39 citations as recorded by crossref.

1. Distinct responses of East Asian and Indian summer monsoons to astronomical insolation during Marine Isotope Stages 5c and 5e Z. Shi et al. 10.1016/j.palaeo.2017.12.029
2. Asynchronous variation in the East Asian winter monsoon during the Holocene X. Zhang et al. 10.1002/2014JD022585
3. Initial Expansion of C4 Vegetation in Australia During the Late Pliocene J. Andrae et al. 10.1029/2018GL077833
4. Spatial variation of East Asian winter monsoon evolution between northern and southern China since the last glacial maximum Q. Li et al. 10.1017/qua.2020.101
5. Multiscale monsoon variability during the last two climatic cycles revealed by spectral signals in Chinese loess and speleothem records Y. Li et al. 10.5194/cp-11-1067-2015
6. Mechanisms rectifying the annual mean response of tropical Atlantic rainfall to precessional forcing M. Tigchelaar & A. Timmermann 10.1007/s00382-015-2835-3
7. A review of orbital-scale monsoon variability and dynamics in East Asia during the Quaternary Y. Sun et al. 10.1016/j.quascirev.2022.107593
8. Anti-phased response of northern and southern East Asian summer precipitation to ENSO modulation of orbital forcing Z. Shi et al. 10.1016/j.quascirev.2012.02.019
9. A Holocene East Asian winter monsoon record at the southern edge of the Gobi Desert and its comparison with a transient simulation Y. Li & C. Morrill 10.1007/s00382-014-2372-5
10. Obliquity-driven changes in East Asian seasonality C. Wu & P. Tsai 10.1016/j.gloplacha.2020.103161
11. Indo‐Pacific Hydroclimate in Response to Changes of the Intertropical Convergence Zone: Discrepancy on Precession and Obliquity Bands Over the Last 410 kyr P. Zhang et al. 10.1029/2019JD032125
12. Differences in Late Quaternary primary productivity between the western tropical Pacific and the South China Sea: Evidence from coccoliths X. Su et al. 10.1016/j.dsr2.2015.07.008
13. Orbital‐ to millennial‐scale variation of the speleothem δ18O record during Marine Isotope Stages 5 to 3 on the southeast Chinese Loess Plateau and its climatic and environmental implications Y. CAI et al. 10.1002/jqs.3489
14. Precession control of interglacial winter monsoon intensity over tropical East Asia E. Huang et al. 10.1016/j.gloplacha.2023.104247
15. Geomorphological and palaeoclimate dynamics recorded by the formation of aeolian archives on the Tibetan Plateau G. Stauch 10.1016/j.earscirev.2015.08.009
16. Responses of global monsoon and seasonal cycle of precipitation to precession and obliquity forcing Z. Ding et al. 10.1007/s00382-021-05663-6
17. Response of summer extreme precipitation over East Asia during the mid-Holocene versus future global warming X. Ren et al. 10.1016/j.gloplacha.2020.103398
18. Multi-decadal periods of enhanced aeolian activity on the north-eastern Tibet Plateau during the last 2ka G. Stauch 10.1016/j.quascirev.2016.07.027
19. Palaeoclimatic records of the loess/palaeosol sequences of the Chinese Loess Plateau B. Maher 10.1016/j.quascirev.2016.08.004
20. Milankovitch theory and monsoon H. Cheng et al. 10.1016/j.xinn.2022.100338
21. Obliquity pacing of the western Pacific Intertropical Convergence Zone over the past 282,000 years Y. Liu et al. 10.1038/ncomms10018
22. Astronomical and glacial forcing of East Asian summer monsoon variability Y. Sun et al. 10.1016/j.quascirev.2015.03.009
23. Quaternary rainfall variability is governed by insolation in northern China and ice-sheet forcing in the South D. Zhao et al. 10.1038/s43247-022-00670-9
24. Aeolian activity in arid central Asia during the past 40000 years inferred from Lake Ailike, Xinjiang Y. Chen & X. Liu 10.1016/j.catena.2023.107106
25. Role of eccentricity in early Holocene African and Asian summer monsoons C. Wu et al. 10.1038/s41598-021-03525-z
26. Strengthened East Asian Winter Monsoon Regulated by Insolation and Arctic Sea Ice Since the Middle Holocene P. Zhou et al. 10.1029/2023GL105440
27. Registration of Precession Signal in the Last Interglacial Paleosol (S1) on the Chinese Loess Plateau L. Ma et al. 10.1002/2017GC006964
28. Relative influence of precession and obliquity in the early Holocene: Topographic modulation of subtropical seasonality during the Asian summer monsoon C. Wu et al. 10.1016/j.quascirev.2018.05.021
29. High-sedimentation-rate loess records: A new window into understanding orbital- and millennial-scale monsoon variability Y. Sun et al. 10.1016/j.earscirev.2021.103731
30. 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
31. Orbitally controls of climate recorded in a series of thin-multiple-layers coal seams in marine–continent transition environment during late Eocene K. Zhao et al. 10.1016/j.palaeo.2022.111233
32. Response of Asian summer monsoon duration to orbital forcing under glacial and interglacial conditions: Implication for precipitation variability in geological records Z. Shi 10.1016/j.quascirev.2016.03.008
33. A Modeling Study of the Tripole Pattern of East China Precipitation Over the Past 425 ka G. Dai et al. 10.1029/2020JD033513
34. Hydrological and vegetation shifts in the Wallacean region of central Indonesia since the Last Glacial Maximum S. Wicaksono et al. 10.1016/j.quascirev.2016.12.006
35. Contrasting responses of summer precipitation to orbital forcing in Japan and China over the past 450 kyr T. Matsushita et al. 10.5194/cp-20-2017-2024
36. Late Quaternary coccolith records in the South China Sea and East Asian monsoon dynamics X. Su et al. 10.1016/j.gloplacha.2013.08.016
37. Sea-level variability over five glacial cycles K. Grant et al. 10.1038/ncomms6076
38. Orbital-scale Asian summer monsoon variations: Paradox and exploration H. Cheng et al. 10.1007/s11430-020-9720-y
39. Loess‐Like Dust Appearance at 40 Ma in Central China N. Meijer et al. 10.1029/2020PA003993