Reorganization of Asian climate in relation to Tibetan Plateau uplift
Reorganization of the Asian climate from one dominated by global planetary wind systems
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …
to a regional monsoon climate is closely related to the surface uplift of the Tibetan Plateau …
Cenozoic evolution of the steppe-desert biome in Central Asia
The origins and development of the arid and highly seasonal steppe-desert biome in Central
Asia, the largest of its kind in the world, remain largely unconstrained by existing records. It …
Asia, the largest of its kind in the world, remain largely unconstrained by existing records. It …
Orographic evolution of northern Tibet shaped vegetation and plant diversity in eastern Asia
The growth of the Tibetan Plateau throughout the past 66 million years has profoundly
affected the Asian climate, but how this unparalleled orogenesis might have driven …
affected the Asian climate, but how this unparalleled orogenesis might have driven …
Late Miocene–Quaternary rapid stepwise uplift of the NE Tibetan Plateau and its effects on climatic and environmental changes
J Li, X Fang, C Song, B Pan, Y Ma, M Yan - Quaternary Research, 2014 - cambridge.org
The way in which the NE Tibetan Plateau uplifted and its impact on climatic change are
crucial to understanding the evolution of the Tibetan Plateau and the development of the …
crucial to understanding the evolution of the Tibetan Plateau and the development of the …
A review of orbital-scale monsoon variability and dynamics in East Asia during the Quaternary
Quaternary monsoon changes in East Asia have been extensively investigated by proxy
records from continental and marine archives. However, these proxy indicators often show …
records from continental and marine archives. However, these proxy indicators often show …
Impacts of uplift of northern Tibetan Plateau and formation of Asian inland deserts on regional climate and environment
Based on the geological evidence that the northern Tibetan Plateau (NTP) had an uplift of a
finite magnitude since the Miocene and the major Asian inland deserts formed in the early …
finite magnitude since the Miocene and the major Asian inland deserts formed in the early …
Cenozoic sediment flux in the Qaidam Basin, northern Tibetan Plateau, and implications with regional tectonics and climate
J Bao, Y Wang, C Song, Y Feng, C Hu, S Zhong… - Global and Planetary …, 2017 - Elsevier
Abstract As the largest Mesozoic-Cenozoic terrestrial intermountain basin in the northern
Tibetan Plateau, the Qaidam Basin is an ideal basin to examine the influences of regional …
Tibetan Plateau, the Qaidam Basin is an ideal basin to examine the influences of regional …
Warming‐induced northwestward migration of the Asian summer monsoon in the geological past: Evidence from climate simulations and geological reconstructions
X Huang, S Yang, A Haywood, D Jiang… - Journal of …, 2021 - Wiley Online Library
The cold and warm intervals during the Plio‐Pleistocene provide an opportunity to assess
the response of the Asian summer monsoon (ASM) to different levels of global warming. In …
the response of the Asian summer monsoon (ASM) to different levels of global warming. In …
Chronology and paleoenvironmental records of a drill core in the central Tengger Desert of China
Z Li, D Sun, F Chen, F Wang, Y Zhang, F Guo… - Quaternary Science …, 2014 - Elsevier
The desertification history of inland Asia provides most direct evidence for Asian drying
history, but the formation ages of the most Asian deserts are not clear due to the lack of …
history, but the formation ages of the most Asian deserts are not clear due to the lack of …
Northern hemisphere ice sheet expansion intensified Asian aridification and the winter monsoon across the mid-Pleistocene transition
Abstract The mid-Pleistocene transition 1.25 to 0.6 million years ago marked a major shift in
global climate periodicity from 41,000 to around 100,000 years without a concomitant orbital …
global climate periodicity from 41,000 to around 100,000 years without a concomitant orbital …