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Theoretical and Applied Climatology

, Volume 135, Issue 3–4, pp 1017–1029 | Cite as

Temporal variation of the wind environment and its possible causes in the Mu Us Dunefield of Northern China, 1960–2014

  • Xujia Cui
  • Hu SunEmail author
  • Zhibao DongEmail author
  • Zhengyao Liu
  • Chao Li
  • Zhengcai Zhang
  • Xiaolan Li
  • Lulu Li
Original Paper

Abstract

Research on the wind environment variation improves our understanding of the process of climate change. This study examines temporal variation of the near-surface wind environment and investigates its possible causes in the Mu Us Dunefield of Northern China from 1960 to 2014, through analyzing the meteorological data from seven stations and the land use and land cover (LUCC) change data with 100 m resolution. The wind speed had a widespread significant decrease with an average trend of − 0.111 m s−1 decade−1, although the rate of decrease differed seasonally. This negative trend was also found in the winds that were above a 5 m s−1 threshold, as well as the percentage of their days, which influenced the wind speed change more strongly. Overall, 88.69% of the annual decrease resulted from decreases in the maximum wind speed, and the percentage even reached 100% in autumn and winter. We further found that the drift potential decreased at decadal time scales, mainly focusing on three prevailing wind groups: the northerly, westerly, and southerly winds. This revealed the weakened East Asian monsoon and westerly circulation in the lower atmosphere. Against the context of climate warming, the decline of wind speeds in spring was closely related to the greenhouse gas, while the winter decline was closely associated with the aerosol or atmospheric dust. Moreover, the LUCC change showed the decreased areas of sand land and the increased areas of vegetation-covered land, which increased the ground surface roughness and was another reason for the weakened wind environment.

Keywords

Temporal variation Wind environment Land use change The Mu Us Dunefield Northern China 

Notes

Acknowledgments

We gratefully acknowledge the China Meteorological Data Service Center for the supply of meteorological data, and the Data Center for Resources and Environmental Sciences of Chinese Academy of Sciences for the supply of LUCC change data.

Funding information

This work was supported by the National Natural Science Foundation of China (41601002) and the Fundamental Research Funds for the Central Universities of China (GK201604011).

