F Chen, D Wu, J Chen, A Zhou, J Yu, J Shen… - Quaternary Science …, 2016 - Elsevier
Climatic and environmental changes in the northeastern Tibetan Plateau are controlled by the Asian summer monsoon (ASM) and the westerlies, two key circulation components of the …
Abstract The International Commission on Stratigraphy (ICS) utilises benchmark chronostratigraphies to divide geologic time. The reliability of these records is fundamental …
Dune systems can have alternative stable states that coexist under certain environmental conditions: a vegetated, stabilized state and a bare active state. This behavior implies the …
H Jin, X Jin, R He, D Luo, X Chang, S Wang… - Science China Earth …, 2019 - Springer
The formation and evolution of permafrost in China during the last 20 ka were reconstructed on the basis of large amount of paleo-permafrost remains and paleo-periglacial evidence …
It is proposed that an extremely warm, humid climate existed in the Tibetan Plateau (TP), including the currently hyper-arid Qaidam Basin (QB), during Marine isotope stage 3 (MIS 3) …
Q Jiang, Q Hao, S Peng, Y Qiao - Aeolian Research, 2020 - Elsevier
Abstract Knowledge of dust sources is crucial for understanding the aeolian system of the Xiashu loess which is distributed in the middle and lower reaches of the Yangtze River and …
H Zhou, W Zhao, Z He, J Yan, G Zhang - Journal of Hydrology, 2019 - Elsevier
Mongolian pine (Pinus sylvestris var. mongolica) has been widely used in vegetation restoration and for windbreaks in sandy regions of northern China where water is the …
Z Ding, R Lu, L Wang, L Yu, X Liu, Y Liu, L Liu, M Bai… - Geoderma, 2021 - Elsevier
Climatic changes of the early-mid Holocene in the monsoon margin of northwest China have long been debated. The extensive eolian deposits of the desert/loess transition in central …