Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1007/s11434-013-5987-8 |
Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution | |
Liu XiaoDong1,2; Dong BuWen3 | |
通讯作者 | Liu XiaoDong |
来源期刊 | CHINESE SCIENCE BULLETIN |
ISSN | 1001-6538 |
EISSN | 1861-9541 |
出版年 | 2013 |
卷号 | 58期号:34页码:4277-4291 |
英文摘要 | As one of the most important geological events in Cenozoic era, the uplift of the Tibetan Plateau (TP) has had profound influences on the Asian and global climate and environment evolution. During the past four decades, many scholars from China and abroad have studied climatic and environmental effects of the TP uplift by using a variety of geological records and paleoclimate numerical simulations. The existing research results enrich our understanding of the mechanisms of Asian monsoon changes and interior aridification, but so far there are still a lot of issues that need to be thought deeply and investigated further. This paper attempts to review the research on the influence of the TP uplift on the Asian monsoon-arid environment, summarize three types of numerical simulations including bulk-plateau uplift, phased uplift and sub-regional uplift, and especially to analyze regional differences in responses of climate and environment to different forms of tectonic uplifts. From previous modeling results, the land-sea distribution and the Himalayan uplift may have a large effect in the establishment and development of the South Asian monsoon. However, the formation and evolution of the monsoon in northern East Asia, the intensified dryness north of the TP and enhanced Asian dust cycle may be more closely related to the uplift of the main body, especially the northern part of the TP. In this review, we also discuss relative roles of the TP uplift and other impact factors, origins of the South Asian monsoon and East Asian monsoon, feedback effects and nonlinear responses of climatic and environmental changes to the plateau uplift. Finally, we make comparisons between numerical simulations and geological records, discuss their uncertainties, and highlight some problems worthy of further studying. |
英文关键词 | Tibetan Plateau tectonic uplift Asian monsoon inland aridity environmental evolution geological record numerical simulation |
类型 | Review |
语种 | 英语 |
国家 | Peoples R China ; England |
收录类别 | SCI-E |
WOS记录号 | WOS:000326942700014 |
WOS关键词 | INDIAN-SUMMER MONSOON ; TECTONIC UPLIFT ; CHINESE LOESS ; MYR AGO ; EOLIAN DEPOSITION ; EURASIAN CLIMATE ; MOUNTAIN UPLIFT ; PLIOCENE UPLIFT ; DESERT DUST ; MIOCENE |
WOS类目 | Multidisciplinary Sciences |
WOS研究方向 | Science & Technology - Other Topics |
来源机构 | 中国科学院地球环境研究所 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/176418 |
作者单位 | 1.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China; 2.Xi An Jiao Tong Univ, Sch Human Settlements & Civil Engn, Xian 710049, Peoples R China; 3.Univ Reading, Natl Ctr Atmospher Sci, Reading RG6 6BB, Berks, England |
推荐引用方式 GB/T 7714 | Liu XiaoDong,Dong BuWen. Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution[J]. 中国科学院地球环境研究所,2013,58(34):4277-4291. |
APA | Liu XiaoDong,&Dong BuWen.(2013).Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution.CHINESE SCIENCE BULLETIN,58(34),4277-4291. |
MLA | Liu XiaoDong,et al."Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution".CHINESE SCIENCE BULLETIN 58.34(2013):4277-4291. |
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