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International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004
purpose of recognition, we need to describe the properties of
pixels or groups of pixels.
2. THE STUDY AREA
The Okavango delta in northwestern Botswana is an extremely
complex and dynamic wetland ecosystem. The increasing water
demand from basin sharing countries (Angola, Namibia and
Botswana) puts the resource under growing pressure and poses
complex management problem. Water is a precious and
important resource for all three riparian states of the basin. The
demand for water is growing due to rapidly rising population
and associated activities like irrigation and power generation.
The Okavango delta (Figure 2), variedly termed as “the jewel”
of the Kalahari (Ross, 1987), Africa’s “Wetland Wilderness”
(Bailey, 1998) and so on. It is the last remnant of the ancient
great Makgadikgadi Lake, which was formed by the Kalahari
sands about three million years ago (Ross, 1987). The delta is a
large alluvial fan and experience annual flooding. It consists of
a series of permanent river channels, semi-permanent drainage
channels, lagoons, islands and floodplains that link up and then
separate again during the course of an annual flood. The delta
has a very low gradient. From Mohembo to Maun with a
distance of 240 km, there is roughly 1m height variation for
every 4 km distance (Figure 2).
x Mohembo
Figure 2. The Okavango delta as seen from Landsat 7 ETM+
(54,2 combination) image, April 2000
The Delta is located in a semi-arid region which experiences
wide variations in flooding over permanent swamps, seasonal
Swamps and other intermittently flooded areas. The permanent
swamp covers approximately 6,000 km’, while the seasonal
swamp varies between 4,000 and 10,000 km?. Water depth in
the permanent swamps averages 1.5m (UNDP, 1977), while in
the seasonal swamps it is generally less than 1m (McCarthy e/
al., 1998).
297
The river and the delta serve as major source of fresh water to
the people of the basin area. The Okavango is one of the few
large rivers in the world without notable man-made
developments and that has so far remained relatively pristine.
3. DATA AND METHODS
3.1 Data
The primary data used in this study were SPOT 5 High
Resolution Geometry (HRG) sensor image acquired on 12
November 2002 and Landsat 7 Enhanced Thematic Mapper
Plus (ETM+) sensor image acquired on 28 March 2001. The
other data used are 1:50,000 scale topographic maps and GPS
measured ground control points. Both SPOT 5 and Landsat &
images are taken during dry seasons. Figure 3 shows the scene
location of SPOT 5 and Landsat 7 over the Okavango delta.
The SPOT 5 satellite was launched on May 2002 with Araine 4
rocket and put on polar sun synchronous orbit at an altitude of
832 km from earth surface, while the Landsat 7 satellite was
launched on April 1999 with Delta rocket and put on polar, sun
synchronous orbit at an altitude of 705 km from earth surface.
Both SPOT 5 and Landsat 7 satellites orbit the earth in sun-
synchronous mode at an inclination of 98.2? and 98° degree
respectively.
Landsat 7
175/073
174/073
SPOT5
118/388
175/074 174/074
A
Figure 3. Landsat 7 ETM+ and SPOT 5 HRG scene location
over the Okavango delta
SPOT 5 HRG sensor provides multispectral (10m resolution in
band 1-3 and 20m resolution in band 4) and one panchromatic
band (Sm resolution) image. Each SPOT 5 HRG scene covers a
ground area of 60 km x 60 km (nadir viewing). The HRG is an
optical/near infrared sensor (Table 1), which is based on High
Resolution Visible (HRV) and High Resolution Visible and
Infrared Sensor (HRVIR). Both HRV and HRVIR are
optical/near infrared CCD (pushbroom) imaging radiometers
carried on SPOT-1 to -3, and SPOT- 4 respectively. The two
HRG instruments aboard SPOT 5 are the main imaging
instruments. They provide panchromatic (black and white)
imagery at a resolution of 2.5 or 5 metres and multispectral
(colour) imagery at a resolution of 10 metres.