The strong signals of climatic shift to warm humid pattern have been appearing in the western part of Chinese Tianshan Mountains and neighborhood regions including Northern Xinjiang since 1987.

Planktonic foraminifera results from ODP Site 1144 in the northern South China Sea indicate that the Mid-Pleistocene climate transition is characterized by high-frequency changes on the millennial scale.

The environmental change and climate transition in Jilantai area since 22 ka BP are responses to the global paleoclimate change,which have great significance in researches of salt resources formation events and the sustainable development of regional economy.

Late Pleistocene epoch lake facies sedimentary characteristics, paleoplant-cover and definition of climate transformation since 17.4 ka B.P.Tanggula area, Qinghai;

With the global warming,there has been a climate transformation of xinjiang,and the paper discusses the trend and its forms and its impacts of the global meterological change

The data of hydrology and meteorology for the recent 40 years were used to analyze the influence of climate warming during 1980s～1990s and human activity on the relationship between precipitation and runoff for middle\|small rivers of northern Xinjiang.