14 citations as recorded by crossref.

1. 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
2. Application of Artificial Intelligence Models for Aeolian Dust Prediction at Different Temporal Scales: A Case with Limited Climatic Data Y. Aryal 10.3390/ai3030041
3. Assessment of PMIP3 model simulations of megadroughts over the eastern China during the last millennium Y. Qin et al. 10.1002/joc.6513
4. A multi-model analysis of ‘Little Ice Age’ climate over China X. Zhou et al. 10.1177/0959683618824761
5. Variability and Mechanisms of Megadroughts over Eastern China during the Last Millennium: A Model Study L. Ning et al. 10.3390/atmos10010007
6. The Asian–Pacific oscillation over the past millennium in PMIP3 and PMIP4 K. Yang et al. 10.1016/j.quascirev.2022.107918
7. 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
8. PDO influenced interdecadal summer precipitation change over East China in mid-18th century G. Chen et al. 10.1038/s41612-024-00666-6
9. 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
10. 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
11. Quantifying the internal and external drivers of Southeast Asian rainfall extremes on decadal timescales S. Wang et al. 10.1007/s00382-024-07412-x
12. Stability of ENSO teleconnections during the last millennium in CESM X. Han et al. 10.1007/s00382-023-06878-5
13. 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
14. 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