Spatial variability in shrub vegetation across dune forms in central Saudi Arabia

被引:10
作者
Bradley, Andrew V. [1 ,3 ]
Haughan, Alice E. [2 ,3 ]
Al-Dughairi, Ahmed [4 ]
McLaren, Sue J. [5 ]
机构
[1] Univ Nottingham, Nottingham Geospatial Inst, Innovat Pk,Jubilee Campus, Nottingham NG7 2TU, England
[2] Zool Soc London, Regents Pk, London NWI 4RY, England
[3] Imperial Coll London, Dept Life Sci, Silwood Pk, Ascot SL5 7PY, Berks, England
[4] Qassim Univ, Geog Dept, Box 1343, Buraydah, Saudi Arabia
[5] Univ Leicester, Dept Geog, Univ Rd, Leicester LE1 7RH, Leics, England
关键词
Dune form; Groundwater; Slope; Remote sensing; WorldView-2; Wadi Al Rimah; DUNEFIELD ACTIVITY; SAND MOVEMENT; DESERT; COVER; PLANT; SOIL; ENVIRONMENT; DYNAMICS; PATTERNS; MOBILITY;
D O I
10.1016/j.jaridenv.2018.10.003
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
In desert dune environments, vegetation may be an indicator of dune stability and rates of sediment transport. As topography and underlying controls of vegetation vary over large spatial areas, variations in dune form make scaling up of field research difficult. To mitigate this, and to identify spatial variations in vegetation distributions in a Saudi Arabian sand sea, spectral information from high resolution satellite images was classified to map polygons of shrub vegetation over 360 km(2) of well-defined linear dunes, broken linear dunes and dome dune forms. When compared to topographic characteristics of the landscape, extracted from a digital elevation model, vegetation densities were often highest on 10-20 degrees slopes elevated above interdune salt deposits on dune flanks. Spatially this was confined to small areas, and density was not always related to dune form, more to access of groundwater which encouraged colonisation on the tops of some dunes. Field observations identified shrubs of mainly Calligonum genus whose size is related to the amounts of salts, moving sediment, and access to the water table that varies within and between dune forms. Shrub density is likened to surface roughness (z(0)) to better understand sediment movement and modelling in dunes.
引用
收藏
页码:72 / 84
页数:13
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