengguo ;
Yan, Libin ;
Xiao, Xiayun ;
Chang, Hong ;
Wu, Feng ;
Ai, Li ;
Lu, Fengyan .
SCIENCE, 2011, 333 (6043) :719-723
[2]   Asynchronous Holocene optimum of the East Asian monsoon [J].
An, ZS ;
Porter, SC ;
Kutzbach, JE ;
Wu, XH ;
Wang, SM ;
Liu, XD ;
Li, XQ ;
Zhou, WJ .
QUATERNARY SCIENCE REVIEWS, 2000, 19 (08) :743-762
[3]   High-resolution climatic evolution of coastal northern California during the past 16,000 years [J].
Barron, JA ;
Heusser, L ;
Herbert, T ;
Lyle, M .
PALEOCEANOGRAPHY, 2003, 18 (01)
[4]   INSOLATION VALUES FOR THE CLIMATE OF THE LAST 10000000 YEARS [J].
BERGER, A ;
LOUTRE, MF .
QUATERNARY SCIENCE REVIEWS, 1991, 10 (04) :297-317
[5]   Sensitivity of Red Sea circulation to monsoonal variability during the Holocene: An integrated data and modeling study [J].
Biton, E. ;
Gildor, H. ;
Trommer, G. ;
Siccha, M. ;
Kucera, M. ;
van der Meer, M. T. J. ;
Schouten, S. .
PALEOCEANOGRAPHY, 2010, 25
[6]   Persistent solar influence on north Atlantic climate during the Holocene [J].
Bond, G ;
Kromer, B ;
Beer, J ;
Muscheler, R ;
Evans, MN ;
Showers, W ;
Hoffmann, S ;
Lotti-Bond, R ;
Hajdas, I ;
Bonani, G .
SCIENCE, 2001, 294 (5549) :2130-2136
[7]   ENSO related decadal scale climate variability from the Indo-Pacific Warm Pool [J].
Brijker, J. M. ;
Jung, S. J. A. ;
Ganssen, G. M. ;
Bickert, T. ;
Kroon, D. .
EARTH AND PLANETARY SCIENCE LETTERS, 2007, 253 (1-2) :67-82
[8]   High-resolution absolute-dated Indian Monsoon record between 53 and 36 ka from Xiaobailong Cave, southwestern China [J].
Cai, Yanjun ;
An, Zhisheng ;
Cheng, Hai ;
Edwards, R. Lawrence ;
Kelly, Megan J. ;
Liu, Weiguo ;
Wang, Xianfeng ;
Shen, Chuan-Chou .
GEOLOGY, 2006, 34 (08) :621-624
[9]   The variation of summer monsoon precipitation in central China since the last deglaciation [J].
Cai, Yanjun ;
Tan, Liangcheng ;
Cheng, Hai ;
An, Zhisheng ;
Edwards, R. Lawrence ;
Kelly, Megan J. ;
Kong, Xinggong ;
Wang, Xianfeng .
EARTH AND PLANETARY SCIENCE LETTERS, 2010, 291 (1-4) :21-31
[10]   Amplitude and timing of temperature and salinity variability in the subpolar North Atlantic over the past 10 k.y. [J].
Came, Rosemarie E. ;
Oppo, Delia W. ;
McManus, Jerry F. .
GEOLOGY, 2007, 35 (04) :315-318