Although recent studies have shown that desertification in northwestern china has generally improved, that in the qaidam basin has intensified (wang et al., 2018). The qaidam basin, located at the eastern edge of arid central asia, is a key region for understanding hydroclimate changes in a warming climate. The best time to visit is from late.
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The qaidam basin is the largest cenozoic sedimentary basin on the tibetan plateau, situated in the northeastern part of the plateau within qinghai province, northwestern china.
The qaidam basin is the northeastern section of the plateau of tibet, occupying the northwestern part of qinghai province, western china.
The basin covers an area of approximately 120,000 km 2. The qaidam, tsaidam, or chaidamu basin is a hyperarid basin that occupies a large part of haixi prefecture in qinghai province, china. Qaidam basin is china’s highest and most evaporative inland basin situated in the border area of the provinces of qinghai, gansu and the autonomous region of xinjiang. The basin lies in a crescent.
For adventure seekers, the qaidam basin offers a rare opportunity to traverse terrain that resembles another planet without leaving the chinese mainland. Regional drying could intensify dust.
