Width, height and slope relationships and aerodynamic maintenance of barchans

被引:133
作者
Hesp, PA
Hastings, K
机构
[1] Massey Univ, Dept Geog, Palmerston North, New Zealand
[2] GIS Asia Pacific, Palmerston North, New Zealand
关键词
barchans; dune height; horn width; morphometric relationships;
D O I
10.1016/S0169-555X(97)00070-6
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The allometric relationship between the height of barchan dunes and horn to horn widths is re-examined. The addition of new data from barchan in the Namib Desert and elsewhere confirms the relationship that the height of a barchan is approximately one-tenth of the width of the dune. Height and width of the dune are closely linked to the three-dimensional morphology of the dune, in particular, the relatively constant mean angles of around 11 degrees at which the side slopes of the dune are maintained. We suggest that the 3-D barchan form is directly controlled by aerodynamic processes. Constant feedback between three-dimensional stoss face (windward) shape of the dune, slipface height and horn to horn width, and shear stress produces an equilibrium dune form. (C) 1998 Elsevier Science B.V.
引用
收藏
页码:193 / 204
页数:12
相关论文
共 45 条
[31]  
LONG JT, 1964, GEOL SOC AM BULL, V75, P149, DOI 10.1130/0016-7606(1964)75[149:BMIIVC]2.0.CO
[32]  
2
[33]  
Mabbutt J.A., 1977, Desert landforms
[34]  
MULLIGAN KR, 1995, DESERT AEOLIAN PROCE, P131
[35]   BARCHAN DUNES OF IMPERIAL VALLEY CALIFORNIA [J].
NORRIS, RM .
JOURNAL OF GEOLOGY, 1966, 74 (03) :292-&
[36]  
Pye K., 1990, AEOLIAN SAND SAND DU
[38]  
TSOAR H, 1984, Z GEOMORPHOL, V28, P99
[39]  
TSOAR H, 1985, AARHUS U MEMOIR 8, V2, P327
[40]  
WALKER HJ, 1979, 5 U TSUK I GEOSC, P43