[1]韩致文,董治宝,王涛,等.塔克拉玛干沙漠风沙运动若干特征观测研究[J].中国科学(D辑),2003,33(3):255-263. [2]Bagnold R A.The Physics of Blown Sand and Desert Dunes[M].London:Methuen & Co,1941:265. [3]Tsoar H.Profile analysis of sand dunes and their study state significance[J].Geografiska Annaler.Series A,Physical Geography,1985,67A:45-59. [4]Lancaster N.Reply:Variation in wind velocity and sand transport on the windward flanks of desert sand dunes[J].Sedimentology,1987,34:511-520. [5]Lancaster N.Dune morphology and dynamics[M]// Abrahams A D.Geomorphology of Desert Environments.London:Chapmem and Hill,1994:417-505. [6]Burukinshaw J R,Llenberget W K,Rust L C.Wind-speed profile over a reversing transverse dune[J].Geological Society,1993,72:25-36. [7]Wiggs G F S.Desert dune dynamics and evaluation of shear velocity:An integrated approach[J].Geological Society,1993,72:37-46. [8]Kenna M C,Neuman C,Lancaster N,et al.Relations between dune morphology,air flow,and sediment flux on reversing dunes[J].Sedimentology,1997,44:1103-1114. [9]Stam J M T.On the modeling of two-dimensional aeolian dunes[J].Sedimentology,1997,44:127-141. [10]Sauermann G,Andrade J S,Maia L P,et al.Wind velocity and sand transport on a barchan dune[J].Geomorphology,2003,54:245-255. [11]Lettau K,Lettau H.Experimental and micrometeorological field studies of dune migration[M]//Lettau H H,lettau K.Exploring the worlds driest climate.Center for Climatic Research University of Madison-Wisconsin,1978:110-147. [12]Srensen M.An analytic model of wind-blown sand transport[J].Acta Mechanica,1991(Suppl.):67-81. [13]Anselin L,Donson R,Hudak S.Linking GIS and spatial data analysis in practice[J].Geographical Systems,1993(1):3-23. [14]艾力·买买提明,杨青,阿吉古丽·沙依提,等.塔中油田作业区防护林带的小气候效应[J].中国沙漠,2005,25(4):535-540. [15]Lancaster N.The Namib Sand Sea:Dune forms,process and sediments[M].A A Balkema,Rotterdam,1989. [16]陈渭南,雷加强.塔克拉玛干沙漠新月形沙丘不同部位的粒度特征[J].干旱区资源与环境,1992,6(2):101-108. [17]张春来,郝青振,邹学勇,等.新月形沙丘迎风坡形态及沉积物对表面气流的响应[J].中国沙漠,1999,19(4):359-364. [18]Goovaerts P.Geostatistical approaches for incorporating elevation into the spatial interpolation of rainfall[J].Journal of Hydrology,2000,228:113-129. [19]Hunt J R C,Leibovich S,Richard K J.Turbulent wind flow over smooth hills[J].Quarterly Journal of the Royal Meteorological Society,1988,114:1435-1470. [20]Mlligan K R.Velocity profiles measured on the windward slope of a transverse dune[J].Earth Surface Processes and Landforms,1988,13:573-582. [21]Finnigan J J,Raupach M R,Bradley E F,et al.A wind tunnel study of turbulent flow over a two-dimensional ridge[J].Boundary-Layer Meteorology,1990,50:277-317. [22]吴正.风沙地貌与治沙工程学[M].北京:科学出版社,2003:36-42. [23]钱光强,董治宝,罗万银,等.横向沙丘背风侧气流重附风洞模拟[J].中国沙漠,2008,28(1):16-20. [24]钱广强,董治宝,罗万银,等.横向沙丘气流平均速度变化规律的风洞模拟[J].中国沙漠,2009,29(1):10-17. [25]Sauermann G,Kroy K,Herrmann H J.A continuum saltation model for sand dunes[J].Physical Review E,2001,E64,031305. [26]黄富祥,牛海山,王明星,等.毛乌素沙地植被覆盖率与风蚀输沙率定量关系[J].地理学报,2001,56(6):700-710. [27]Shao Y,Rauppach M R,Leys J F.A model for predicting aeolian sand drift and dust entrainment on scales from paddock to region[J].Austrain Journal of Soil Research,1996,34:309-342. [28]Shao Y.Physical and Modeling of Wind Erosion[M].Berlin of Germany:Springer Press,2009:49-85. [29]李振山,王怡,贺丽敏.半干旱区植被-风沙动力过程耦合研究:Ⅰ.模型[J].中国沙漠,2009,29(1):23-30. [30]王怡,李振山,陈悠.半干旱区植被-风沙动力过程耦合研究:Ⅱ.模拟[J].中国沙漠,2009,29(1):31-39. [31]陈悠,李振山,王怡.半干旱区植被-风沙动力过程耦合研究:Ⅲ.应用[J].中国沙漠,2009,29(1):39-46. |