References

  1. Azorin-Molina C, Vicente-Serrano SM, McVicar TR, Jerez S, Sanchez-Lorenzo A, López-Moreno JI, Revuelto J, Trigo RM, Lopez-Bustins JA, Espirito-Santo F (2014) Homogenization and assessment of observed near-surface wind speed trends over Spain and Portugal, 1961-2011. J Clim 27(10):3692–3712.  https://doi.org/10.1175/JCLI-D-13-00652.1 CrossRefGoogle Scholar
  2. Azorin-Molina C, Guijarro JA, McVicar TR, Vicente-Serrano SM, Chen D, Jerez S, Espirito-Santo F (2016a) Trends of daily peak wind gusts in Spain and Portugal, 1961-2014. J Geophys Res: Atmos 121(3):1059–1078.  https://doi.org/10.1002/2015JD024485 Google Scholar
  3. Azorin-Molina C, Vicente-Serrano SM, McVicar TR, Revuelto J, Jerez S, Lopez-Moreno JI (2016b) Assessing the impact of measurement time interval when calculating wind speed means and trends under the stilling phenomenon. Int J Climatol 37(1):480–492.  https://doi.org/10.1002/joc.4720 CrossRefGoogle Scholar
  4. Azorin-Molina C, Menendez M, McVicar TR, Acevedo A, Vicente-Serrano SM, Cuevas E, Minola L, Chen DL (2017) Wind speed variability over the Canary Islands, 1948–2014: focusing on trend differences at the land–ocean interface and below–above the trade-wind inversion layer (online). Clim Dyn doi: https://doi.org/10.1007/s00382-017-3861-0
  5. Bichet A, Wild M, Folini D, Schal C (2012) Causes for decadal variations of wind speed over land: sensitivity studies with a global climate model. Geophys Res Lett 39:L11701.  https://doi.org/10.1029/2012GL051685 CrossRefGoogle Scholar
  6. Bigg GR (1993) Comparison of coastal wind and pressure trends over the tropical Atlantic: 1946–1987. Int J Climatol 13(4):411–421.  https://doi.org/10.1002/joc.3370130405 CrossRefGoogle Scholar
  7. Bollasina MA, Ming Y, Ramaswamy V (2011) Anthropogenic aerosols and the weakening of the South Asian summer monsoon. Science 334:502–505.  https://doi.org/10.1126/science.1204994 CrossRefGoogle Scholar
  8. China Meteorological Adminisitration (CMA) (1979) Ground surface meteorological observation specification. China Meteorological Press, BeijingGoogle Scholar
  9. Dadaser-Celik F, Cengiz E (2014) Wind speed trends over Turkey from 1975 to 2006. Int J Climatol 34:1913–1927CrossRefGoogle Scholar
  10. 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.  https://doi.org/10.1016/j.geomorph.2008.10.015 CrossRefGoogle Scholar
  11. Dong ZB, Qian GQ, Lv P, Hu GY (2013) Investigation of the sand sea with the tallest dunes on Earth: China’s Badain Jaran Sand Sea. Earth Sci Rev 120:20–39.  https://doi.org/10.1016/j.earscirev.2013.02.003 CrossRefGoogle Scholar
  12. Fryberger SG (1979) Dune forms and wind regime. In: McKee ED (ed) A study of global sand seas. U.S. Government Printing Office, Washington, pp 137–160Google Scholar
  13. Fu GB, Yu JJ, Zhang YC, Hu SS, Ouyang RL, Liu WB (2011) Temporal variation of wind speed in China for 1961–2007. Theor Appl Climatol 104(3):313–324.  https://doi.org/10.1007/s00704-010-0348-x CrossRefGoogle Scholar
  14. Goudie AS, Middleton NJ (2006) Desert dust in the global system. Springer, HeidelbergGoogle Scholar
  15. Gower JFR (2002) Temperature, wind and wave climatologies, and trends from marine meteorological buoys in the Northeast Pacific. J Clim 15(24):3709–3718.  https://doi.org/10.1175/1520-0442(2002)015<3709:TWAWCA>2.0.CO;2 CrossRefGoogle Scholar
  16. Greeley R, Iversen JD (1985) Wind as a geologic process on Earth, Mars, Venus and Titan. Cambridge University Press, CambridgeCrossRefGoogle Scholar
  17. Greene JS, Chatelain M, Morrissey M, Stadler S (2012) Estimated changes in wind speed and wind power density over the Western High Plains, 1971–2000. Theor Appl Climatol 109:507–518.  https://doi.org/10.1007/s00704-012-0596-z CrossRefGoogle Scholar
  18. Guo H, Xu M, Hu Q (2011) Changes in near-surface wind speed in China: 1969-2005. Int J Climatol 31(3):349–358.  https://doi.org/10.1002/joc.2091 CrossRefGoogle Scholar
  19. Jewell PW, Nicoll K (2011) Wind regimes and aeolian transport in the Great Basin, U.S.A. Geomorphology 129(1–2):1–13.  https://doi.org/10.1016/j.geomorph.2011.01.005 CrossRefGoogle Scholar
  20. Jia FF, Lu RJ, Gao SY, Li JF, Liu XK (2015) Holocene aeolian activities in the southeastern mu Us Desert, China. Aeolian Res 19:267–274.  https://doi.org/10.1016/j.aeolia.2015.01.002 CrossRefGoogle Scholar
