supported by the National Natural Science Foundation of China(41988101);the International Partnership Program of Chinese Academy of Sciences for Future Network Project(162GJHZ2023053FN).
The spheres of the Earth—specifically the lithosphere,hydrosphere,atmosphere,and biosphere—are intricately connected and interact through the fluxes of matter and energy,forming a complex and ever-evolving Earth sys...
supported by the National Research Foundation of Korea(NRF) grant(NRF-2018R1A5A1024958)。
Understanding the regional hydrological response to varying CO_(2)concentration is critical for cost-benefit analysis of mitigation and adaptation polices in the near future. To characterize summer monsoon rainfall ch...
supported by the National Natural Science Foundation of China(41790421,41722105,41988101)。
Asian dust storms have long been a major environmental concern in China,affecting the lives of about one billion people.However,it is unclear whether the mechanisms responsible for Asian dust storms during the Holocen...
supported by the Strategic Priority Research Program of Chinese Academy of Sciences(XDB40010200 and XDA2009000004);the Program of Global Change and Mitigation;Ministry of Science and Technology of China(2016YFA0600502);the National Natural Science Foundation of China(41877293,41672162,41977381,and 41472315)。
Orbital-scale global climatic changes during the late Quaternary are dominated by high-latitude influenced~100,000-year global ice-age cycles and monsoon influenced~23,000-year low-latitude hydroclimate variations.How...
supported by the Natural Science Foundation for Distinguished Young Scholars of Hubei Province of China (2016CFA051);the National Natural Science Foundation of China (41772029, 41322013);Overseas Expertise Introduction Project for Discipline Innovation (B08030);the National Basic Research Program of China (2014CB239101);the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (CUGCJ1703, CUGQYZX1705)
Nearly 90% of the Ediacaran Period(635–541 Ma) of the Neoproterozoic is represented by the Doushantuo Formation(DST Fm) in South China.Its lowest Member I is a 3.7 m-thick cap carbonate deposited at the termination o...
supported by the National Basic Research Program of China (2011CB403606);the National Natural Science Foundation of China (40830854 and 40806001)
The diffusion boundary layer (DBL) significantly limits the exchange between sediment and overlying water and therefore becomes a bottleneck of diffusive vertical flux at the sediment-water interface (SWI). Variable D...
This work was supported by the National Natural Science Foundation of China (Grant No. 49775261); the "Research Program for State Excellent Key Laboratory (Grant No. 49823002); and the Study on Formation Mechanism of Key Weather Disaster in China (Gran
The tropical heating and transient activity features during the period of the persistent anomaly of summertime circulation over the Ural Mountains are studied, and a possible mechanism responsible for formation and ma...
This note presents a new result of terrestrial mollusk study from the Luochuan loesssection since the last 250 ka. A total of 213 samples, taken at intervals of 10 cm in the S0-L3 portion, were analyzed for fossil mol...
Based on the climate records derived from loess deposits in north-central China, the characteristics of the East-Asia paleomonsoonal changes during the Late Pleistocene are summarized as follows: (ⅰ) The 0.1_Ma clima...
The distribution of global persistent anomalies shows that the subtropical western Pacific is a key region with high_frequency occurrence of persistent anomalies. Analyses of streamfunction anomalies, OLR anomalies et...