[1]. Ahmadi, H. (2008). Application Geomorphology, Volume2, Desert-Wind erosion, Tehran university publication (In Farsi).
[2]. Al-Awadhi, J.M., & Al-Dousari, A.M., (2013). Morphological Characteristics and Development of Coastal Nabkhas, North-East Kuwait, International Journal of Earth Sci- ences (Geologische Rundschau), 102 (3): 949-958.
[3]. Bonham, C.D.,(1989). Measurement for Terrestrial Vegetation. John wiley & Sons, Inc, 23: 65-62.
[4]. Bishop, S. R., Momiji, H., Carretero-Gonzalez, R. & Warren, A.,(2002). Modeling desert dune fields based on discrete dynamics, Discrete Dynamicsin Nature and Society, 7: 7–17.
[5]. Danin, A., (1996). Plants of desert dunes. Springer, 43: 136-177.
[6]. Dougill, A.J., & Thomas, A.D. (2002). Nebkha dunes in the Molopo Basin, south Africa and Botswana formation controls and their validity as indicators of soil degradation, Journal of arid environment,50 : 413-423.
[7]. Douseri, A. (1995). Sedimentolongical and Morohological characteristics of some nebkha deposits in the northern coastal plain of Kuwait. Arid Environ, 29: 267-292.
[8]. Hesp, P., & Mclachlan, A., (2000). Morphology, dynamics, ecology and fauna of Arc Totheca populifolia andAzania regions nebkha dunes. Journal of arid environments, 44: 155-172.
[9]. Hesp, P., (2002). Foredunes and blowouts: Initiation, geomorphology and dynamics. Geomorphology, 48: 245–268.
[10]. Hersen, P. (2004). On the crescentic shape of barchan dunes. The European Physical Journal, 37: 507–514.
[11]. Jasem, M. (2014). The Effect of a Single Shrub on Wind Speed and Nabkhas Dune Development: A Case Study in Kuwait. International Journal of Geosciences, 5: 20-26.
[12]. Mahmodi, F., (2000). Dynamic Geomorphology, University of Payamenour Press, Tehran (in Farsi).
[13]. Mohammadrezayi, S.H. (2003). Systematical Approach to acosystema analysis, First publish. Tehra (in Farsi).
[14]. Musick, H.B., & Gillette, S.M. (1996). Wind-tunnel Modeling of the Influence of Vegetation Structure on Saltation Threshold, Earth Surface Processes and Landforms, 21: 589-606.
[15]. Khalaf, F.I., Miska, R., & Al-Douseri, A ,(1995). Sedimentolongical and Morphological characteristics of some nebkha deposits in the northern coastal plain of Kuwait, Arabia. Journal Arid Environment, 29: 267-292.
[16]. Lin, G. (2002). Dust bowl in the 1930' sand storms in the USA, Global Alarm, Dustand sand storms from the world's dry lands. United Nations, 43-37.
[17]. Nicholas, P., Hamish, A., McGowan, R. & Grant, H. (2006).AUSLEM (Australian Land Erodibility Model): A tool for identifying wind erosionhazard in Australia, Geomorphology, 78, 179-200.
[18]. Poorgsrvani, M., Vali, A., & Movahedi, S., (2009). Grouped an Comparative Nebkas Type Sedliziavloreda, Romarlatorkestenica and Alhaji Mannifera the Basis of the Righteousness of Performance of Plants in the Vegetative forms in Kheirabadi Sirjan, Geography Space, 9 (31), 137-158(In Farsi).
[19]. Ramesht, M.H. (2006). Geomorphology Maps, Tehran. Samt Publication (in Farsi).
[20]. Squires, R. (2002). Dust and sand storms: An early warning of impending disaster, Global Alarm: Dust and sand storms from the world's dry lands, United Nations, 65-75.
[21]. Thomas, D.S.G., Knight, M., & Wiggs, G.F.S. (2005). Remobilization of southern African desert dune systems by twenty-first century globalwarming. Nature, 435, 1218–1221.
[22]. Tsoar, H., & Møller, J.T., (1986). The Role of Vegetation in the Formation of Linear Sand Dunes’, in Nickling, W. G. (Ed.), Aeolian Geomorphology, Allen and Unwin, Boston.
[23]. Vali, A., & Poorgsrvani, M., (2008). Comparison Analysis Nebka Morphometric Relationships between Components and Morphology of Plant Species Tamarix Mascatensis, Reaumuria Turkestanica, Mannifera Alhagi in Khairabad Sirjan, Geography and Environmental Planning, 20 (35), 119-134 (in Farsi).
[24]. Wasson, R.J., & Hyde, R. (1983). Factors determining desert dune type. Nature, 304, 337–339.
[25]. Werner, B.T. (1995). Aeolian dunes: computer simulation and attractor interpretation. Geology, 23, 1107–1110.
[26]. Wiggs, G.F.S., Livingstone, I., Thomas, D.S.G., & Bullard, J. E. (1996). Airflow and Roughness Characteristics over Partially Vegetated Linear Dunes in the Southwest Kalahari Desert, Earth Surface Processes and Landforms, 21: 19-34.
[27]. Wiggs, G.F.S., Thomas, D.S.G., Bullard, J.E., & Livingstone, I., (1995). Dune Mobility and Vegetation Cover in the Southwest Kalahari Desert, Earth Surface Processes and Landforms, 20, 515-530.
[28]. Wolfe, S.A., & Nickling, W. G., (1993). The Protective Role of Sparse Vegetation in Wind Erosion, Progress in Physical Geography, 17, 50-68.
[29]. Youlin, Y. (2002). Black windstorm in northwest China: A case study of the stormy sanddust storms on May 5th 1993, Global Alarm: Dust and sand storms from the world's dry lands, United Nations.
[30]. Yong Zhong, S.U., Rong, Y., ZhiHui, Z., & Ming, W D. (2012). Distribution and Characteristics of Nitraria sphaerocarpa nebkhas in a Gobi habitat outside an oasis in Hexi Corridor region, China, Sciences in Cold and Arid Regions, 4(4), 0288–0295.
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