Climate change, vegetation history, and landscape responses on the Tibetan Plateau during the Holocene: A comprehensive review

F Chen, J Zhang, J Liu, X Cao, J Hou, L Zhu… - Quaternary Science …, 2020 - Elsevier
Numerous studies of changes in the climate, vegetation and landscape responses of the
Tibetan Plateau (TP) during the Holocene have been published in recent decades …

The global monsoon across time scales: Mechanisms and outstanding issues

PX Wang, B Wang, H Cheng, J Fasullo, ZT Guo… - Earth-Science …, 2017 - Elsevier
The present paper addresses driving mechanisms of global monsoon (GM) variability and
outstanding issues in GM science. This is the second synthesis of the PAGES GM Working …

An optimized scheme of lettered marine isotope substages for the last 1.0 million years, and the climatostratigraphic nature of isotope stages and substages

LB Railsback, PL Gibbard, MJ Head… - Quaternary Science …, 2015 - Elsevier
A complete and optimized scheme of lettered marine isotope substages spanning the last
1.0 million years is proposed. Lettered substages for Marine Isotope Stage (MIS) 5 were …

Milankovitch theory and monsoon

H Cheng, H Li, L Sha, A Sinha, Z Shi, Q Yin, Z Lu… - The Innovation, 2022 - cell.com
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 …

A persistent Holocene wetting trend in arid central Asia, with wettest conditions in the late Holocene, revealed by multi-proxy analyses of loess-paleosol sequences in …

F Chen, J Jia, J Chen, G Li, X Zhang, H **e… - Quaternary Science …, 2016 - Elsevier
There are significant differences in the interpretation of the moisture (precipitation) history of
arid central Asia (ACA) during the Holocene, as inferred on one hand from speleothem …

Sea-level variability over five glacial cycles

KM Grant, EJ Rohling, CB Ramsey, H Cheng… - Nature …, 2014 - nature.com
Research on global ice-volume changes during Pleistocene glacial cycles is hindered by a
lack of detailed sea-level records for time intervals older than the last interglacial. Here we …

Palaeoclimatic records of the loess/palaeosol sequences of the Chinese Loess Plateau

BA Maher - Quaternary Science Reviews, 2016 - Elsevier
Whether during past climate stages or into a progressively warming world, changes in
precipitation constitute a key component of climatic change. Quantitative proxies for palaeo …

Hydroclimatic changes in China and surroundings during the Medieval Climate Anomaly and Little Ice Age: spatial patterns and possible mechanisms

J Chen, F Chen, S Feng, W Huang, J Liu… - Quaternary science …, 2015 - Elsevier
Investigating hydroclimatic changes during key periods such as the Medieval Climate
Anomaly (MCA, 1000–1300 AD) and the Little Ice Age (LIA, 1400–1900 AD) is of …

[HTML][HTML] Indian monsoon variability on millennial-orbital timescales

G Kathayat, H Cheng, A Sinha, C Spötl, RL Edwards… - Scientific reports, 2016 - nature.com
The Indian summer monsoon (ISM) monsoon is critical to billions of people living in the
region. Yet, significant debates remain on primary ISM drivers on millennial-orbital …

Chinese stalagmite paleoclimate researches: A review and perspective

H Cheng, H Zhang, J Zhao, H Li, Y Ning… - Science China Earth …, 2019 - Springer
Stalagmite is one kind of secondary carbonates formed in limestone caves (speleothem).
After cave water droplets containing Ca 2+ and HCO _3^-HCO 3− drip onto floor, carbonate …