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(2009CB421407);the Knowledge Innovation Program of the Chinese Academy of Sciences(KZCX2-EW-QN202);the National Natural Science Foundation of China(40975050,41175072 and 40825008)
Considering the different uplifting time of different subregions of the Himalaya-Tibetan Plateau(TP),a series of numerical simulations have been conducted with the Community Atmosphere Model(CAM4) developed at the Nat...
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...
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)
The Middle Pliocene (ca 3.12–2.97 Ma) is a recent warm period in the Earth’s history. In many respects, the warmth of the Middle Pliocene is similar to the probable warm situation of the late 21st century predicted ...