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...