supported by the Strategic Priority Research Program (Grant No.XDB03020602) of the Chinese Academy of Sciences;the National Natural Science Foundation of China (Grant Nos. 41175072, 41222034 and 41305073)
Studying the vegetation feedback during warm periods of the past can lead to better understanding of those in the future.In this study,we conducted several simulations to analyze vegetation feedback during the mid-Pli...
supported by the National Basic Research Program of China(2010CB950102 and 2009CB421406);the Strategic and Special Frontier Project of Science and Technology of the Chinese Academy of Sciences(XDA05080803)
One of the key uncertainties in future sea-level projections is attributed to the Greenland ice sheet(GrIS).Studying the response of the GrIS to climate changes during the past warm periods is helpful for understandin...
supported by the Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-EW-QN202);the National Natural Science Foundation of China(40975050 and41175072)
A global atmospheric general circulation model and an asynchronously coupled global atmosphere-biome model are used to simulate vegetation feedback at the mid-Pliocene approximately 3.3 to 3.0 million years ago.For th...
supported by the National Basic Research Program of China(973 Program,Grant No.2010CB950102);the Strategic and Special Frontier Project of Science and Technology of the Chinese Academy of Sciences(Grant No. XDA05080803);the National Natural Science Foundation of China(Grant No.40902054)
The mid-Pliocene, the most recent warm geological period, is thought to be indicative of the fate of the Earth's climate under global warming. Earlier evidence has suggested that permanent El Nio-like conditions exist...
supported by the National Basic Research Program of China(2009CB421406);the Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-YW-Q1-02);the National Natural Science Foundation of China(4090205 and 40975050)
In this study, the authors simulate the East Asian climate changes in the mid-Pliocene (~3.3 to 3.0 Ma BP) with the Community Atmosphere Model version 3.1 (CAM3.1) and compare the simulated East Asian monsoon with pa...
the Chinese Academy of Sciences under Grant Nos. KZCX2-YW-205 and KZCX3-SW-229;the National NaturalScience Foundation of China under Grant Nos. 40505017and 40775052.
A global atmospheric general circulation model has been used to perform eleven idealized numerical experiments, i.e., TP10, TP10, .., TP100, corresponding to different percentages of the Tibetan Plateau altitude. The ...