Articles | Volume 14, issue 5
https://doi.org/10.5194/cp-14-653-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-14-653-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Decreasing Indian summer monsoon on the northern Indian sub-continent during the last 180 years: evidence from five tree-ring cellulose oxygen isotope chronologies
Chenxi Xu
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and
Geophysics, Chinese Academy of Sciences, Beijing 100029, China
CAS Center for Excellence in Life and Paleoenvironment, Beijing,
100044, China
Masaki Sano
CORRESPONDING AUTHOR
Research Institute for Humanity and Nature, 457-4 Motoyama, Kamigamo,
Kita, Kyoto, Japan
Faculty of Human Sciences, Waseda University, 2-579-15 Mikajima, Tokorozawa
359-1192, Japan
Ashok Priyadarshan Dimri
School of Environmental Sciences, Jawaharlal Nehru University, New Delhi,
India
Rengaswamy Ramesh
Geoscience Division, Physical Research Laboratory, Navrangpura, Ahmedabad
380009, India
School of Earth and Planetary Sciences, National Institute of Science
Education and Research, Odisha 752050, India
deceased, April 2018
Takeshi Nakatsuka
Research Institute for Humanity and Nature, 457-4 Motoyama, Kamigamo,
Kita, Kyoto, Japan
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and
Geophysics, Chinese Academy of Sciences, Beijing 100029, China
CAS Center for Excellence in Life and Paleoenvironment, Beijing,
100044, China
Zhengtang Guo
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and
Geophysics, Chinese Academy of Sciences, Beijing 100029, China
CAS Center for Excellence in Life and Paleoenvironment, Beijing,
100044, China
University of Chinese Academy of Sciences, Beijing, China
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- Tree rings reveal recent intensified spring drought in the central Himalaya, Nepal S. Panthi et al. 10.1016/j.gloplacha.2017.08.012
- Moisture source signals preserved in a 242-year tree-ring δ18O chronology in the western Himalaya M. Sano et al. 10.1016/j.gloplacha.2017.08.009
- Regional drought shifts (1710–2010) in East Central Asia and linkages with atmospheric circulation recorded in tree-ring δ18O G. Xu et al. 10.1007/s00382-018-4215-2
- Decadal variability of precipitation over the Tibetan Plateau modulated by the 11-year solar cycle over the past millennium Y. Hu et al. 10.3389/feart.2023.1137205
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
We have constructed a regional tree ring cellulose oxygen isotope record using a total of five chronologies obtained from the Himalaya. Centennial changes in the regional tree ring record indicate a trend of weakened Indian summer monsoon (ISM) intensity since 1820. Decreasing ISM activity is also observed in various high-resolution ISM records from southwest China and Southeast Asia, and may be the result of reduced land–ocean thermal contrasts since 1820.
We have constructed a regional tree ring cellulose oxygen isotope record using a total of five...