Results from the EO‐1 experiment—A comparative study of Earth Observing‐1 Advanced Land Imager (ALI) and Landsat ETM+ data for land cover mapping in the Okavango Delta, Botswana

The Earth Observing‐1 (EO‐1) satellite acquired a sequence of data in 2001 and 2002 that highlighted the annual flooding of the lower Okavango Delta. The data were collected as part of the calibration/validation programme for the Advanced Land Imager (ALI) sensor on the NASA EO‐1 satellite. The primary purpose of this study was to compare the capability of ALI to that of Landsat ETM+ for large‐scale mapping applications in the Okavango Delta. While the extent and inaccessibility of many areas of the Delta make application of remote sensing attractive, the availability of data with adequate spatial and spectral resolution has limited the characterization of the complex patterns of land cover and geomorphology in the Delta. Initial analysis of the ALI data via supervised classification clearly showed macro‐flood features, delineation of downstream channel flow areas, and lateral‐downstream inundation of the floodplain. These patterns and the proportions of flooding of the channel compared to that of the floodplain (impoundment) varied annually, from the wetter seasonal swamps through the drier seasonal and occasional swamps. Consistently higher classification accuracies achieved using ALI data relative to ETM+ data are attributed to the higher signal‐to‐noise ratio and the increased dynamic range of the ALI data.

[1]  F. White The vegetation of Africa : a descriptive memoir to accompany the Unesco/AETFAT/UNSO vegetation map of Africa , 1985 .

[2]  H. Sternberg,et al.  The gradient of the Okavango fan, Botswana, and its sedimentological and tectonic implications , 1997 .

[3]  Use of image processing and GIS techniques to determine the extent and possible causes of land management/fenceline induced degradation problems in the Okavango area, northern Botswana , 1997 .

[4]  P. A. Larkin,et al.  Observations on the hydrology and geohydrology of the Okavango Delta , 1998 .

[5]  W. Ellery,et al.  THE OKAVANGO DELTA , 1998 .

[6]  Donald E. Lencioni,et al.  EO-1 Advanced Land Imager , 1999, Optics & Photonics.

[7]  Melba M. Crawford,et al.  Fusion of airborne polarimetric and interferometric SAR for classification of coastal environments , 1999, IEEE Trans. Geosci. Remote. Sens..

[8]  P. Keddy,et al.  Wetland Ecology: Principles and Conservation , 2000 .

[9]  Jeffrey A. Mendenhall,et al.  EO-1 Advanced Land Imager Technology Validation Report , 2002 .

[10]  S. Ringrose,et al.  Origin and palaeo‐environments of calcareous sediments in the Moshaweng dry valley, southeast Botswana , 2002 .

[11]  Hao Chen,et al.  Processing Hyperion and ALI for forest classification , 2003, IEEE Trans. Geosci. Remote. Sens..

[12]  Susan Ringrose,et al.  Mapping ecological conditions in the Okavango delta, Botswana using fine and coarse resolution systems including simulated SPOT vegetation imagery , 2003 .

[13]  Stephen G. Ungar,et al.  Overview of the Earth Observing One (EO-1) mission , 2003, IEEE Trans. Geosci. Remote. Sens..

[14]  James C. Storey,et al.  A geometric performance assessment of the EO-1 advanced land imager , 2004, IEEE Transactions on Geoscience and Remote Sensing.

[15]  S. Ringrose,et al.  Use of remotely sensed data in the analysis of soil‐vegetation changes along a drying gradient peripheral to the Okavango Delta, Botswana , 2005 .