Articles | Volume 17, issue 6
https://doi.org/10.5194/cp-17-2381-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-17-2381-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
A 406-year non-growing-season precipitation reconstruction in the southeastern Tibetan Plateau
Maierdang Keyimu
State Key Laboratory of Urban and Regional Ecology, Research Center
for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
Xinjiang Key Laboratory of Desert Plant Roots Ecology and Vegetation Restoration, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
Cele National Station of Observation and Research for Desert-Grassland Ecosystems, Cele 848300, China
State Key Laboratory of Urban and Regional Ecology, Research Center
for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
Bojie Fu
State Key Laboratory of Urban and Regional Ecology, Research Center
for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
Guohua Liu
State Key Laboratory of Urban and Regional Ecology, Research Center
for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
Fanjiang Zeng
State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
Xinjiang Key Laboratory of Desert Plant Roots Ecology and Vegetation Restoration, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
Cele National Station of Observation and Research for Desert-Grassland Ecosystems, Cele 848300, China
Weiliang Chen
State Key Laboratory of Urban and Regional Ecology, Research Center
for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
Zexin Fan
Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla 666303, China
Keyan Fang
Key Laboratory of Humid Subtropical Eco-Geographical Process (Ministry of Education), College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China
Xiuchen Wu
State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing 100875, China
Xiaochun Wang
College of Forestry, Northeast Forestry University, Harbin 150040, China
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Cited
9 citations as recorded by crossref.
- Radial growth response of Euphrates poplar to thermo-hydroclimatic changes in a desert oasis ecotone Y. Qi et al. 10.1016/j.ecofro.2024.09.001
- Strong coupling between soil moisture and temperature intensifies warming and humidification on the Tibetan Plateau: Evidence from 200-year tree ring records M. Hu et al. 10.1016/j.palaeo.2024.112206
- A 217-year precipitation reconstruction in the Habahe area, Xinjiang, Northeast China H. Zhang et al. 10.1007/s11676-024-01733-7
- Assessing Sources and Distribution of Heavy Metals in Environmental Media of the Tibetan Plateau: A Critical Review W. Wang et al. 10.3389/fenvs.2022.874635
- Radial growth response of Quercus liaotungensis to climate change–a case study on the central Loess Plateau, China M. Keyimu et al. 10.1007/s00468-022-02329-6
- The Radial Growth of Juniperus squamata Showed Sharp Increase in Response to Climate Warming on the Three-River Headwaters Region of Tibetan Plateau since the Early 21st Century G. Zhao et al. 10.3390/f14061219
- Drought variations in the southeastern Tibetan Plateau region since 1704 and their link to the Atlantic Multidecadal Oscillation W. Tang et al. 10.1016/j.palaeo.2023.111813
- Variability of the Early Summer Temperature in the Southeastern Tibetan Plateau in Recent Centuries and the Linkage to the Indian Ocean Basin Mode J. Li et al. 10.2113/2022/9648384
- The recent high occurrence of spring atmospheric droughts over central Hengduan Mountains is unprecedented in 669-year tree-ring records L. Cui et al. 10.1016/j.palaeo.2024.112318
9 citations as recorded by crossref.
- Radial growth response of Euphrates poplar to thermo-hydroclimatic changes in a desert oasis ecotone Y. Qi et al. 10.1016/j.ecofro.2024.09.001
- Strong coupling between soil moisture and temperature intensifies warming and humidification on the Tibetan Plateau: Evidence from 200-year tree ring records M. Hu et al. 10.1016/j.palaeo.2024.112206
- A 217-year precipitation reconstruction in the Habahe area, Xinjiang, Northeast China H. Zhang et al. 10.1007/s11676-024-01733-7
- Assessing Sources and Distribution of Heavy Metals in Environmental Media of the Tibetan Plateau: A Critical Review W. Wang et al. 10.3389/fenvs.2022.874635
- Radial growth response of Quercus liaotungensis to climate change–a case study on the central Loess Plateau, China M. Keyimu et al. 10.1007/s00468-022-02329-6
- The Radial Growth of Juniperus squamata Showed Sharp Increase in Response to Climate Warming on the Three-River Headwaters Region of Tibetan Plateau since the Early 21st Century G. Zhao et al. 10.3390/f14061219
- Drought variations in the southeastern Tibetan Plateau region since 1704 and their link to the Atlantic Multidecadal Oscillation W. Tang et al. 10.1016/j.palaeo.2023.111813
- Variability of the Early Summer Temperature in the Southeastern Tibetan Plateau in Recent Centuries and the Linkage to the Indian Ocean Basin Mode J. Li et al. 10.2113/2022/9648384
- The recent high occurrence of spring atmospheric droughts over central Hengduan Mountains is unprecedented in 669-year tree-ring records L. Cui et al. 10.1016/j.palaeo.2024.112318
Latest update: 20 Nov 2024
Short summary
We created a residual tree-ring width chronology and reconstructed non-growth-season precipitation (NGSP) over the period spanning 1600–2005 in the southeastern Tibetan Plateau (SETP), China. Reconstruction model verification as well as similar variations of NGSP reconstruction and Palmer Drought Severity Index reconstructions from the surrounding region indicate the reliability of the present reconstruction. Our reconstruction is representative of NGSP variability of a large region in the SETP.
We created a residual tree-ring width chronology and reconstructed non-growth-season...