Delineation of erosion classes in semi‐arid southern African grasslands using vegetation indices from optical remote sensing data

As stated by many authors in the recent past, soil erosion is one of the major environmental problems in southern Africa and it will become even more severe in the future due to population growth and potential climatic changes. This study concerns the detection of different land degradation stages in semi‐arid grassland areas in the upper Mbuluzi‐river catchment (Kingdom of Swaziland). It has been carried out within the framework of an interdisciplinary EU‐funded project aimed at developing an integrated water resources management system (IWRMS) for water resources analyses and prognostic scenario planning in semi‐arid catchments of Southern Africa (Flügel et al., 2001 URL: http://www.iwrms.uni‐jena.de/download/Eu‐reports/report_final.pdf). Within this more general framework, particular attention was focused on the determination of high‐resolution morphometric parameters for detailed erosion process studies, as well as on the derivation of relationships between vegetation cover and bare soil. The latter has subsequently been used to delineate the vegetation cover density and C‐factor values for erosion models such as the revised universal soil loss equation. The examples from Southern Africa show that the methods applied are able to identify areas affected by different types of erosion. Furthermore, it is possible to estimate the parameters for a subsequent erosion modelling. Copyright © 2003 John Wiley & Sons, Ltd.

[1]  H. M. Mushala An investigation of the spatial distribution of soil erosion in the Mbuluzi River Basin of Swaziland , 2000 .

[2]  R. Tateishi,et al.  Vegetation cover estimate of arid and semi-arid regions by NOAA AVHRR data , 1998 .

[3]  D. Evans,et al.  Review article Synthetic aperture radar (SAR) frequency and polarization requirements for applications in ecology, geology, hydrology, and oceanography: A tabular status quo after SIR-C/X-SAR , 1997 .

[4]  Jerry C. Ritchie,et al.  Remote sensing applications to hydrology: airborne laser altimeters , 1996 .

[5]  K. Price Detection of soil erosion within pinyon-juniper woodlands using Thematic Mapper (TM) data☆ , 1993 .

[6]  F. Baret,et al.  Potentials and limits of vegetation indices for LAI and APAR assessment , 1991 .

[7]  Volker Hochschild Die Integration hochauflösender Fernerkundungsdaten für die physio-graphische Parametrisierung von Wasser- und Stofftransportmodellen - Fallbeispiele aus Thüringen und dem südlichen Afrika , 2001 .

[8]  M. Herold,et al.  Hydrological analysis of high resolution multifrequent, multipolarimetric and interferometric airborne SAR data , 2001 .

[9]  M. Märker,et al.  Soil erosion modelling in the Mbuluzi river catchment (Swaziland, South Africa). Part I: Modelling the dynamic evolution of gullies , 2001 .

[10]  M. Thompson,et al.  A standard land-cover classification scheme for remote-sensing applications in South Africa , 1996 .

[11]  T. Scholten,et al.  Morphogenesis and erodibility of soil‐saprolite complexes from magmatic rocks in Swaziland (Southern Africa) , 1995 .

[12]  G. R. Foster,et al.  RUSLE: Revised universal soil loss equation , 1991 .

[13]  T. Frank,et al.  Assessing change in the surficial character of a semiarid environment with Landsat residual images , 1984 .

[14]  D. Gehring,et al.  Arid Land Monitoring Using Landsat Albedo Difference Images , 1981 .

[15]  W. H. Wischmeier,et al.  Predicting rainfall erosion losses : a guide to conservation planning , 1978 .

[16]  G. Murdoch Soils and land capability in Swaziland , 1969 .