Qaidam Basin
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- Responses of Aeolian Desertification to a Range of Climate Scenarios In
- Survival of the Qaidam Mega-Lake System Under Mid-Pliocene Climates and Its Restoration Under Future Climates
- Aeolian-Fluvial Interactions Stabilize Desert in the Qaidam Basin, Qinghai-Tibetan Plateau
- Applicability Analysis of Vegetation Condition and Dryness for Sand and Dust Storm (SDS) Risk Reduction in SDS Source and Receptor Region
- Aridification Signatures from Fossil Pollen Indicate a Drying Climate In
- Late Quaternary Qaidam Lake Histories and Implications for an MIS 3 ‘‘Greatest Lakes’’ Period in Northwest China
- Soil Moisture and Soluble Salt Content Dominate Changes in Foliar Δ13c and Δ15n of Desert Communities in the Qaidam Basin, Qinghai-Tibetan Plateau
- The Spatial Variation of Asian Dust and Marine Aerosol Contributions to Glaciochemical Signals in Central Asia
- China's Deserts
- Climatic and Tectonic Evolution in the North Qaidam Since the Cenozoic: Evidence from Sedimentology and Mineralogy
- Monitoring 40-Year Lake Area Changes of the Qaidam Basin, Tibetan Plateau, Using Landsat Time Series
- Eolian Sediments • Eolian Environments Include Those Where Wind Is the Major Agent of Sediment Deposition
- Wind As the Primary Driver of Erosion in the Qaidam Basin, China
- Eolian Cannibalism: Reworked Loess and Fluvial Sediment As the Main Sources of the Chinese Loess Plateau
- Supplement of Responses of Aeolian Desertification to a Range of Climate
- The Qaidam Basin, Tibetan Plateau (NW China)
- Sediment History Mirrors Pleistocene Aridification in the Gobi Desert
- Qaidam Basin, Ne Tibetan Plateau: a New Unique Mars Analogue Site for Its Wet Past and Dry Environemnt Today L