Hydrological Extremes in the Upper Yangtze River Over the Past 700 yr Inferred From a Tree Ring <i>δ</i> <sup>18</sup> O Record-Reference-Cited by-同舟云学术

Hydrological Extremes in the Upper Yangtze River Over the Past 700 yr Inferred From a Tree Ring δ ¹⁸ O Record

Published:2022-05-18 Issue:10 Volume:127 Page:
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:JGR Atmospheres

Author:

An Wenling¹,Li Jinjian²^ORCID,Wang Shu³,Xu Chenxi¹⁴^ORCID,Shao Xuemei⁵,Qin Ningsheng³,Guo Zhengtang¹⁴^ORCID

Affiliation:

1. Key Laboratory of Cenozoic Geology and Environment Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

2. School of Atmospheric Sciences Plateau Atmosphere and Environment Key Laboratory of Sichuan Province Chengdu University of Information Technology Chengdu China

3. Institute of Plateau Meteorology China Meteorological Administration Chengdu/Heavy Rain and Drought‐Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province Chengdu China

4. CAS Center for Excellence in Life and Paleoenvironment Beijing China

5. Key Laboratory of Land Surface Pattern and Simulation Institute of Geographic Sciences and Natural Resources Chinese Academy of Sciences Beijing China

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JD036109

Reference85 articles.

1. Relative humidity history on the Batang–Litang Plateau of western China since 1755 reconstructed from tree-ring δ18O and δD

2. A 576-Year Weber River Streamflow Reconstruction from Tree Rings for Water Resource Risk Assessment in the Wasatch Front, Utah

3. Response of the Indian summer monsoon to global warming, solar geoengineering and its termination

4. Reconstruction of soil water oxygen isotope values from tree ring cellulose and its implications for paleoclimate studies

5. Recent European drought extremes beyond Common Era background variability

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