25 citations as recorded by crossref.

1. East Asian summer precipitation in AWI‐CM3: Comparison with observations and CMIP6 models J. Shi et al. 10.1002/joc.8075
2. Response of the Asian summer monsoons to idealized precession and obliquity forcing in a set of GCMs J. Bosmans et al. 10.1016/j.quascirev.2018.03.025
3. Evaluation of CMIP5 palaeo-simulations to improve climate projections S. Harrison et al. 10.1038/nclimate2649
4. Strengthening of the East Asian winter monsoon during the mid-Holocene Z. Tian & D. Jiang 10.1177/0959683618777076
5. Revisiting last glacial maximum climate over China and East Asian monsoon using PMIP3 simulations Z. Tian & D. Jiang 10.1016/j.palaeo.2016.04.020
6. Drivers of reduced ENSO variability in mid-Holocene in a coupled model L. Chen et al. 10.1007/s00382-018-4496-5
7. Vegetation and Ocean Feedbacks on the Asian Climate Response to the Uplift of the Tibetan Plateau R. Zhang et al. 10.1029/2019JD030503
8. Simulated warm periods of climate over China during the last two millennia: The Sui‐Tang warm period versus the Song‐Yuan warm period Q. Yan et al. 10.1002/2014JD022941
9. The PMIP3 Simulated Climate Changes over Arid Central Asia during the Mid‐Holocene and Last Glacial Maximum H. XU et al. 10.1111/1755-6724.14542
10. Simulated Cycles of East Asian Temperature and Precipitation Over the Past 425 ka G. Dai et al. 10.1029/2022JD036802
11. Precipitation pattern of the mid-Holocene simulated by a high-resolution regional climate model E. Yu et al. 10.1007/s00376-013-3178-9
12. The role of dispersal limitation in the forest biome shifts of Europe in the last 18,000 years D. Zani et al. 10.1111/jbi.14836
13. Reproduction of climate for the mid-Holocene over the Korean Peninsula using a high-resolution numerical model S. Kim & J. Kim 10.1016/j.quaint.2014.04.052
14. Paleoclimate modeling in China: A review D. Jiang et al. 10.1007/s00376-014-0002-0
15. Mechanisms of Reduced Mid‐Holocene Precipitation in Arid Central Asia as Simulated by PMIP3/4 Models T. Wang et al. 10.1029/2021JD036153
16. Global and regional evaluation of a global model simulated AODs with AERONET and MODIS observations V. Sheel et al. 10.1002/joc.5367
17. Northern Hemisphere vegetation change drives a Holocene thermal maximum A. Thompson et al. 10.1126/sciadv.abj6535
18. New Data on Deuterium Excess Values of Glacial Ice in Kamchatka Peninsula Y. Chizhova et al. 10.1134/S1028334X24602190
19. The sensitivity of Northern Hemisphere ice sheets to atmospheric forcing during the last glacial cycle using PMIP3 models L. NIU et al. 10.1017/jog.2019.42
20. Shortwave forcing and feedbacks in Last Glacial Maximum and Mid-Holocene PMIP3 simulations P. Braconnot & M. Kageyama 10.1098/rsta.2014.0424
21. Role of the tropical Indian Ocean in orbitally induced mid-Holocene precipitation variation in northwest China J. Yang et al. 10.1016/j.quascirev.2023.108285
22. Mid-Holocene global monsoon area and precipitation from PMIP simulations D. Jiang et al. 10.1007/s00382-014-2175-8
23. Northwestward shift of the northern boundary of the East Asian summer monsoon during the mid-Holocene caused by orbital forcing and vegetation feedbacks J. Chen et al. 10.1016/j.quascirev.2021.107136
24. Glacial Inception in Marine Isotope Stage 19: An Orbital Analog for a Natural Holocene Climate S. Vavrus et al. 10.1038/s41598-018-28419-5
25. East–west contrast of Northeast Asian summer precipitation during the Holocene X. Zhang et al. 10.1016/j.gloplacha.2018.08.018