  21. Jiang Y, Luo Y, Zhao ZC, Tao SW (2010) Changes in wind speed over China during 1956–2004. Theor Appl Climatol 99:421–430.  https://doi.org/10.1007/s00704-009-0152-7 CrossRefGoogle Scholar
  22. Kim J, Paik K (2015) Recent recovery of surface wind speed after decadal decrease: a focus on South Korea. Clim Dyn 45(5):1699–1712.  https://doi.org/10.1007/s00382-015-2546-9 CrossRefGoogle Scholar
  23. Klink K (1999) Trends in mean monthly maximum and minimum surface wind speeds in the coterminous United States, 1961–1990. Clim Res 13(3):193–205.  https://doi.org/10.3354/cr013193 CrossRefGoogle Scholar
  24. Lancaster N (1995) Geomorphology of desert dunes. Routledge, LondonGoogle Scholar
  25. Liang P, Yang XP (2016) Landscape spatial patterns in the Maowusu (Mu Us) Sandy Land, Northern China and their impact factors. Catena 145:321–333.  https://doi.org/10.1016/j.catena.2016.06.023 CrossRefGoogle Scholar
  26. Liu JY, Liu ML, Tian HQ, Zhuang DF, Zhang ZX, Zhang W, Tang XM, Deng XZ (2005) Spatial and temporal patterns of China’s cropland during 1990–2000: an analysis based on Landsat TM data. Remote Sens Environ 98:442–456.  https://doi.org/10.1016/j.rse.2005.08.012 CrossRefGoogle Scholar
  27. Livingstone I, Warren A (1996) Aeolian geomorphology: an introduction. Longman, SingaporeGoogle Scholar
  28. Lorenz RD (2010) Planetary science: winds of change on Titan. Science 329(5991):519–520.  https://doi.org/10.1126/science.1192840 CrossRefGoogle Scholar
  29. Mason JA, Swinehart JB, Lu HY, Miao XD, Cha P, Zhou YL (2008) Limited change in dune mobility in response to a large decrease in wind power in semi-arid Northern China since the 1970s. Geomorphology 102(3–4):351–363.  https://doi.org/10.1016/j.geomorph.2008.04.004 CrossRefGoogle Scholar
  30. McKee ED (ed) (1979) A study of global sand seas. United States Geological Survey, Professional Paper 1052Google Scholar
  31. McVicar TR, Roderick ML (2010) Atmospheric science: winds of change. Nat Geosci 3(11):747–748.  https://doi.org/10.1038/ngeo1002 CrossRefGoogle Scholar
  32. McVicar TR, Van Niel TG, Li LT, Roderick ML, Rayner DP, Ricciardulli L, Donohue RJ (2008) Wind speed climatology and trends for Australia, 1975-2006: capturing the stilling phenomenon and comparison with near-surface reanalysis output. Geophys Res Lett 35(20):L20403.  https://doi.org/10.1029/2008GL035627 CrossRefGoogle Scholar
  33. McVicar TR, Roderick ML, Donohue RJ, Li LT, Van Niel TG, Thomas A, Grieser J, Jhajharia D, Himri Y, Mahowald NM, Mescherskaya AV, Kruger AC, Rehman S, Dinpashoh Y (2012) Global review and synthesis of trends in observed terrestrial near-surface wind speeds: implications for evaporation. J Hydrol 416-417:182–205.  https://doi.org/10.1016/j.jhydrol.2011.10.024 CrossRefGoogle Scholar
  34. Minola L, Azorin-Molina C, Chen DL (2016) Homogenization and assessment of observed near-surface wind speed trends across Sweden, 1956–2013. J Clim 29(20):7397–7415.  https://doi.org/10.1175/JCLI-D-15-0636.1 CrossRefGoogle Scholar
  35. Newman M (2013) Atmospheric science: winds of change. Nat Clim Chang 3(7):538–539.  https://doi.org/10.1038/nclimate1915 CrossRefGoogle Scholar
  36. Ramage CS (1987) Secular change in reported surface wind speeds over the ocean. J Appl Meteorol Climatol 26(4):525–528.  https://doi.org/10.1175/1520-0450(1987)026<0525:SCIRSW>2.0.CO;2 CrossRefGoogle Scholar
  37. Roderick ML, Rotstayn LD, Farquhar GD, Hobbins MT (2007) On the attribution of changing pan evaporation. Geophys Res Lett 34:L17403.  https://doi.org/10.1029/2007GL031166 CrossRefGoogle Scholar
  38. Seidel DJ, Fu Q, Randel WJ, Reichle TJ (2008) Widening of the tropical belt in a changing climate. Nat Geosci 1(1):21–24.  https://doi.org/10.1038/ngeo.2007.38 CrossRefGoogle Scholar
  39. Si P, Luo CJ, Liang DP (2017) Homogenization of Tianjin monthly near-surface wind speed using RHtestsV4 for 1951–2014 (online). Theor Appl Climatol doi: https://doi.org/10.1007/s00704-017-2140-7
  40. Sivakumar MVK (2007) Interactions between climate and desertification. Agric For Meteorol 142(2–4):143–155.  https://doi.org/10.1016/j.agrformet.2006.03.025 CrossRefGoogle Scholar
  41. Tuller SE (2004) Measured wind speed trends on the west coast of Canada. Int J Climatol 24(11):1359–1374.  https://doi.org/10.1002/joc.1073 CrossRefGoogle Scholar
