2.6 Ma BP 前后亚洲季风系统的重组

doi:10.7605/gdlxb.2000.02.008

Abstract
Figure/Table
References()
Related Citation (15)
Read Tracking
Download Tracking

Download: PDF (0 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS) Supporting Info

Abstract

In this paper, the changes of the Asian monsoon system at about 2.6 Ma ago are discussed based on atmospheric simulations and analysis of the geological records. The results show that the Asian monsoon system reorganized at about 2.6 Ma ago. At that time, both winter and summer monsoons being strengthened obviously and the direction of the winter monsoon in North China changed from NorthWestWest to NorthWestNorth. In China, the area influenced by the East Asian monsoon increased, but the area influenced by Indian monsoon decreased. This is attributed to the uplifting of the Qinghai—Xizang Plateau and the southwestward migration of the center of the Asian Low. At some time of the Pliocene, the Tropical Southwest Monsoon had spreaded onto the Qinghai—Xizang region and has influenced areas over the North China and Northwest China. However, after 2.6 Ma BP, the effects of the Tropical Southwest Monsoon on Northwest China and the Northern part of the Qinghai—Xizang Plateau has decreased again. All these suggest that the Qinghai—Xizang Plateau perhaps reached about 2000 meter elevation above sea level at about 2.6 Ma BP.

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors

Published: 01 April 2000

About author: Wang Jian, born in 1962, has received his Ph.D. degree in Nanjing University in 1989. Now he is a professor in Nanjing Normal University and is engaged in geomorphology and Quaternary environment.

Cite this article:

. REORGANIZATION OF THE ASIAN MONSOONSYSTEM AT ABOUT 2.6 Ma AGO[J]. JOURNAL OF PALAEOGEOGRAPHY, 2000, 2(2): 73-83.

. REORGANIZATION OF THE ASIAN MONSOONSYSTEM AT ABOUT 2.6 Ma AGO[J]. JOPC, 2000, 2(2): 73-83.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2000.02.008 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2000/V2/I2/73

1Ding Zhongli, Nat Rutter, Han Jingtai and Liu Tungsheng. A coupled environmental system formed at about 2.5 Ma in East Asia. Palaeogeography, Palaeoclimatology, Palaeoecology, 1992，94：223～242
2汤懋苍，刘晓东. 一个新的划分第四纪的标志—高原季风演变的地质环境后果. 第四纪研究，1995，（1）：82～
3刘东生等. 中国第四纪环境概要. 见：Williams M A J等箸. 刘东生等编译. 第四纪环境. 北京：科学出版社，1997. 221～231
4吴锡浩等. 关于晚新生代准1.2 Ma周期构造气候旋回. 地质力学学报，1998，4（4）：1～11
5安芷生，王苏民，吴锡浩等. 中国黄土高原的风积证据：晚新生代北半球大冰期开始及青藏高原的隆升驱动. 中国科学（D缉），1998，28（6）：481～490
6丁仲礼，杨石岭，孙继敏，刘东生. 2.6 Ma前后大气环流重构的黄土-红粘土沉积证据. 第四纪研究，1999，3：277～281
7李吉均. 青藏高原的地貌演化与亚洲季风. 海洋地质与第四纪地质，1999，19（2）：1～11
8梁必颢. 热带气象学. 广州：中山大学出版社，1990. 50～72
9Hahn D G and Manabe S. The role of mountains in the South Asian Monsoon circulation. Journal of Atmospheric Sciences, 1975, 32：1515～1535
10Trenberth K E and ShyhChin Chen. Planetary waves kinematically forced by Himalayan orography. Journal of Atmospheric Sciences, 1988, 45(20)：2934～2948
11赵景波. 西安、山西保德第三纪晚期红土的研究. 1989，7（3）：113～119
12孙东怀，刘东生，陈明扬等. 中国黄土高原红粘土序列的磁性地层年代与古气候变化. 中国科学(D缉)，1997，23（3）：265～270
13丁仲礼，孙继敏，朱日祥，郭斌. 黄土高原红粘土成因及上新世干旱化问题. 第四纪研究，1997，2：147～175
14陈明扬. 中国风尘堆积与全球干旱化. 第四纪研究，1991，（4）：361～371
15刘东生等. 中国的黄土堆积. 北京：科学出版社，1966. 198～201
16董光荣，李保生，高尚玉，吴正，邵亚军. 鄂尔多斯高原第四纪古风成沙的发现及其意义. 科学通报，1983，16：998～1001
17Li Jijun．The environmental effects of the uplift of the Qinghai-Xizang Plateau．Quaternary Science Review, 1991, 10：479～483
18李华章，刘清泗. 北京平原第四纪环境演变初议. 见：第四纪冰川与第四纪地质论文集. 北京：地质出版社，1988. 41～51
19吴锡浩，钱方，兰朝玉. 北京延庆盆地早更新世古气候重建. 见：刘东生主编. 黄土. 第四纪地质. 全球变化（第一集）. 北京：科学出版社， 1990. 47～61
20An Z S, Liu T S, Lu Y C et al. The long term paleomonsoon variation recorded by the loesspaleosol sequence in Central China．Quaternary International,
1990, 7/8：91～95
21Dersch M And Stein R. Late Cenozoic records of eolian quartz flux in the Sea of Japan (ODPleg128, Sites 798 and 799) and paleoclimate in Asia. Palaeaogeography, Palaeaoclimatology, Palaeaoecology, 1994, 108:523～535
22唐领余，沈才明. 青藏高原的植被演变. 见：施雅凤、李吉均、李炳元主编. 青藏高原晚新生代隆升与环境变化. 广州：广东科技出版社，1998. 314～331
23Janecek T R. Eolian sedimentation in the Northwest Pacific Ocean: Apreluiminary examination of the data from deep sea drilling project sites 576 and 578. In: Initial Reports of the Deep Sea Drilling Project. Washington D. C.: US Government Printing Office, 1985, 86:589～603
24李炳元. 青藏高原的湖泊演化. 见：施雅凤、李吉均、李炳元主编. 青藏高原晚新生代隆升与环境变化. 广州：广东科技出版社，1998. 331～347
25王跃，董光荣，陈惠忠等. 中国西北地区晚第三纪末古风向重大变化的两例证据. 见：刘东生，安芷生，吴锡浩主编. 黄土. 第四纪地质. 全球变化，第四集. 北京：科学出版社，1996. 18～21
26陈隆勋，刘骥平，周秀骥，汪品先. 青藏高原隆起及海陆分布变化对亚洲大陆气候的影响. 第四纪研究，1999（4）：314～32927Ruddiman W F And Kutzbach J E. Forcing of Late Cenozoic Northern Hemisphere climate by Plateau Uplift in Sourthern Asia and the American West. Journal of Geophysical Research,1989, 94(D15)：18409～18427
28Coleman M and Hodges K. Euidence for Tibetan Plateau uplift before 14 Myr ago from a new minimum age for eastwest extension. Nature, 1995, 374：49～52
29Harrison T M, Copelan D, Kidd W S F and Yin A. Rising Tibet. Science, 1992，255：1663～1670
30Molnar P, England P And Martinod J. Mantle Dynamics,uplift of the Tibetan Plateau and the Indian Monsoon. Reviews of Geophysics,1993, 31(4):357～396
31刘晓东、汤懋苍. 青藏高原影响气候的临界高度. 见：青藏项目专家委员会编. 青藏高原形成演化、环境变迁、生态系统的研究. 北京：科学出版社，1996. 188～195