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Milankovitch theory...
Milankovitch theory and monsoon
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- Cheng, Hai (författare)
- Xi'an Jiaotong University
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- Li, Hanying (författare)
- Xi'an Jiaotong University
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- Sha, Lijuan (författare)
- Xi'an Jiaotong University
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- Sinha, Ashish (författare)
- Xi'an Jiaotong University
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- Shi, Zhengguo (författare)
- Xi'an Jiaotong University
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- Yin, Qiuzhen (författare)
- Catholic University of Louvain
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- Lu, Zhengyao (författare)
- Lund University,Lunds universitet,MERGE: ModElling the Regional and Global Earth system,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,Institutionen för naturgeografi och ekosystemvetenskap,Centre for Environmental and Climate Science (CEC),Faculty of Science,Dept of Physical Geography and Ecosystem Science
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- Zhao, Debo (författare)
- Institute of Oceanology, Chinese Academy of Sciences
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- Cai, Yanjun (författare)
- Xi'an Jiaotong University
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- Hu, Yongyun (författare)
- Peking University
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- Hao, Qingzhen (författare)
- Institute of Geology and Geophysics, Chinese Academy of Sciences
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Tian, Jun (författare)
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- Kathayat, Gayatri (författare)
- Xi'an Jiaotong University
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- Dong, Xiyu (författare)
- Xi'an Jiaotong University
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- Zhao, Jingyao (författare)
- Xi'an Jiaotong University
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- Zhang, Haiwei (författare)
- Xi'an Jiaotong University
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(creator_code:org_t)
- Elsevier BV, 2022
- 2022
- Engelska.
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Ingår i: The Innovation. - : Elsevier BV. - 2666-6758. ; 3:6
- Relaterad länk:
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http://dx.doi.org/10... (free)
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https://lup.lub.lu.s...
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https://doi.org/10.1...
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Abstract
Ämnesord
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- 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 (∼30° N to ∼30° 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 “Milankovitch-Kutzbach 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.
Ämnesord
- NATURVETENSKAP -- Geovetenskap och miljövetenskap (hsv//swe)
- NATURAL SCIENCES -- Earth and Related Environmental Sciences (hsv//eng)
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Cheng, Hai
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Li, Hanying
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Sha, Lijuan
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Sinha, Ashish
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Shi, Zhengguo
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Yin, Qiuzhen
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visa fler...
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Lu, Zhengyao
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Zhao, Debo
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Cai, Yanjun
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Hu, Yongyun
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Hao, Qingzhen
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Tian, Jun
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Kathayat, Gayatr ...
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Dong, Xiyu
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Zhao, Jingyao
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Zhang, Haiwei
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The Innovation
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