Milankovitch theory and monsoon
Cheng, Hai1,2; Li, Hanying1; Sha, Lijuan1; Sinha, Ashish1,3; Shi, Zhengguo1,2; Yin, Qiuzhen4; Lu, Zhengyao5; Zhao, Debo6; Cai, Yanjun1; Hu, Yongyun7
刊名INNOVATION-THE EUROPEAN JOURNAL OF SOCIAL SCIENCE RESEARCH
2022-11-08
卷号3期号:6页码:15
ISSN号1351-1610
DOI10.1016/j.xinn.2022.100338
通讯作者Cheng, Hai(cheng021@xjtu.edu.cn)
英文摘要The widely accepted "Milankovitch theory" explains insolation-induced waxing and waning of the ice sheets and their effect on the global climate on orbital timescales. In the past half century, however, the theory has often come under scrutiny, especially regarding its "100-ka problem." Another drawback, but the one that has received less attention, is the "monsoon problem," which pertains to the exclusion of monsoon dynamics in classic Milankovitch theory even though the monsoon prevails over the vast low-latitude (similar to 30 degrees N to similar to 30 degrees S) region that covers half of the Earth's surface and receives the bulk of solar radiation. In this review, we discuss the major issues with the current form of Milankovitch theory and the progress made at the research forefront. We suggest shifting the emphasis from the ultimate outcomes of the ice volume to the causal relationship between changes in northern high-latitude insolation and ice age termination events (or ice sheet melting rate) to help reconcile the classic "100-ka problem." We discuss the discrepancies associated with the characterization of monsoon dynamics, particularly the so-called "sea-land precession-phase paradox" and the "Chinese 100-ka problem." We suggest that many of these discrepancies are superficial and can be resolved by applying a holistic " monsoon system science" approach. Finally, we propose blending the conventional Kutzbach orbital monsoon hypothesis, which calls for summer insolation forcing of monsoons, with Milankovitch theory to formulate a combined "MilankovitchKutzbach hypothesis" that can potentially explain the dual nature of orbital hydrodynamics of the ice sheet and monsoon systems, as well as their interplays and respective relationships with the northern high-latitude insolation and inter-tropical insolation differential.
资助项目National Natural Science Foundation of China[41888101] ; National Natural Science Foundation of China[42150710534]
WOS研究方向Sociology
语种英语
出版者ROUTLEDGE JOURNALS, TAYLOR & FRANCIS LTD
WOS记录号WOS:000883049100004
内容类型期刊论文
源URL[http://ir.qdio.ac.cn/handle/337002/180250]  
专题海洋研究所_海洋地质与环境重点实验室
通讯作者Cheng, Hai
作者单位1.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian 710049, Peoples R China
2.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
3.Calif State Univ Dominguez Hills, Dept Earth Sci, Carson, CA 90747 USA
4.Catholic Univ Louvain, Georges Lemaitre Ctr Earth & Climate Res, Earth & Life Inst, B-1348 Louvain La Neuve, Belgium
5.Lund Univ, Dept Phys Geog & Ecosyst Sci, Solvegatan 12, S-22362 Lund, Sweden
6.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
7.Peking Univ, Sch Phys, Dept Atmospher & Ocean Sci, Beijing 100871, Peoples R China
8.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China
9.Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China
推荐引用方式
GB/T 7714
Cheng, Hai,Li, Hanying,Sha, Lijuan,et al. Milankovitch theory and monsoon[J]. INNOVATION-THE EUROPEAN JOURNAL OF SOCIAL SCIENCE RESEARCH,2022,3(6):15.
APA Cheng, Hai.,Li, Hanying.,Sha, Lijuan.,Sinha, Ashish.,Shi, Zhengguo.,...&Zhang, Haiwei.(2022).Milankovitch theory and monsoon.INNOVATION-THE EUROPEAN JOURNAL OF SOCIAL SCIENCE RESEARCH,3(6),15.
MLA Cheng, Hai,et al."Milankovitch theory and monsoon".INNOVATION-THE EUROPEAN JOURNAL OF SOCIAL SCIENCE RESEARCH 3.6(2022):15.
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