  42. Udden JA (1894) Erosion, transportation and sedimentation performed by the atmosphere. J Geol 2:318–331.  https://doi.org/10.1086/606957 CrossRefGoogle Scholar
  43. UNEP (2017) Frontiers 2017 emerging issues of environmental concern. United Nations Environment Programme, NairobiGoogle Scholar
  44. Vautard R, Cattiaux J, Yiou P, Thepaut JN, Ciais P (2010) Northern hemisphere atmospheric stilling partly attributed to increased surface roughness. Nat Geosci 3(11):756–761.  https://doi.org/10.1038/NGEO979 CrossRefGoogle Scholar
  45. Vecchi GA, Soden BJ, Wittenberg AT, Held IM, Leetmaa A, Harrison MJ (2006) Weakening of tropical Pacific atmospheric circulation due to anthropogenic forcing. Nature 441(7089):73–76.  https://doi.org/10.1038/nature04744 CrossRefGoogle Scholar
  46. Wan H, Wang XL, Swail VR (2010) Homogenization and trend analysis of Canadian near-surface wind speeds. J Clim 23:1209–1225.  https://doi.org/10.1175/2009JCLI3200.1 CrossRefGoogle Scholar
  47. Wang XM, Dong ZB, Yan P, Zhang JW, Qian GQ (2005) Wind energy environments and dunefield activity in the Chinese deserts. Geomorphology 65(1–2):33–48.  https://doi.org/10.1016/j.geomorph.2004.06.009 CrossRefGoogle Scholar
  48. Wang XM, Eerdun H, Zhou ZJ, Liu XP (2007a) Significance of variations in the wind energy environment over the past 50 years with respect to dune activity and desertification in and semiarid Northern China. Geomorphology 86(3–4):252–266.  https://doi.org/10.1016/j.geomorph.2006.09.003 CrossRefGoogle Scholar
  49. Wang XL, Wen QH, Wu YH (2007b) Penalized maximal t test for detecting undocumented mean change in climate data series. J Appl Meteorol Climatol 46(6):916–931.  https://doi.org/10.1175/JAM2504.1 CrossRefGoogle Scholar
  50. Wever N (2012) Quantifying trends in surface roughness and the effect on surface wind speed observations. J Geophys Res: Atmos 117:D11104.  https://doi.org/10.1029/2011JD017118 CrossRefGoogle Scholar
  51. Wu J, Zha JL, Zhao DM (2016) Estimating the impact of the changes in land use and cover on the surface wind speed over the East China Plain during the period 1980–2011. Clim Dyn 46:847–863CrossRefGoogle Scholar
  52. Xu M, Chang C, Fu C, Ye Q, Robock A, Robinson D, Zhang H (2006) Steady decline of East Asian monsoon winds, 1969-2000: evidence from direct ground measurements of wind speed. J Geophys Res 111:D24111.  https://doi.org/10.1029/2006JD007337 CrossRefGoogle Scholar
  53. Yan HM, Liu JY, Huang HQ, Cao MK (2009) Assessing the consequence of land use change on agricultural productivity in China. Glob Planet Chang 67:13–19.  https://doi.org/10.1016/j.gloplacha.2008.12.012 CrossRefGoogle Scholar
  54. Yang XM, Li ZX, Feng Q, He YQ, An WL, Zhang W, Cao WH, Yu TF, Wang YM, Theakstone WH (2012a) The decreasing wind speed in southwestern China during 1969-2009 and possible causes. Quat Int 263:71–84.  https://doi.org/10.1016/j.quaint.2012.02.020 CrossRefGoogle Scholar
  55. Yang XP, Li HW, Conacher A (2012b) Large-scale controls on the development of sand seas in Northern China. Quat Int 250:74–83.  https://doi.org/10.1016/j.quaint.2011.03.052 CrossRefGoogle Scholar
  56. Yang XP, Wang XM, Liu ZT, Li HW, Ren XZ, Zhang DG, Ma ZB, Rioual P, Jin XD, Scuderi L (2013) Initiation and variation of the dune fields in semi-arid China—with a special reference to the Hunshandake Sandy Land, Inner Mongolia. Quat Sci Rev 78:369–380.  https://doi.org/10.1016/j.quascirev.2013.02.006 CrossRefGoogle Scholar
  57. Young IR, Zieger S, Babanin AV (2011) Global trends in wind speed and wave height. Science 332(6028):451–455.  https://doi.org/10.1126/science.1197219 CrossRefGoogle Scholar
  58. Zhang XL, Xiong Z, Zhang XZ, Shi Y, Liu JY, Shao QQ (2017) Simulation of the climatic effects of land use/land cover changes in eastern China using multi-model ensembles. Glob Planet Chang 154:1–9.  https://doi.org/10.1016/j.gloplacha.2017.05.003 CrossRefGoogle Scholar
  59. Zheng CW, Pan J, Li CY (2016) Global oceanic wind speed trends. Ocean Coast Manag 129:15–24.  https://doi.org/10.1016/j.ocecoaman.2016.05.001 CrossRefGoogle Scholar

Copyright information

© Springer-Verlag GmbH Austria, part of Springer Nature 2018

Authors and Affiliations

  1. 1.School of Geography and TourismShaanxi Normal UniversityXi’anChina
  2. 2.Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhouChina

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