Abstract
The watershed of the Ningxia–Inner Mongolia reach of the Yellow River suffers serious wind erosion hazards and the areas with high wind erosion probabilities need to be identified to help in the building of the correct wind-sand blown hazard protection systems. In this study, the Integrated Wind-Erosion Modelling System model and Normalized Difference Vegetation Index (NDVI) data set were used to identify the distributions of threshold wind speeds and wind erosion occurrence probabilities. Through field observations, the relationships among NDVI, vegetation cover, frontal area (lateral cover), roughness length, and threshold friction velocity were obtained. Then, using these relationships, the spatial distributions of threshold wind speeds for wind erosion at a height of 10 m for the different months were mapped. The results show that the threshold wind speed ranged from 7.91 to 35.7 m/s. Based on the threshold wind speed distributions, the wind erosion occurrence probabilities of different months were calculated according to the current wind speed. The results show that the distributions of wind erosion occurrence probabilities and threshold wind speeds were related to each other. The resulting maps of threshold wind speeds and wind erosion occurrence probabilities would help environmental and agricultural researchers in determining some strategies for mitigating or adapting from wind erosion hazards.
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References
Bagnold RA (1941) The physics of blown sand and desert dunes. Chapman and Hall, London, pp 182–256
Buschiazzo DE, Zobeck TM (2008) Validation of WEQ, RWEQ and WEPS wind erosion for different arable land management systems in the Argentinean Pampas. Earth Surf Proc Land 33:1839–1850
Chen W, Lei J (1992) The particle size types of barchans dunes different sections in Taklimakan Desert. J Arid Land Resour Environ 6:101–118
Du H, Han Z, Deng X, Zhang Y, Sun J (2011) A sand flux model for the surface of barchans dunes using GIS-based spatial analysis. J Desert Res 31:815–823
Du H, Xue X, Sun J (2012) Surface characters and blown-sand movement in Ulanbuh Desert along Yellow River’s Bank. Trans Chin Soc Agric Eng 28:156–165
Du H, Xue X, Wang T (2014) Estimation of saltation emission in the Kubuqi Desert, North China. Sci Total Environ 479–480:77–92
Gao Y, Wang Y, Qiu X, Chen Z, Chen Y, Ma L, Miao Q, Wang Z (2008) Simulation study on wind energy resource over rugged terrains based on GIS. Acta Energiae Solaris Sinica 2:163–169
Hoffmann C, Funk R, Wieland R, Li Y, Sommer M (2008) Effects of grazing and topography on dust flux and deposition in the Xilingele grassland, Inner Mongolia. J Arid Environ 72:792–807
Honda Y (1999) Development of estimation method for vegetation biomass using satellite observation. Report of CREST by Japan Science and Technology Agency, pp 1154–1161
Jugder D, Shinoda M, Sugimoto N (2011) Spatial and temporal variations of dust concentrations in the Gobi Desert of Mongolia. Global Planet Change 78:14–22
Kimura R, Shinoda M (2010) Spatial distribution of threshold wind speeds for dust outbreaks in northeast Asia. Geomorphology 114:319–325
Kimura R, Bai L, Wang J (2009) Relationship among dust outbreaks, vegetation cover, and surface soil water content on the Loess Plateau of China, 1999–2000. Catena 77:292–296
Kurosaki Y, Mikami M (2004) Effect of snow cover on threshold wind velocity of dust outbreak. Geophys Res Lett. doi:10.1029/2003GL018632
Kurosaki Y, Mikami M (2005) Regional difference in the characteristic of dust event in East Asia: relationship among dust outbreak, surface wind, and land surface condition. J Meteorol Soc Jpn 83:1–18
Kurosaki Y, Mikami M (2007) Threshold wind speed for dust emission in east Asia and its seasonal variations. J Geophys Res. doi:10.1029/2006JD007988
Lancaster N, Bass A (1998) Influence of vegetative cover on sand transport by wind: field studies at Owens lake, Califomia. Earth Surf Proc Land 23:69–82
