This work was jointly supported by the National Key Basic Research Project“The Process of Desertification and Its Control in Northern China”(Grant No.G2000048701);the Knowledge Innovation Fund of the Chinese Academy of Sciences(Grant No.KZCXl-10-02);the National Natural Science Foundation of China(Grant Nos.40201011,40272123 and 90102005)
The paleoclimate data recovered from ice cores, tree rings and lake sediments indicate regional features of climatic change on the Tibetan Plateau (TP) during the last 2000 years. The composite temperature reconstruct...