过去5000年西太平洋副热带高压活动的泥炭纤维素碳同位素记录
Subtropical high activity of western pacific ocean during the last 5 000 years recorded in isotope time series of peat bog
查看参考文献19篇
|
文摘
|
文章以金川和红原两组泥炭纤维素Δδ~(13)C时间序列值的反向变化来指示西太平洋副热带高压活动变化。结果表明，在过去5 000年中，西太平洋副热带高压的活动可分为4个阶段，即西太平洋副热带高压位置在2800-2200 B.C. 期间持续偏北，2200-600 B.C.期间持续偏南，600 B.C.-1200 A.D.期间在北进与南移之间频繁波动，以及1200-1900A.D.期间再次持续偏北，它们导致降雨量在中国大陆上不同的分布。从约1900A.D.起西太平洋副热带高压的活动似乎又开始一个新的偏南阶段，值得进一步加强研究。 |
|
其他语种文摘
|
An inverse correlation between the isotope time series of peat cellulose from Jinchuan and Hongyuan has been used for indicating the subtropical high activities of the Western Pacific Ocean. Tlae results show that the subtropical high aclivities can be divided inlo four stages during the last 5 000 years. In the period from 2800 B.C. to 2200 B.C. the ridge line of subtropical high seems to tend to move to the north part of the China continent, which led to an increase precipitation in the region covering the northeastern China, the north China and the Yellow river basin; and at the same time caused a decrease precipitation in the region between the Changjiang and Huai rivers. On the contraiy, during the period from 2200 B.C. to 600 B.C. the ridge line was in the south of China, which led to a decrease precipitation in Yellow river basin and so on, and at the same time caused an increase precipitation in the region between the Changjiang and Huai rivers. After walking back and forth between the north and south for around 1 800 years the subtropical high seems to move to the north again during the period from 1200 A. D. to 1900 A. D. What is worth to paying particular attention to is that from around 1900 A. D. the subtropical high seems to begin to move again to the south part of China continent, for which it remains to be studied further. |
|
来源
|
第四纪研究
,2003,23(5):485-492 【核心库】
|
|
关键词
|
西太平洋副热带高压
;
季风降雨
;
泥炭纤维素碳同位素
;
全新世
|
|
地址
|
中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵阳, 550002
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
1001-7410 |
|
学科
|
地质学 |
|
基金
|
国家自然科学基金
|
|
文献收藏号
|
CSCD:1172949
|
参考文献 共
19
共1页
|
|
1.
陶诗言. 中国夏季副热带天气系统若干问题的研究.
中国夏季副热带天气系统若干问题的研究,1963:106-146
|
被引
11
次
|
|
|
|
|
2.
刘屹岷. 副热带高压研究回顾及对几个基本问题的再认识.
气象学报,2000,58(4):500-512
|
被引
57
次
|
|
|
|
|
3.
仇永炎. 副热带高压.
中国大百科全书*大气科学,1983:188-189
|
被引
1
次
|
|
|
|
|
4.
黄荣辉. 热带西太平洋暖池的热状态及其上空的对流活动对东亚夏季气候异常的影响.
大气科学,1994,18(2):141-151
|
被引
266
次
|
|
|
|
|
5.
章名立. 西太平洋云量变化与中国东部的降水.
大气科学,1993,17(5):576-583
|
被引
11
次
|
|
|
|
|
6.
Yapp C J. Climatic implications of D/H ratios of meteoric water over North America (9.
Earth and Planetary Science Letters,1977,34:333-350
|
被引
5
次
|
|
|
|
|
7.
Hong Y T. A 6000-year record of changes in drought and precipitation in northeastern China based on a δ13C time series from peat cellulose.
Earth and Planetary Science Letters,2001,185:111-119
|
被引
70
次
|
|
|
|
|
8.
Hong Y T. A 6000-year record of changes in drought and precipitation in northeastern China based on a δ13C time series from peat cellulose.
Earth and Planetary Science Letters,2001,185:111-119
|
被引
70
次
|
|
|
|
|
9.
Denton G H. Their pattern and possible cause.
Quaternary Research,1973,3:155-205
|
被引
64
次
|
|
|
|
|
10.
O'Brien S R. Complexity of Holocene climate as reconstructed from a Greenland Ice core.
Science,1995,270:1962-1964
|
被引
90
次
|
|
|
|
|
11.
Bond G. Persistent solar influence on North Atlantic climate during the Holocene.
Science,2001,294:2130-2136
|
被引
240
次
|
|
|
|
|
12.
Hong Y T. Response of climate to solar forcing recorded in a 6000-year δ18O time series of Chinese peat cellulose.
The Holocene,2000,10:1-7
|
被引
62
次
|
|
|
|
|
13.
洪业汤. 近5ka温度的金川泥炭δ↑（18）O记录.
中国科学(D辑),1997,27(6):525-530
|
被引
68
次
|
|
|
|
|
14.
靳桂云. 华北北部中全新世降温气候事件与古文化变迁.
科学通报,2001,46(20):1725-1730
|
被引
59
次
|
|
|
|
|
15.
徐海. 红原泥炭纤维素氧同位素指示的距今6 ka温度变化.
科学通报,2002,47(15):1181-1186
|
被引
69
次
|
|
|
|
|
16.
侯甬坚. 历史记录提取的近5—2．7ka黄河中下游平原重要气候事件及其环境意义.
海洋地质与第四纪地质,2000,20(4):23-29
|
被引
25
次
|
|
|
|
|
17.
洪业汤. 气候变化与文明发展.
中国第四纪地质与环境,1997:359-367
|
被引
4
次
|
|
|
|
|
18.
夏商周断代工程专家组. 夏商周断代工程1996-2000年阶段成果报告(简本).
夏商周断代工程1996～2000年阶段成果报告(简本),2000:1-118
|
被引
1
次
|
|
|
|
|
19.
张德二. 近1千年我国东部6个区域干湿气候跃变分析.
全球变化与我国未来的生存环境,1996:37-44
|
被引
1
次
|
|
|
|
|
了解气象卫星更多信息，请访问