Alexandersson H. 1986. A homogeneity test applied precipitation data. International Journal of Climatology, 6: 661–675.
Azorin-Molina C, Vicente-Serrano S M, Mcvicar T R et al. 2014 Homogenization and assessment of observed near-surface wind speed trends over Spain and Portugal, 1961–2011. Journal of Climate, 27(10): 3692–3712.
Bagnold R A. 1941. The Physics of Blown Sand and Desert Dunes. Methuen, London.
Cui X J, Dong Z B, Sun H, et al. 2017. Spatial and temporal variation of the near-surface wind environment in the dune fields of northern China. International Journal of Climatology, 38(5): 2333–2351.
Dong Y X, Li S, Dong G R. 1999. Present status and cause of land desertification in the Yarlung Zangbo River basin. Chinese Geographical Science, 9(3): 36–43.
Dong Z.B. 2017. Tibetan Plateau Atlas of Aeolian Geomorphology. Xi’an, Xi’an Map Press.
Dong Z B, Hu G Y, Qian G Q, et al. 2017. High-altitude aeolian research on the Tibetan Plateau. Reviews of Geophysics, 55(6): 864–901.
Dong Z B, Li Z S. 1998. Wind erodibility of aeolian sand as influenced by grain size parameters. Journal of Soil Erosion and Soil and Water Conservation, 4(4): 1–5 (in Chinese).
Dong Z B, Su Z Z, Qian G Q, et al. 2011. Aeolian Geomorphology of the Kumtagh Desert. Beijing: Science Press.
Fang X M, Han Y X, Ma J H, et al. 2004. Dust storms and loess accumulation on the Tibetan Plateau: a case study of dust event on 4 March 2003 in Lhasa. Chinese Science Bulletin, 49(9): 953–960.
Folk R L, Ward W C. 1957. Brazos River bar: a study in the significance of grain size parameters. Journal of Sedimentary Research, 27(1): 3–26.
Fryberger S G, Dean G. 1979. Dune forms and wind regime. In: Mckee E D (ed). A Study of Global Sand Seas. Washington: US Government Printing Office.
Guo H, Xu M, Hu Q. 2011. Changes in near-surface wind speed in China: 1969–2015. International Journal of Climatology, 31(3): 349–358.
Han Q J, Qu J, Dong Z B, et al. 2015. Air density effects on aeolian sand movement: implications for sediment transport and sand control in regions with extreme altitudes or temperatures. Sedimentology, 62(4): 1024–1038.
Han Q J, Qu J, Dong Z B. et al. 2014. The effect of air density on sand transport structures and the Adobe Abrasion Profile: a field wind-tunnel experiment over a wide range of altitude. Boundary-Layer Meteorology, 150(2): 299–317.
Han Y X, Fang X M, Kang S C, et al. 2008. Shifts of dust source regions over central Asia and the Tibetan Plateau: connections with the Arctic oscillation and the westerly jet. Atmospheric Environment, 42(10): 2358–2368.
Han Y X, Fang X M, Zhao T L, et al. 2009. Suppression of precipitation by dust particles originated in the Tibetan Plateau. Atmospheric Environment, 43(3): 568–574.
He D H, Tian H, Deng W T, 2012. Comparative analysis of the effects of different methods in homogenetiy test on annual wind speed. Transactions of Atmospheric Sciences, 35(3): 342–349 (in Chinese).
Jiang Y Y, E CY, Hou G L, et al. 2015. Temporal and spatial distribution of surface wind in the region of northeast Tibetan Plateau. Journal of Qinghai Normal University (Natural Science), 31(1): 62–70 (in Chinese).
Kim J C, Paik K. 2015. Recent recovery of surface wind speed after decadal decrease: a focus on South Korea. Climate Dynamics, 45: 1699–1712.
Li C, Dong Z B, Yin SY, et al. 2019. Influence of salinity and moisture on the threshold shear velocity of saline sand in the Qarhan Desert, Qaidam Basin of China: a wind tunnel experiment. Journal of Arid Land, 11(5): 674–684.
