Articles | Volume 14, issue 4
https://doi.org/10.5194/cp-14-577-2018
© Author(s) 2018. 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-14-577-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Timescale dependence of the relationship between the East Asian summer monsoon strength and precipitation over eastern China in the last millennium
Jian Shi
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Nanjing University of Information Science and
Technology, Nanjing, 210044, China
Nansen-Zhu International Research Centre, Institute of Atmospheric
Physics, Chinese Academy of Sciences, Beijing, 100029, China
Huijun Wang
Collaborative Innovation Center on Forecast and Evaluation of
Meteorological Disasters, Nanjing University of Information Science and
Technology, Nanjing, 210044, China
Nansen-Zhu International Research Centre, Institute of Atmospheric
Physics, Chinese Academy of Sciences, Beijing, 100029, China
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Cited
15 citations as recorded by crossref.
- Separation of the Asian summer monsoon and local precipitation from stalagmite oxygen isotope records in Eastern China during the last millennium Z. Hu et al. 10.1016/j.quascirev.2023.108498
- Application of Artificial Intelligence Models for Aeolian Dust Prediction at Different Temporal Scales: A Case with Limited Climatic Data Y. Aryal 10.3390/ai3030041
- Assessment of PMIP3 model simulations of megadroughts over the eastern China during the last millennium Y. Qin et al. 10.1002/joc.6513
- A multi-model analysis of ‘Little Ice Age’ climate over China X. Zhou et al. 10.1177/0959683618824761
- Variability and Mechanisms of Megadroughts over Eastern China during the Last Millennium: A Model Study L. Ning et al. 10.3390/atmos10010007
- The Asian–Pacific oscillation over the past millennium in PMIP3 and PMIP4 K. Yang et al. 10.1016/j.quascirev.2022.107918
- Improvement of summer precipitation simulation in China by assimilating spring soil moisture over the Tibetan Plateau J. Shen et al. 10.1007/s00704-021-03840-5
- PDO influenced interdecadal summer precipitation change over East China in mid-18th century G. Chen et al. 10.1038/s41612-024-00666-6
- Divergent response of eastern China precipitation to the Pacific decadal oscillation during the last Interglacial N. Jiang et al. 10.1016/j.quascirev.2023.108344
- Solar modulation of hydroclimatic patterns in eastern China under influences of the Pacific Decadal Oscillation and Atlantic Multidecadal Oscillation L. Zhang et al. 10.1016/j.palaeo.2025.112796
- Quantifying the internal and external drivers of Southeast Asian rainfall extremes on decadal timescales S. Wang et al. 10.1007/s00382-024-07412-x
- Environmental Conditions of Floodplain Sedimentation during the Little Ice Age in the Deltaic Zone of the Tsukanovka River (Southwestern Primorye) V. Bazarova et al. 10.1134/S181971402570006X
- Stability of ENSO teleconnections during the last millennium in CESM X. Han et al. 10.1007/s00382-023-06878-5
- Decadal causes of the Wanli megadrought in northern China during the Ming Dynasty: Perspectives from the Pacific Ocean X. Li et al. 10.1016/j.gloplacha.2025.104824
- The Interdecadal Pacific Oscillation is responsible for the linkage of decadal changes in precipitation and moisture in arid central Asia and the humid Asian monsoon region during the last millennium H. Xu et al. 10.5194/cp-20-107-2024
15 citations as recorded by crossref.
- Separation of the Asian summer monsoon and local precipitation from stalagmite oxygen isotope records in Eastern China during the last millennium Z. Hu et al. 10.1016/j.quascirev.2023.108498
- Application of Artificial Intelligence Models for Aeolian Dust Prediction at Different Temporal Scales: A Case with Limited Climatic Data Y. Aryal 10.3390/ai3030041
- Assessment of PMIP3 model simulations of megadroughts over the eastern China during the last millennium Y. Qin et al. 10.1002/joc.6513
- A multi-model analysis of ‘Little Ice Age’ climate over China X. Zhou et al. 10.1177/0959683618824761
- Variability and Mechanisms of Megadroughts over Eastern China during the Last Millennium: A Model Study L. Ning et al. 10.3390/atmos10010007
- The Asian–Pacific oscillation over the past millennium in PMIP3 and PMIP4 K. Yang et al. 10.1016/j.quascirev.2022.107918
- Improvement of summer precipitation simulation in China by assimilating spring soil moisture over the Tibetan Plateau J. Shen et al. 10.1007/s00704-021-03840-5
- PDO influenced interdecadal summer precipitation change over East China in mid-18th century G. Chen et al. 10.1038/s41612-024-00666-6
- Divergent response of eastern China precipitation to the Pacific decadal oscillation during the last Interglacial N. Jiang et al. 10.1016/j.quascirev.2023.108344
- Solar modulation of hydroclimatic patterns in eastern China under influences of the Pacific Decadal Oscillation and Atlantic Multidecadal Oscillation L. Zhang et al. 10.1016/j.palaeo.2025.112796
- Quantifying the internal and external drivers of Southeast Asian rainfall extremes on decadal timescales S. Wang et al. 10.1007/s00382-024-07412-x
- Environmental Conditions of Floodplain Sedimentation during the Little Ice Age in the Deltaic Zone of the Tsukanovka River (Southwestern Primorye) V. Bazarova et al. 10.1134/S181971402570006X
- Stability of ENSO teleconnections during the last millennium in CESM X. Han et al. 10.1007/s00382-023-06878-5
- Decadal causes of the Wanli megadrought in northern China during the Ming Dynasty: Perspectives from the Pacific Ocean X. Li et al. 10.1016/j.gloplacha.2025.104824
- The Interdecadal Pacific Oscillation is responsible for the linkage of decadal changes in precipitation and moisture in arid central Asia and the humid Asian monsoon region during the last millennium H. Xu et al. 10.5194/cp-20-107-2024
Latest update: 03 Jul 2025
Short summary
The paleo-East Asian summer monsoon (EASM) is widely reconstructed by precipitation/humidity proxies over East Asia. However, based on numerical simulations over the last millennium, we find that the multi-decadal relationship between the EASM and precipitation over eastern China is non-stationary, which may be attributed to the internal variability of the climate system rather than the external forcings. In contrast, the centennial EASM–precipitation relationship is much more close and stable.
The paleo-East Asian summer monsoon (EASM) is widely reconstructed by precipitation/humidity...