轨道尺度亚洲气候演化机理的数值模拟:历史与展望
NUMERICAL SIMULATION RESEARCHES ON ORBITAL-SCALE ASIAN CLIMATE DYNAMICS:HISTORY AND PERSPECTIVE
查看参考文献94篇
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文摘
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轨道尺度亚洲气候演化是古气候热点问题之一,其变化过程和机理对理解当前全球变暖下亚洲气候变化具有重要参考意义。最近几十年,基于黄土、石笋、湖泊等载体的轨道尺度亚洲气候重建研究获得显著进展,气候演化历史的基本框架已被构建,不同区域和指标记录之间的差异暗示了气候演化机理的复杂性。数值模拟作为研究气候动力学的重要工具之一,在轨道尺度亚洲气候变化中也得到广泛应用和快速发展。基于此,本文尝试对最近十数年轨道尺度亚洲气候演化机理的数值模拟研究做一简单总结和梳理。目前的数值模拟尚未对地质记录给出的各种变化特征、区域差异等现象,尤其是东亚夏季风的黄土和石笋差异、季风和干旱气候的耦合关系等,给出合理解释。因此,在未来工作中亟须涵盖多轨道旋回的高分辨率瞬变试验,结合良好定年的重建记录,以期对轨道尺度亚洲气候变化机理获得更深入完整的认识。 |
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其他语种文摘
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Orbital-scale Asian climate evolution is one of the hot topics of paleoclimate researches, and its changing processes and mechanisms have significant value for understanding the Asian climate change under current global warming. In recent decades, researches on orbital-scale Asian climate reconstruction, based on loess, stalagmites, lake sediments and other proxies, have achieved prominent progress and the basic framework of Asian climate evolution has been constructed. Differences between regions and proxy records suggest the complicated mechanisms of Asian climate change. As one of the important tools to explore climate dynamics, numerical simulations have been widely used and rapidly developed in the orbital-scale Asian climate studies. Based on this, this paper attempts to summarize the advances of the numerical studies on mechanisms of orbital-scale Asian climate during the past several years. The current numerical simulations have not yet given reasonable explanations to a variety of variation characteristics and regional differences in geological records, especially the difference between loess and stalagmites about the East Asian summer monsoon, and the relationship between monsoon and arid climate. Therefore, high-resolution transient experiments covering multi-orbital cycles, in combination with good dating proxies,are required in the future work to gain comprehensive understanding of the orbital-scale climate dynamics over Asia. |
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来源
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第四纪研究
,2020,40(1):8-17 【核心库】
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DOI
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10.11928/j.issn.1001-7410.2020.01.02
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关键词
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亚洲气候
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轨道尺度
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动力机制
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数值模拟
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地址
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中国科学院地球环境研究所, 黄土与第四纪地质国家重点实验室, 陕西, 西安, 710061
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中国科学院第四纪科学与全球变化卓越创新中心, 中国科学院第四纪科学与全球变化卓越创新中心, 陕西, 西安, 710061
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西安交通大学全球环境变化研究院, 陕西, 西安, 710049
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北京师范大学地球科学前沿交叉研究中心, 北京, 100875
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语种
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中文 |
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文献类型
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综述型 |
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ISSN
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1001-7410 |
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学科
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大气科学(气象学);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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中国科学院青年创新促进会共同资助
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文献收藏号
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CSCD:6656861
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参考文献 共
94
共5页
|
|
1.
An Z. Global monsoon dynamics and climate change.
Annual Review of Earth and Planetary Sciences,2015,43(1):29-77
|
被引
13
次
|
|
|
|
|
2.
Sung M K. A possible impact of the North Atlantic Oscillation on the East Asian summer monsoon precipitation.
Geophysical Research Letters,2006,33(21):L21713
|
被引
21
次
|
|
|
|
|
3.
Wang B. Pacific-East Asian teleconnection: How does ENSO affect East Asian climate?.
Journal of Climate,2000,13(9):1517-1536
|
被引
502
次
|
|
|
|
|
4.
Liu X D. Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution.
Chinese Science Bulletin,2013,58(34):4277-4291
|
被引
29
次
|
|
|
|
|
5.
Liu Z. Chinese cave records and the East Asia summer monsoon.
Quaternary Science Reviews,2014,83(1):115-128
|
被引
37
次
|
|
|
|
|
6.
Zhang X. Abrupt glacial climate shifts controlled by ice sheet changes.
Nature,2014,512:290-294
|
被引
14
次
|
|
|
|
|
7.
Berger A. Long-term variations of caloric insolation resulting from the Earth's orbital elements.
Quaternary Research,1978,9(2):139-167
|
被引
75
次
|
|
|
|
|
8.
Laskar J. Long-term solution for the insolation quantities of the Earth.
Proceedings of the International Astronomical Union,2004,2(14):101-106
|
被引
4
次
|
|
|
|
|
9.
Chen F. Moisture changes over the last millennium in arid Central Asia: A review, synthesis and comparison with monsoon region.
Quaternary Science Reviews,2010,29(7/8):1055-1068
|
被引
8
次
|
|
|
|
|
10.
Sun Y. Astronomical timescale and palaeoclimatic implication of stacked 3.6-Myr monsoon records from the Chinese Loess Plateau.
Quaternary Science Reviews,2006,25(1):33-48
|
被引
32
次
|
|
|
|
|
11.
Wang Y. Millennial-and orbitalscale changes in the East Asian monsoon over the past 224, 000 years.
Nature,2008,451:1090-1093
|
被引
81
次
|
|
|
|
|
12.
An Z. Glacial-interglacial Indian summer monsoon dynamics.
Science,2011,333(6043):719-723
|
被引
14
次
|
|
|
|
|
13.
Cheng H. Climate variations of Central Asia on orbital to millennial timescales.
Scientific Reports,2016,6:36975
|
被引
28
次
|
|
|
|
|
14.
Lu H. Periodicities of palaeoclimatic variations recorded by loess-paleosol sequences in China.
Quaternary Science Reviews,2004,23(18):1891-1900
|
被引
13
次
|
|
|
|
|
15.
Braconnot P. How well do PMIP simulations reproduce African monsoon and ENSO?.
Quaternary International,2012,279/280:64
|
被引
1
次
|
|
|
|
|
16.
Harrison S P. Evaluation of CMIP5 palaeo-simulations to improve climate projections.
Nature Climate Change,2015,5:735-743
|
被引
9
次
|
|
|
|
|
17.
Kutzbach J E. Simulation of the evolutionary response of global summer monsoons to orbital forcing over the past 280, 000 years.
Climate Dynamics,2008,30(6):567-579
|
被引
22
次
|
|
|
|
|
18.
Liu Z. Evolution and forcing mechanisms of El Nino over the past 21,000 years.
Nature,2014,515:550-553
|
被引
12
次
|
|
|
|
|
19.
Weber S L. The impact of varying ice sheets and greenhouse gases on the intensity and timing of boreal summer monsoons.
Quaternary Science Reviews,2011,30(3):469-479
|
被引
7
次
|
|
|
|
|
20.
Kutzbach J E. Monsoon climate of the Early Holocene: Climate experiment with the Earth's orbital parameters for 9000 years ago.
Science,1981,214(4516):59-61
|
被引
53
次
|
|
|
|
|
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