Spatial distribution of sand dunes and their relationship with fluvial systems on the southern margin of the Taklimakan Desert, China

References

• Al-Masrahy MA, Mountney NP. 2015. A classification scheme for fluvial-aeolian system interaction in desert-margin settings. Aeolian Res. 17:67–88.
   Google Scholar
• Barchyn TE, Hugenholtz CH. 2012. A process-based hypothesis for the barchans-parabolic transformation and implications for dune activity modelling. Earth Surf Process Landforms. 37(13):1456–1462.
   Google Scholar
• Belnap J, Munson SM, Field JP. 2011. Aeolian and fluvial processes in dryland regions: the need for integrated studies. Ecohydrology. 4(5):615–622.
   Google Scholar
• Bourke MC, Lancaster N, Fenton LK, Parteli EJR, Zimbelman JR, Radebaugh J. 2010. Extraterrestrial dunes: an introduction to the special issue on planetary dune systems. Geomorphology. 121(1–2):1–14.
   Google Scholar
• Bullard JE, Livingstone I. 2002. Interactions between aeolian and fluvial systems in dry land. Environ Area. 34(1):8–16.
   Google Scholar
• Bullard JE, McTainsh GH. 2003. Aeolian-fluvial interactions in dryland environments: examples, concepts and Australia case study. Prog Phys Geogr. 27(4):471–501.
   Google Scholar
• Courrech Du Pont S, Narteau C, Gao X. 2014. Two modes for dune orientation. Geology. 42(9):743–746.
   Google Scholar
• Dee DP, Uppala SM, Simmons AJ, Berrisford P, Poli P, Kobayashi S, Andrae U, Balmaseda M, Balsamo G, Bauer P, et al. 2011. The ERA-interim reanalysis: configuration and performance of the data assimilation system. QJR Meteorol Soc. 137(656):553–597.
   Google Scholar
• Dong ZB, Qian GQ, Luo WY, Zhang ZC, Xiao SC, Zhao AG. 2009. Geomorphological hierarchies for complex mega-dunes and their implications for mega-dune evolution in the Badain Jaran Desert. Geomorphology. 106(3–4):180–185.
   Google Scholar
• Dong ZB, Wei ZH, Qian GQ, Zhang ZC, Luo WY, Hu GY. 2010. “Raked” linear dunes in the Kumtagh Desert, China. Geomorphology. 123(1–2):122–128.
   Google Scholar
• El-Baz F, Maingue M, Robinson C. 2000. Fluvio-aeolian dynamics in the north-eastern Sahara: the relationship between fluvial/aeolian systems and ground-water concentration. J Arid Environ. 44(2):173–183.
   Google Scholar
• Fedele JJ, Paola C. 2007. Similarity solutions for fluvial sediment fining by selective deposition. J Geophys Res. 112(F2):F02038.
   Google Scholar
• Fenton LK, Michaels TI, Beyer RA. 2014. Inverse maximum gross bedform-normal transport 1: how to determine a dune-constructing wind regime using only imagery. Icarus. 230(4):5–14.
   Google Scholar
• Ferguson R, Hoey T, Wathen S, Werritty A. 1996. Field evidence for rapid downstream fining of river gravels through selective transport. Geology. 24(2):179–182.
   Google Scholar
• Field JP, Breshears DD, Whicker JJ. 2009. Toward a more holistic perspective of soil erosion: why aeolian research needs to explicitly consider fluvial processes and interactions. Aeolian Res. 1(1–2):9–17.
   Google Scholar
• Gao X, Narteau C, Rozier O, Courrech Du Pont S. 2015. Phase diagram of dune shape and orientation depending on sand availability. Sci Rep. 5:14677.
   Google Scholar
• Gao X, Narteau C, Rozier O. 2016. Controls on and effects of armoring and vertical sorting in aeolian dune fields: a numerical simulation study. Geophys Res Lett. 43(6):2614–2622.
