Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon
By D. Yuan, Hai Cheng, R. Edwards, C. A. Dykoski, M. J. Kelly, Meiliang Zhang, Jiaming Qing, Yushi Lin, Yongjin Wang, Jiangying Wu and 3 more. Science, 2004
1,225 citations recorded by the source corpus.
Subfields: Anthropology, Atmospheric Science, Ecology
View Paper: https://www.semanticscholar.org/paper/894218eb964e1a05aee708331bde09d10c5444a7
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Citations in the corpus
- Revisiting long-range dependence in annual precipitation (2018, neutral): “…Air Cave; South Africa 24°S 29°E - -41 7925 1139 7 Holmgren et al. 2003 CWC1s Cold Water Cave; Iowa; USA 43°N 92°W - 10 7760 156 50 Denniston et al. 1999 CWC3L Cold Water Cave; Iowa; USA 43°N 92°W - 2017 7857 147 40 Denniston et al. 1999 D4 Dongge Cave; China 25°N 108°E - 14 7874 263 30 Yuan…”
- Influence of the intertropical convergence zone on the East Asian monsoon (2007, background): “The Huguang Maar sediments record the strength of the wintermonsoon in two independent ways: (1) the accumulation of wind-blown material, and (2) the redox-sensitive characteristics and total organic carbon (TOC) content of the sediment as a result of changes in wind stress and watercolumn mixing.”
- Species diversification and phylogeographical patterns of birds in response to the uplift of the Qinghai-Tibet Plateau and Quaternary glaciations (2014, background): “Palynological research indicates that a series of prolonged, mild interglacial periods led to a vegetation that is similar to the present-day flora of East Asia during MIS5 (0.11 to 0.071 Mya) (Li et al., 1996; Liu et al., 2002; Yuan et al., 2004).”