Laurent B, Marticorena B, Bergametti G (2005) Simulation of the mineral dust emission frequencies from desert areas of China and Mongolia using an arodynamic roughness length map derived from the POLDER/ADEOS 1 surface products. J Geophys Res. doi:10.1029/2004JD005013
Li F, Kang L, Zhang H, Zhao L, Shirato Y, Taniyama I (2005) Changes in intensity of wind erosion at different stages of degradation development in grasslands of Inner Mongolia, China. J Arid Environ 62:567–585
Liu T, Yang X, Dong J, Fan X, Li H, Zhu B (2010) A preliminary study of relation between Megadune shape and wind regime in the Badain Jaran Desert. J Desert Res 30:1285–1291
McTainsh GH, Lynch AW, Tew EK (1998) Climatic controls upon dust storm occurrence in eastern Australia. J Arid Environ 39:457–466
Musick HB, Gillette DA (1990) Field evaluation of relationship between a vegetation structural parameter and sheltering against wind erosion. Land Degrad Dev 2:87–94
O’Loingsigh T, McTainsh GH, Tews EK, Strong CL, Leys JF, Shinkfield P, Tapper NJ (2014) The dust storm index (DSI): a method for monitoring broadscale wind erosion using meteorological records. Aeolian Res 12:29–40
Owen RP (1964) Saltation of uniform grains in air. J Fluid Mech 20:225–242
Raupach MR, Gillette DA, Leys JF (1993) The effect of roughness elements on wind erosion threshold. J Geophys Res 98(D2):3023–3029
Shao Y (2001) A model for mineral dust emission. J Geophys Res 106(20):239–254
Shao Y (2008) Physical and modeling of wind erosion. Springer Press, Berlin, p 174
Shao Y, Raupach M, Leys JF (1996) A model for prediction Aeolian sand drift and dust entrainment on scales form paddock to region. Aust J Soil Res 34:309–342
Sharratt B, Feng G, Wendling L (2007) Loss of soil and PM10 from agricultural fields associated with high winds on the Columbia Plateau. Earth Surf Proc Land 32:621–630
Sherman DJ (1992) An equilibrium relationship for shear velocity and apparent roughness length in aeolian saltation. Geomorphology 5:419–431
Shi T, Yan Y, Wang L, Wang Z (2007) Large-scale wind speed simulation based on DEM. Geogr Geo-Inf Sci 23:26–29
Song SK (2005) Synoptic meteorological feature affecting Asian dust transport and its quantitative estimation. Ph.D. Thesis, Pusan National University, Pusan, Korea
Sterk G, Raats PAC (1996) Comparison of models describing the vertical distribution of wind-eroded sediment. Soil Sci Soc Am J 60(6):1914–1919
Stroosnijder L (2007) Rainfall and land degradation. In: Sivakumar MVK, Ndiang’ui N (eds) Climate and land degradation. Springer, Berlin, pp 167–195
Visser SM, Sterk G (2007) Nutrient dynamics—wind and water erosion at the village scale in the Sahel. Land Degrad Dev 18(5):578–588
Zhang Z, Wieland R, Reiche M, Funk R, Hoffmann C, Li Y, Sommer M (2012) Identifying sensitive areas to wind erosion in the Xilingele grassland by computational fluid dynamics modelling. Ecol Inform 8:37–47
Zhi S, Qian G, Luo J (2001) A study of wind velocity varying with altitude on the coastal areas of Guangdong Province. Trop Geogr 21(2):131–134
Acknowledgments
This work was financially supported by the National Key Basic Research Program of China (Grant No. 2011CB403306), and the Foundation for Excellent Youth Scholars of CAREERI, CAS (Y451201001). Some of the data set has been provided by the Environmental and Ecological Science Data Center for West China, the National Natural Science Foundation of China (http://westdc.westgis.ac.cn). All assistance we received has been greatly appreciated.
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Du, H., Xue, X., Deng, X. et al. Wind erosion occurrence probabilities maps in the watershed of the Ningxia–Inner Mongolia reach of the Yellow River, China. Environ Earth Sci 75, 86 (2016). https://doi.org/10.1007/s12665-015-4945-y
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DOI: https://doi.org/10.1007/s12665-015-4945-y