This article pointed out that the distributing pattern of Chinese desert and desertification is V shapesd, and the Qinghai-Tibet plateau uplift may be the main factor to this pattern.

Problems and suggestions in research on aeolian desertification in Tibetan Plateau

The results from remote sensor monitoring and field survey show that aeolian desertification process in the study area can be distributed into two stages: the developing stage from late 1980s to 2000,and the reversing stage form 2000 to 2006.

The aeolian desertification is a land degradation characterized by wind erosion mainly resulted from the excessive human activities in arid, semiarid and part of sub-humid regions in Northern Chian.

Study on the control of land desertification and its project construction in Tibet autonomous region;

The reclamation of land desertification in Shiyang river basin mainly depends on governments and experts in the last 50 years.

To prevent and combat land desertification in Bashang has very important realistic and historical significance.

A new approach to desertification process of sandy lands in east of the Yellow River in Ningxia;

Ecological Restoration Measures for the Desertification of Both Sides of National Highway G304 in the Hinterland of Inner Mongolia Kerqin Sandy Land;

Threshold friction velocity of various land cover types with strong desertification on north of Yinshan mountain in Inner Mongolia;

Studies on Desertization Driving Forces Mechanism in Mu Us Region;

94 km 2 of desertization land in mining area have been controlled by setting up sand barrier in moving sandy land and planting windbreak forest of arbor and shrub, which has preliminarily restricted the desertization land in development district.

Here is also the eastern fringe of desertization land in P.