supported by the National Natural Science Foundation of China(Grant Nos.42361144879&42303063);the National Key Research and Development Project(Grant No.2020YFA0607700);the Second Tibetan Plateau Scientific Expedition and Research(STEP)Program(Grant No.2019QZKK0707);the Tianjin Natural Science Foundation(Grant No.22JCQNJC00140);supported by the Science and Technology Innovation Project for Training Leading Talent of Tianjin University。
The terrestrial cosmogenic nuclide dataset consisting of 1233^(10)Be measurements of fluvial sediment samples across the Asian mountain belts is used to constrain the influence of climate,tectonics and topography on E...
supported by the National Natural Science Foundation of China(Grant Nos.42072205&41301582);the National Key R&D Program of China(Grant No.2022YFF0801501);the Innovation Group Project of Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai)(Grant No.311022010)。
Reconstructing the Holocene megaflood history is a key component of understanding the mechanism of past climate change and assessing the potential impact of future catastrophic events.The Pearl River is the longest wa...
supported by the National Natural Science Foundation of China (Nos. 41772029, 41322013);Natural Science Foundation for Distinguished Young Scholars of Hubei Province of China (No. 2016CFA051);the Program of Introducing Talents of Discipline to Universities (Nos. B14031, B08030);the Fundamental Research Funds for the Central Universities, China University of Geosciences (Wuhan) (Nos. CUGCJ1703, CUGQYZX1705);Hydrogeological Environmental Geological Survey of Kashi, Xinjiang (No. S15-2LQ1)。
Paleoclimate changes during the last glacial in the arid central Asia are not as well understood as the monsoon-dominated areas of Asia. Here we report a 75-m-long sediment core over past 120 kyr based on astronomical...
supported by the National Natural Science Foundation of China (Grant Nos. 41822708 and 41571178);the Strategic Priority Research Program of Chinese Academy of Sciences (Grant No. XDA20100102);the Fundamental Research Funds for the Central Universities (Grant No. lzujbky-2018-k15);the Second Tibetan Plateau Scientific Expedition (STEP) program (Grant No. XDA20060700)
Lakes have received considerable attention as long-term sinks for organic carbon(C)at regional and global scales.Previ ous studies have focused on assessment and quantification of carbon sinks,and few have worked on t...
With the support by the National Natural Science Foundation of China,Prof.Li Yu(李育)and his colleagues at the College of Earth and Environmental Science,Lanzhou University,reported a record of millennial-scale monsoo...
supported by the National Natural Science Foundation of China (Grant No. 41371009);the Fundamental Research Fund for the Central Universities of China (Grant No. lzujbky2013-127)
Ecosystem response to climate change in high-altitude regions is a focus on global change research. Picea/Abies forests are widely distributed at high altitudes of East and Central Asia, and their distribution changes...
supported by the Special Foundation for the National Science and Technology Major Project of China(2011FY120300);the National Natural Science Foundation of China(41001058)
This study employed proxy data to investigate the phase relationship between the North Atlantic deep-level temperature and the Qinghai-Tibet Plateau(TP)surface air temperature(TP temperature)and its evolution at the m...
by the Chinese National Natural Science Foundation (40971005)
The Hunshandake Desert is located at the northern edge of the East Asian monsoon region,and its natural environment is sensitive to monsoonal changes.Geologic records suggest that desert evolution corresponding to cli...
supported by the National Natural Science Foundation of China (Grant Nos. 40631003 and 40771009) ;Innovation Project in Graduate Education of Jiangsu Province (Grant No. CX07B-051Z)
从 Sanbao 洞的一个石笋氧同位素记录,中国,与 7 230Th 年龄和 355 氧同位素数据建立了,在现在( ka BP )前从 284~240 千年为时期向东方亚洲季风(电动会计记帐机)紧张的连续历史提供 34 ka 的典型错误。这个新记录扩大以前出版...
Whether climatic changes in high latitudes of the Northern Hemisphere since the last glaciation have effects on the Tibetan Plateau monsoon, and the variation characteristics of the Plateau monsoon itself are still no...