Li H D, Fang Y, Shen W S, et al. 2011. Spatial distribution and evolution of aeolian sandy land in the areas around Shigatse Peace Airport of Tibet, China since 1975. Journal of Natural Resources, 26(7): 1148–1155 (in Chinese).
Li S, Dong G R, Shen JY, et al. 1999. Formation mechanism and development pattern of aeolian sand landform in Yarlung Zangbo River valley. Science in China (Series D), 42(3): 273–284.
Li S, Wang Y, Ha S, et al. 1997. Classification and development of aeolian sand landforms in the Yurlung Zangbo Valley. Journal of Desert Research, 17(4): 342–350 (in Chinese).
Li S, Yan P, Gao S Y, et al. 2004. Dynamic changes and developmental trends of the land desertification in Tibetan Plateau over the past 10 years. Advances in Earth Science, 19(1): 63–70 (in Chinese).
Ling Z Y, Yang S L, Wang X, et al. 2020. Spatial-temporal differentiation of eolian sediments in the Yarlung Tsangpo catchment, Tibetan Plateau, and response to global climate change since the Last Glaciation. Geomorphology, 357: 107104.
Liu H, Li X Y, Xiao J H, et al. 2019. Variations of wind erosion climatic erosivity in the Yarlung Zangbo River basin during 1961–2015. Scientia Geographica Sinica, 39(4): 688–695 (in Chinese).
Liu X N. 2000. The homogeity test on mean annual wind speed over China. Quarterly Journal of Applied Meteorology, 11(1): 28–34 (in Chinese).
Liu Y, Wang Y S, Shen T. 2019. Spatial distribution and formation mechanism of aeolian sand in the middle reaches of the Yarlung Zangbo River. Journal of Mountain Science, 16(9): 1987–2000.
McVicar T R, Roderick M L, Donohue R J, et al. 2012. Global review and synthesis of trends in observed terrestrial near-surface wind speeds: implications for evaporation. Journal of Hydrology, 416–417: 182–205.
Sahu R K. 1964. Depositional mechanisms from the size analysis of clastic sediments. Journal of Sediment Research, 34(1): 73–83.
Shen W S, Li H D, Sun M, et al. 2012. Dynamics of aeolian sandy land in the Yarlung Zangbo River basin of Tibet, China from 1975 to 2008. Global and Planetary Change, 86–87: 37–44.
Shi P J, Chen Y Q, Zhang AY, et al. 2019. Factors contribution to oxygen concentration in Qinghai-Tibetan Plateau. Chinese Science Bulletin, 64(7): 715–724 (in Chinese).
Sun J M, Li S H, Muhs D R, et al. 2007. Loess sedimentation in Tibet: provenance, processes, and link with Quaternary glaciations. Quaternary Science Reviews, 26: 2265–2280.
Sun M, Shen W S, Li H D, et al. 2010. Traits and dynamic changes of the aeolian sandy land in the source region of the Yarlung Zangbo River in Tibet. Journal of Natural Resources, 25(7): 1163–1171 (in Chinese).
Swet N, Elperin T, Kok J F, et al. 2019. Can active sands generate dust particles by wind-induced processes? Earth and Planetary Science Letters, 506: 371–380.
Vautard R, Cattiaux J, Yiou P, et al. 2010. Northern Hemisphere atmospheric stilling partly attributed to an increase in surface roughness. Nature Geoscience, 3(11): 756–761.
Wang X M, Lang L L, Yan P, et al. 2016. Aeolian processes and their effect on sandy desertification of the Qinghai-Tibet Plateau: a wind tunnel experiment. Soil and Tillage Research, 158: 67–75.
Wu J, Zha J L, Zhao D M, 2016. Estimating the impact of the changes in land use and cover on the surface wind speed over the East China Plain during during the period 1980–2011. Climate Dynamics, 46: 847–863.
