Response of terrace deposit thickness to climate change and tectonic deformation: An example of the Liyuan River in the Northeast Tibetan Plateau

Terra Nova ◽  
2021 ◽  
Author(s):  
Zhenling Wen ◽  
Dianbao Chen ◽  
Lianyong Guo ◽  
Baotian Pan ◽  
Xiaofei Hu ◽  
...  
Keyword(s):  
Climate Change ◽  
Tibetan Plateau ◽  
Tectonic Deformation ◽  
Deposit Thickness ◽  
Terrace Deposit

Multiproxy records in middle–late Miocene sediments from the Wushan Basin: Implications for climate change and tectonic deformation in the northeastern Tibetan Plateau

2020 ◽  
Vol 133 (1-2) ◽  
pp. 149-158 ◽  
Author(s):  
Weitao Wang ◽  
Peizhen Zhang ◽  
Zhicai Wang ◽  
Kang Liu ◽  
Hongyan Xu ◽  
...  
Keyword(s):  
Climate Change ◽  
Magnetic Susceptibility ◽  
Tibetan Plateau ◽  
Late Miocene ◽  
Phase Changes ◽  
Dominant Factor ◽  
Tectonic Deformation ◽  
The Tibetan Plateau ◽  
Global Cooling ◽  
Δ18o And Δ13c

Abstract To help understand the relationship between global cooling and Tibetan uplift in the middle to late Miocene, multiple proxy data including carbonate stable isotope records, magnetic susceptibility, and sediment color references were obtained from a magnetostratigraphic section (14.5–6.0 Ma) of the Wushan Basin along the northeastern margin of the Tibetan Plateau. New proxies identify two phase changes that may have been controlled by global cooling and tectonic deformation at this time. During 14.5–13.2 Ma, positive shifts of ∼2.0‰ in δ18O and δ13C, an increase in lightness (L*), and a decrease in redness (a*) suggest gradually increasing aridity. Relatively high δ18O and δ13C values and low a*/L* and magnetic susceptibility values continue until ca. 10 Ma, when δ18O and δ13C significantly decrease and redness as well as magnetic susceptibility significantly increase. The negative shifts in δ18O and δ13C and increases in redness and magnetic susceptibility at 10 Ma are consistent with coeval basin environment and provenance changes. Combining these data with basin analysis, we suggest that global cooling was the dominant factor and Tibetan uplift was the subordinate factor for the middle Miocene aridification of the Wushan Basin. In contrast, the contribution of Tibetan uplift was dominant and global climate change was subordinate in the late Miocene basin paleogeographic reorganization.

scholarly journals Contrasting Evolution Patterns of Endorheic and Exorheic Lakes on the Central Tibetan Plateau and Climate Cause Analysis during 1988–2017

Water ◽  
2021 ◽  
Vol 13 (14) ◽  
pp. 1962
Author(s):  
Zhilong Zhao ◽  
Yue Zhang ◽  
Zengzeng Hu ◽  
Xuanhua Nie
Keyword(s):  
Climate Change ◽  
Tibetan Plateau ◽  
Climatic Factors ◽  
Global Climate ◽  
Rapid Expansion ◽  
Annual Precipitation ◽  
The Tibetan Plateau ◽  
Lake Area ◽  
Climate Change Research ◽  
Mean Temperature

The alpine lakes on the Tibetan Plateau (TP) are indicators of climate change. The assessment of lake dynamics on the TP is an important component of global climate change research. With a focus on lakes in the 33° N zone of the central TP, this study investigates the temporal evolution patterns of the lake areas of different types of lakes, i.e., non-glacier-fed endorheic lakes and non-glacier-fed exorheic lakes, during 1988–2017, and examines their relationship with changes in climatic factors. From 1988 to 2017, two endorheic lakes (Lake Yagenco and Lake Zhamcomaqiong) in the study area expanded significantly, i.e., by more than 50%. Over the same period, two exorheic lakes within the study area also exhibited spatio-temporal variability: Lake Gaeencuonama increased by 5.48%, and the change in Lake Zhamuco was not significant. The 2000s was a period of rapid expansion of both the closed lakes (endorheic lakes) and open lakes (exorheic lakes) in the study area. However, the endorheic lakes maintained the increase in lake area after the period of rapid expansion, while the exorheic lakes decreased after significant expansion. During 1988–2017, the annual mean temperature significantly increased at a rate of 0.04 °C/a, while the annual precipitation slightly increased at a rate of 2.23 mm/a. Furthermore, the annual precipitation significantly increased at a rate of 14.28 mm/a during 1995–2008. The results of this study demonstrate that the change in precipitation was responsible for the observed changes in the lake areas of the two exorheic lakes within the study area, while the changes in the lake areas of the two endorheic lakes were more sensitive to the annual mean temperature between 1988 and 2017. Given the importance of lakes to the TP, these are not trivial issues, and we now need accelerated research based on long-term and continuous remote sensing data.

Spring phenology outweighed climate change in determining autumn phenology on the Tibetan Plateau

2021 ◽  
Vol 41 (6) ◽  
pp. 3725-3742
Author(s):  
Jie Peng ◽  
Chaoyang Wu ◽  
Xiaoyue Wang ◽  
Linlin Lu
Keyword(s):  
Climate Change ◽  
Tibetan Plateau ◽  
The Tibetan Plateau ◽  
Spring Phenology

scholarly journals Seasonal Response of Grasslands to Climate Change on the Tibetan Plateau

PLoS ONE ◽  
2012 ◽  
Vol 7 (11) ◽  
pp. e49230 ◽  
Author(s):  
Haiying Yu ◽  
Jianchu Xu ◽  
Erick Okuto ◽  
Eike Luedeling
Keyword(s):  
Climate Change ◽  
Tibetan Plateau ◽  
The Tibetan Plateau
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