   Google Scholar
• Gu X, Zhang Q, Singh VP, Chen YD, Shi P. 2016. Temporal clustering of floods and impacts of climate indices in the Tarim River Basin, China. Global Planet Change. 147:12–24.
   Google Scholar
• Gutman G, Ignatov A. 1998. The derivation of the green vegetation fraction from NOAA/AVHRR data for use in numerical weather prediction models. Int J Remote Sens. 19(8):1533–1543.
   Google Scholar
• Heller PL, Paola C. 1992. The large-scale dynamics of grain-size variation in alluvial basins, 2: application to syntectonic conglomerate. Basin Res. 4(2):91–102.
   Google Scholar
• Hunter RE, Richmond BM, Alpha TR. 1983. Storm-controlled oblique dunes of the Oregon coast. Geol Soc America Bull. 94(12):1450–1465.
   Google Scholar
• Iversen JD, Rasmussen KR. 1999. The effect of wind speed and bed slope on sand transport. Sedimentology. 46(4):723–731.
   Google Scholar
• Jackson PS, Hunt J. 1975. Turbulent wind flow over a low hill. QJR Meteorol Soc. 101(430):929–955.
   Google Scholar
• Lancaster N. 1982. Linear dunes. Prog Phys Geogr. 6(4):475–504.
   Google Scholar
• Lancaster N. 1989. The dynamics of star dunes: an example from the Gran Desierto, Mexico. Sedimentology. 36(2):273–289.
   Google Scholar
• Lancaster N. 2010. Assessing dune-forming winds on planetary surfaces: application of the gross bedform normal concept. Rev Brasil Ginecol Obstet. 2(26):193–200.
   Google Scholar
• Langford RP. 1989. Fluvial-aeolian interactions: part I, modern systems. Sedimentology. 36(6):1023–1035.
   Google Scholar
• Langford RP, Chan MA. 1989. Fluvial-aeolian interactions: part II, ancient systems. Sedimentology. 36(6):1037–1051.
   Google Scholar
• Langston G, Neuman CM. 2005. An experimental study on the susceptibility of crusted surfaces to wind erosion: a comparison of strength properties of biotic and salt crusts. Geomorphology. 72(1–4):40–53.
   Google Scholar
• Liu B, Coulthard TJ. 2015. Mapping the interactions between rivers and sand dunes: implications for fluvial and aeolian geomorphology. Geomorphology. 231:246–257.
   Google Scholar
• Liu YC, Zimbelman JR. 2015. Recent near-surface wind directions inferred from mapping sand ripples on Martian dunes. Icarus. 261:169–181.
   Google Scholar
• Livingstone I, Thomas D. 1993. Modes of linear dune activity and their palaeoenvironmental significance: an evaluation with reference to southern African examples. Geol Soc London Spec Publ. 72(1):91–101.
   Google Scholar
• Lucas A, Rodriguez S, Narteau C, Charnay B, Courrech Du Pont S, Tokano T, Garcia A, Thiriet M, Hayes AG, Lorenz RD, et al. 2014. Growth mechanisms and dune orientation on titan. Geophys Res Lett. 41(17):6093–6100.
   Google Scholar
• Lv P, Narteau C, Dong ZB, Zhang ZC, Courrech Du Pont S. 2014. Emergence of oblique dunes in a landscape-scale experiment. Nat Geosci. 7:99–103.
   Google Scholar
• Muhs DR, Reynolds RL, Been J, Skipp G. 2003. Eolian sand transport pathways in the southwestern United States: importance of the Colorado River and local sources. Quatern Int. 104(1):3–18.
   Google Scholar
• Pye K, Tsoar H. 1990. Aeolian bed forms. In: Pye K, Tsoar H, editors. Aeolian sand and sand dunes. London: Unwin Hyman; p. 175–251.
   Google Scholar
• Reffet E, Courrech Du Pont S, Hersen P, Douady S. 2010. Formation and stability of transverse and longitudinal sand dunes. Geology. 38(6):491–494.
   Google Scholar
• Rubin DM. 2012. A unifying model for planform straightness of ripples and dunes in air and water. Earth Sci Rev. 113(3–4):176–185.