Wu J, Zha J L, Zhao D M, et al. 2018a. Changes of wind speed at different heights over eastern China during 1980–2011. International Journal of Climatology, 38: 4476–4495.
Wu J, Zha J L, Zhao D M, et al. 2018b. Changes in terrestrial near-surface wind speed and their possible causes: an overview. Climate Dynamics, 51: 2039–2078.
Xu C, Ma Y M, Yang K, et al. 2018. Tibetan Plateau impacts on global dust transport in the upper troposphere. Journal of Climate, 31(12): 4745–4756.
Xu M, Chang C, Fu C B, et al. 2006. Steady decline of east Asian monsoon winds, 1969–2000: Evidence from direct ground measurements of wind speed. Journal of Geophysical Research, 111: D24111. doi: https://doi.org/10.1029/2006JD007337.
Yang J H, Dong Z B, Liu Z Y, et al. 2019a. Migration of barchan dunes in the western Quruq Desert, northwestern China. Earth Surface Processes and Landforms, 44(10): 2016–2029.
Yang J H, Xia D S, Gao F Y, et al. 2020. Aeolian deposits in the Yarlung Zangbo River basin, southern Tibetan Plateau: A brief review. Advances in Earth Science, 35(8): 863–877 (in Chinese).
Yang Y C, Gao D Y, Li B S. 1989. Study on the moisture passage on the lower reaches of the Yarlung Zangbo River. Science in China (Series D), 32(5): 580–593.
Yang Y Y, Liu L Y, Li X Y, et al. 2019b. Aerodynamic grain-size distribution of blown sand. Sedimentology, 66: 590–603.
Yuan L, Shen W S, Li H D, et al. 2010. Evolution and causes of aeolian desertification of the middle reaches of Yarlung Zangbo River, China. Journal of Ecology and Rural Environment, 26(4): 301–305 (in Chinese).
Zeng Z Z, Ziegler A D, Searchinger T, et al. 2019. A reversal in global terrestrial stilling and its implications for wind energy production. Nature Climate Change, 9: 979–985.
Zha J L, Wu J. 2017. Effects of land use and cover change on the near-surface wind speed over China in the last 30 years. Progress in Physical Geography, 41(1): 46–67.
Zha J L, Wu J, Zhao D M. 2016. Changes of probabilities in different wind grades induced by land use and cover change in Eastern China Plain during 1980–2011. Atmospheric Science Letters: 17, 264–269.
Zha J L, Wu J, Zhao D M, et al. 2019. A possible recovery of the near-surface wind speed in Eastern China during winter after 2000 and the potential causes. Theoretical and Applied Climatology, 136: 119–134.
Zhang Z C, Dong Z B. 2015. Grain size characteristics in the Hexi Corridor Desert. Aeolian Research, 18: 55–67.
Zhang Z C, Dong Z B, Hu G Y, et al. 2018a. Migration and morphology of asymmetric barchans in the central Hexi Corridor of northwest China. Geosciences, 8(6): 204.
Zhang Z C, Dong Z B, Li C X. 2015. Wind regime and sand transport in China’s Badain Jaran Desert. Aeolian Research, 17: 1–13.
Zhang Z C, Dong Z B, Qian G Q, et al. 2018b. Formation and development of dunes in the northern Qarhan Desert, central Qaidam Basin, China. Geological Journal, 53: 1123–1134.
Zhang Z T, Wang K C. 2020. Stilling and recovery of the surface wind speed based on observation, reanalysis, and geostrophic wind theory over China from 1960 to 2017. Journal of Cliamte, 33: 3989–4008.
Zhou N, Zhang C L, Liu Y G. 2011. Variation of grain size on surface of barchans in Mainling Great valley, Yarlung Zangbo River. Scientia Geographica Sinica, 31(8): 958–963 (in Chinese).
Zou X Y, Li S, Zhang C L, et al. 2002. Desertification and control plan in the Tibet Autonomous Region of China. Journal of Arid Environments, 51: 183–198.