This work was supported by the Chinese Academy of Sciences (grant XDA05080502, 132B61KYSB20130003), National Natural Science Foundation of China grants (41271229, 41420104008, 41290254), and partly supported by the US National Science Foundation (AGS-1405479 to J.C.H. Chiang, and EAR-1211299 to H. Cheng and R. L. Edwards)
; and funding from the European Union's Horizon 2020 Research and Innovation programme under the Marie Skłodowska-Curie grant agreement No 691037 (to S.F.M. Breitenbach). We thank W. Kong for providing the CAM5 simulations used in this study, and acknowledge high-performance computing support for the CAM5 from the Yellowstone cluster (ark:/85065/d7wd3xhc) provided by NCAR's Computational and Information Systems Laboratory, sponsored by the National Science Foundation.
State Key Lab of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China; Institute of Global Environmental Change, Xi'an Jiaotong University, Xi'an, China; Department of Geography and Berkeley Atmospheric Science Center, University of California, Berkeley, CA, United States; Department of Sediment- and Isotope Geology, Ruhr-Universität Bochum, Germany; Department of Earth Sciences, University of Minnesota, Minneapolis, MN, United States
Recommended Citation:
Cai Y.,Chiang J.C.H.,Breitenbach S.F.M.,et al. Holocene moisture changes in western China, Central Asia, inferred from stalagmites[J]. Quaternary Science Reviews,2017-01-01,158