   Google Scholar
• Rubin DM, Hunter RE. 1987. Bedform alignment in directionally varying flows. Science. 237(4812):276–278.
   Google Scholar
• Rubin DM, Ikeda H. 1990. Flume experiments on the alignment of transverse, oblique, and longitudinal dunes in directionally varying flows. Sedimentology. 37(4):673–684.
   Google Scholar
• Rubin DM, Tsoar H, Blumberg DG. 2008. A second look at western Sinai seif dunes and their lateral migration. Geomorphology. 93(3–4):335–342.
   Google Scholar
• Rubin DM, Hesp PA. 2009. Multiple origins of linear dunes on Earth and Titan. Nat Geosci. 2(9):653–658.
   Google Scholar
• Shao Y, Dong CH. 2006. A review on East Asian dust storm climate, modelling and monitoring. Global Planet Change. 52(1–4):1–22.
   Google Scholar
• Smith K G. 1954. Standards for grading texture of erosional topography. American Journal of Science. 248(9):655–668. .
   Google Scholar
• Song Y, Yan P, Liu LY. 2006. A review of the research on complex erosion by wind and water. J Geogr Sci. 16(2):231–241.
   Google Scholar
• Stock JD, Schmidt KM, Miller DM. 2008. Controls on alluvial fan longprofiles. Geol Soc Am Bull. 120(5–6):619–640.
   Google Scholar
• Telfer M, Hesse P. 2013. Palaeoenvironmental reconstructions from linear dunefields: recent progress, current challenges and future directions. Quatern Sci Rev. 78(454):1–21.
   Google Scholar
• Thomas DSG, Tsoar H. 1990. The geomorphological role of vegetation in desert dune systems. In: Thornes JB, editor. Vegetation and erosion. Chichester: Wiley; p. 471–489.
   Google Scholar
• Ungar JE, Haff PK. 1987. Steady state saltation in air. Sedimentology. 34(2):289–299.
   Google Scholar
• Uppala SM, Kôllberg PW, Simmons AJ, Andrae U, Bechtold VDC, Fiorino M, Gibson JK, Haseler J, Hernandez A, Kelly GA, et al. 2005. The era-40 reanalysis. QJR Meteorol Soc. 131(612):2961–3012.
   Google Scholar
• Wang H, Jia X. 2013. Field observations of windblown sand and dust in the Taklimakan Desert, NW China, and insights into modern dust sources. Land Degrad Dev. 24(4):323–333.
   Google Scholar
• Wasson R, Hyde R. 1983. Factors determining desert dune types. Nature. 304(5924):337–339.
   Google Scholar
• Wiggs GFS, Livingstone I, Thomas DSG, Bullard JE. 1995. Dune mobility and vegetation cover in the Southwest Kalahari Desert. Earth Surf Process Landforms. 20(6):515–529.
   Google Scholar
• Xiong HG, Yu L. 2008. Relationship between the ancient oasis changes and rivers, glaciers in the southern Tarim Basin. Arid Land Geogr. 01:17–22. (In Chinese with English abstract).
   Google Scholar
• Yan P, Li XM, Ma YF, Wu W, Qian Y. 2015. Morphological characteristics of interactions between deserts and rivers in northern China. Aeolian Res. 19:225–233.
   Google Scholar
• Zhang D, Narteau C, Rozier O, Courrech Du Pont S. 2012. Morphology and dynamics of star dunes from numerical modelling. Nat Geosci. 5(7):463–467.
   Google Scholar
• Zhang XY, Gong SL, Zhao TL, Arimoto R, Wang YQ, Zhou ZJ. 2003. Sources of Asian dust and role of climate change versus desertification in Asian dust emission. Geophys Res Lett. 30(24):5–8.
   Google Scholar
• Zu R, Xue X, Qiang M, Yang B, Qu J, Zhang K. 2008. Characteristics of near-surface wind regimes in the Taklimakan Desert, China. Geomorphology. 96(1–2):39–47.
   Google Scholar