末次盛冰期以来中国湖泊记录对环流系统及气候类型的响应
The response of lake records to the circulation system and climate zones in China since the Last Glacial Maximum
查看参考文献85篇
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文摘
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为了探讨中国长时间尺度湖泊时空演变规律和潜在的驱动机制,本文在柯本气候分区和中国季风—非季风区的划分基础上,对中国34个有明确数据的典型湖泊运行CCSM 3.0气候模拟系统和水量能量平衡模型模拟其水位变化,同时利用NCEP/NCAR再分析资料对中国按水汽输送划分的季风区进行验证。结果表明,末次盛冰期以来中国湖泊演化主要受千年尺度大气环流的驱动影响,在各个柯本气候区内没有明显的规律性。末次盛冰期以来,在季风区中国湖泊演化主要有早中全新世湖泊水位相对较高以及末次盛冰期和早全新世湖泊水位均较高2种演变规律;在东亚干旱区主要有中晚全新世期间湖泊水位相对较高以及末次盛冰期和中全新世湖泊水位均较高2种演变规律。本文为中国过去气候变化及湖泊演化机制研究提供新的证据,同时为人类全面认识末次盛冰期以来湖泊水位变化提供了新的视角。 |
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其他语种文摘
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In order to investigate the spatial- temporal evolution pattern and potential driving mechanism of lakes on a long time- scale, based on the Koppen climate classification, we classify Chinese climate as 4 climate zones, 6 climatic types and select 34 lakes which have reliable dating, and its lake records have certain continuity since the Last Glacial Maximum. At the same time, NCEP/NCAR 0.5°×0.5° 1900-2015 grid data are used to verify our traditional monsoon region which is defined based on water vapor transportation field. Meanwhile, this study uses a series of models, i.e., the NCAR CCSM 3, a lake energy-balance and a lake waterbalance model, to examine the lake-level evolution process and potential driving mechanism in monsoonal Asia and arid central Asia since the Last Glacial Maximum. Our results indicate that the evolution of lakes in China is mainly affected by millennial-scale atmospheric circulation, and lake-level changes in all climate zones have no obvious regularity. In the monsoon region, there are two kinds of evolvement rules, a relatively high lake- level in the early and mid- Holocene and a relatively high lake- level in the Last Glacial Maximum and early Holocene. Meanwhile, in the arid region of East Asia controlled by westerlies, there are also two kinds of evolvement rules. One is that the lake- level in mid- and late Holocene is relatively high, and the other is that the lake- level is relatively high in mid- Holocene and the Last Glacial Maximum. This study provides a large amount of new evidence, which reflects the past climate change and mechanism of lake evolvement, as well as a new perspective to comprehensively understand lake-level changes since the Last Glacial Maximum. |
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来源
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地理学报
,2016,71(11):1898-1910 【核心库】
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DOI
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10.11821/dlxb201611003
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关键词
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湖泊
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末次盛冰期
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全新世
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环流系统
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气候区
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地址
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兰州大学资源环境学院兰州大学干旱区水循环与水资源研究中心, 西部教育部重点实验室, 兰州, 730000
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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0375-5444 |
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学科
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地质学 |
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基金
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国家自然科学基金项目
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兰州大学中央高校基本科研业务费专项基金
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文献收藏号
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CSCD:5858860
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参考文献 共
85
共5页
|
|
1.
Harrison S P. Late Quaternary lake-level changes and climates of Australia.
Quaternary Science Reviews,1993,12(4):211-231
|
CSCD被引
1
次
|
|
|
|
|
2.
Chen G J. Late Quaternary palaeolake levels in Tengger Desert, NW China.
Palaeogeography, Palaeoclimatology, Palaeoecology,2004,211(1):45-58
|
CSCD被引
2
次
|
|
|
|
|
3.
施雅风. 山地冰川与湖泊萎缩所指示的亚洲中部气候干暖化趋势与未来展望.
地理学报,1990,45(1):1-13
|
CSCD被引
96
次
|
|
|
|
|
4.
于革. 末次盛冰期中国湖泊记录及其气候意义.
科学通报,2000,45(3):250-255
|
CSCD被引
34
次
|
|
|
|
|
5.
薛滨. 中国古湖泊水位记录及末次间冰阶以来大气环流变化.
地质学报,2000,74(4):379-380
|
CSCD被引
1
次
|
|
|
|
|
6.
Chen F H. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history.
Quaternary Science Reviews,2008,27(3/4):351-364
|
CSCD被引
217
次
|
|
|
|
|
7.
Li Y. Multiple factors causing Holocene lake-level change in monsoonal and arid central Asia as identified by model experiments.
Climate Dynamics,2010,35(6):1119-1132
|
CSCD被引
18
次
|
|
|
|
|
8.
郑景云. 中国气候区划新方案.
地理学报,2010,65(1):3-12
|
CSCD被引
184
次
|
|
|
|
|
9.
沈吉. 末次盛冰期以来中国湖泊时空演变及驱动机制研究综述:来自湖泊沉积的证据.
科学通报,2012,57(34):3228-3242
|
CSCD被引
34
次
|
|
|
|
|
10.
吴敬禄. 新疆干旱区湖泊演化及其气候水文特征.
海洋地质与第四纪地质,2011,31(2):135-143
|
CSCD被引
16
次
|
|
|
|
|
11.
姜世中.
气象学与气候学,2010
|
CSCD被引
5
次
|
|
|
|
|
12.
Peel M C. Updated world map of the Koppen-Geiger climate classification.
Hydrology& Earth System Sciences Discussions,2007,4(2):439-473
|
CSCD被引
20
次
|
|
|
|
|
13.
Kottek M. World map of the Koppen-Geiger climate classification updated.
Meteorologische Zeitschrift,2006,15(3):259-263
|
CSCD被引
100
次
|
|
|
|
|
14.
Trenberth K E. The global monsoon as seen through the divergent atmospheric circulation.
Journal of Climate,2000,13(13):3969-3993
|
CSCD被引
59
次
|
|
|
|
|
15.
Berger A. Long-term variations of caloric insolation resulting from the earth's orbital elements.
Quaternary Research,1978,9(2):139-167
|
CSCD被引
76
次
|
|
|
|
|
16.
Wang B. Changes in global monsoon precipitation over the past 56 years.
Geophysical Research Letters,2006,33(6):272-288
|
CSCD被引
9
次
|
|
|
|
|
17.
Wang B. Global monsoon: Dominant mode of annual variation in the tropics.
Dynamics of Atmospheres & Oceans,2008,44(3/4):165-183
|
CSCD被引
66
次
|
|
|
|
|
18.
Liu J. Centennial variations of the global monsoon precipitation in the Last Millennium: Results from ECHO-G Model.
Journal of Climate,2009,22(22):2356-2371
|
CSCD被引
28
次
|
|
|
|
|
19.
Wang B. Recent change of the global monsoon precipitation (1979-2008).
Climate Dynamics,2011,39(5):1123-1135
|
CSCD被引
1
次
|
|
|
|
|
20.
黄荣辉. 夏季东亚季风区水汽输送特征及其与南亚季风区水汽输送的差别.
大气科学,1998,28(4):460-469
|
CSCD被引
172
次
|
|
|
|
|
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