气候变化领域集成服务门户(CCPortal): Global warming-induced Asian hydrological climate transition across the Miocene

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DOI	10.1038/s41467-021-27054-5
	Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary
	Ao H.; Rohling E.J.; Zhang R.; Roberts A.P.; Holbourn A.E.; Ladant J.-B.; Dupont-Nivet G.; Kuhnt W.; Zhang P.; Wu F.; Dekkers M.J.; Liu Q.; Liu Z.; Xu Y.; Poulsen C.J.; Licht A.; Sun Q.; Chiang J.C.H.; Liu X.; Wu G.; Ma C.; Zhou W.; Jin Z.; Li X.; Li X.; Peng X.; Qiang X.; An Z.
发表日期	2021
ISSN	2041-1723
卷号	12 期号:1
英文摘要	Across the Miocene–Pliocene boundary (MPB; 5.3 million years ago, Ma), late Miocene cooling gave way to the early-to-middle Pliocene Warm Period. This transition, across which atmospheric CO2 concentrations increased to levels similar to present, holds potential for deciphering regional climate responses in Asia—currently home to more than half of the world’s population— to global climate change. Here we find that CO2-induced MPB warming both increased summer monsoon moisture transport over East Asia, and enhanced aridification over large parts of Central Asia by increasing evaporation, based on integration of our ~1–2-thousand-year (kyr) resolution summer monsoon records from the Chinese Loess Plateau aeolian red clay with existing terrestrial records, land-sea correlations, and climate model simulations. Our results offer palaeoclimate-based support for ‘wet-gets-wetter and dry-gets-drier’ projections of future regional hydroclimate responses to sustained anthropogenic forcing. Moreover, our high-resolution monsoon records reveal a dynamic response to eccentricity modulation of solar insolation, with predominant 405-kyr and ~100-kyr periodicities between 8.1 and 3.4 Ma. © 2021, The Author(s).
语种	英语
scopus关键词	aridification; global warming; human activity; hydrology; Miocene; paleoclimate; Pliocene; Central Asia; China; Far East; Loess Plateau
来源期刊	Nature Communications
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/250565
作者单位	State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an, China; Open Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao, China; Research School of Earth Sciences, Australian National University, Canberra, ACT, Australia; Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton, United Kingdom; Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; Institute of Geosciences, Christian-Albrechts-University, Kiel, Germany; Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI, United States; Laboratoire des Sciences du Climat et de l’Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, 91191, France; Géosciences Rennes, UMR-CNRS 6118, University Rennes, Rennes, France; Department of Geosciences, Potsdam University, Potsdam, Germany; Pa...
推荐引用方式 GB/T 7714	Ao H.,Rohling E.J.,Zhang R.,等. Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary[J],2021,12(1).
APA	Ao H..,Rohling E.J..,Zhang R..,Roberts A.P..,Holbourn A.E..,...&An Z..(2021).Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary.Nature Communications,12(1).
MLA	Ao H.,et al."Global warming-induced Asian hydrological climate transition across the Miocene–Pliocene boundary".Nature Communications 12.1(2021).