In: Wagner W., Szekely, B. (eds.): ISPRS TC VII Symposium - 100 Years ISPRS, Vienna, Austria, July 5-7, 2010, IAPRS, Vol. XXXVIII, Part 7B
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however, is sometimes weak (Jensen, 2005). In heterogeneous
areas, such as residential areas, it has been shown that
classification accuracies may improve even as spatial resolution
decreases (Cushnie, 1987). This occurs due to the potentials of
urban features to blend together to form composite distinctive
“urban signals” that can be distinguished from other landcovers.
In this study, the capabilities of three satellite imageries
including Landsat, NigeriaSat-1 and SPOT-XS for landuse
studies are evaluated with a view to amplifying the
understanding of their specific potentials, advantages and
limitations for environmental studies. This is borne out of the
growing recognition of the need to develop “appropriate
technology” for developing countries to enable researchers
based in these countries to accomplish desirable level of
sophistication in earth’s resources analyses even with their
limited access to spatial data.
2. THE STUDY AREA/ LOCATION EXTENT
The study area is made up of Ekiti west, Ado-Ekiti,
Irepodun/ Ifelodun and Ekiti south-west. Local government
areas in Ekiti State of western Nigeria (Figure 1). The State lies
within Longitudes 4° 5 and 5° 45 East of the Greenwich
Meridian and Latitudes 7° 15 and 8° 5 North of the Equator. It
is about 6,353 square kilometers in size. It is bounded in the
north by Kwara and Kogi States, in the West by Osun State and
Ondo State in the East and in the South. The State has 16 Local
Government Areas. By 1991 Census, its population was
1,647,822. The estimated population upon its creation on
October 1 st 1996 was 1,750,000 with the capital located at Ado-
Ekiti (Ekiti Investors Handbook, 2002). The current estimated
population based on 2006 census, was 2384212 million people
(NPC, 2006).
Figure 1: Map of Ekiti State and the LGAs used for the study
The State is mainly an upland area, rising generally around
250 meters above the sea level (Ekiti Investors Handbook,
2002). The landscape consists of ancient plains broken by
steep-sided outcropping dome rocks. These rocks occur singly
or in groups or ridges and the most notable of these are to be
found in Efon-Alaaye, Ikere-Ekiti and Okemesi-Ekiti (EKSG,
1997). The area is underlain by metamorphic rock of the
basement complex. The State is dotted with hills of varying
heights. The notable ones among them are Ikere-Ekiti Hills in
the southern, Efon-Alaaye Hills in the western and Ado-Ekiti
Hills in the central parts.
The State enjoys the tropical climate with two distinct
seasons. These are the rainy (April-October) and the dry
(November-March) seasons with an annual rainfall of around
1150mm. Temperatures range between 21° and 28°C with high
humidity. The South-Westerly wind and the North-Easterly
Trade winds blow in the rainy and dry (harmattan) season
respectively. The tropical forest originally covered this part of
Nigeria. However, as a result of exploitation for many centuries
of exploitation, the original vegetation has been removed and
now replaced with anthropic covers. Forest is now confined
largely in the south, while savanna dominates the natural
landscape in the north (Kayode, 1999 and EKSG, 1997).
3. METHODOLOGY
3.1 Data Acquisition and Image Preprocessing
Relevant data were collected on the physical attributes of
the five landuse types, i.e. farmland, built-up areas, forest
regrowth, bare lands and water bodies, which were the
dominant landuse in the area. Sample sites for data collection
were determined from the remotely sensed imageries .For each
landuse, five sample sites measuring 100 x 100m were selected
and were fully described during field observations, variables
examined for site characterization included dominant, concrete
among others and drainage characteristics of the site . The
coordinates of the sample sites were tracked with Global
Positioning System (GPS) receiver. Secondary data used were
Landsat TM, SPOT- XS NigeriaSat-1 covering the study area.
Table 1 shows key parameters of the data used for the study.
Images were obtained from the National Centre for Remote
Sensing Jos, Forest Monitoring, Evaluation and Coordinating
Unit (FORMECU) Abuja and Global Land Cover Facility
(GLCF) an Earth Science Data Interface. The topographic map
covering the study area was collected from the Ministry of Land
and Surveys, Lagos.
The satellite data were extracted one after the other as sub
scenes from the original datasets. For the purpose of
landuse/cover assessment, a common window covering the
same geographical coordinates of the study area was extracted
from the scene of the images obtained. This made the band Red,
Blue, Green (RGB-123) colour combination. For SPOT XS
data, Channel 3 was assigned red plane, Channel 2 to green and
channel 1 to blue plane. The band combination then consisted
of Blue, Green and Red (BGR-321) colour combination. For
NigeriaSat_l data set, colour combination, channel 1 was
assigned to red plane, channel 2 to green plane and 3 to blue
plane. This puts the band combination as Red, Green and Blue
(RGB-123).
The geometric errors were corrected using ground control
points (GCP). The process of georeferencing in this study
started with the identification of features on the image data,
which can be clearly recognized on the topographical map of
the study area and whose geographical locations were clearly
defined. Stream intersections and the intersection of the
highways were used as ground control points (GCP). The
latitude and longitude of the GCPs of clearly seen features
obtained in the base map were used to register the coordinates
of the image data used for the study. All the images were
georeferenced to Universal Transverse Mercator projection of
WGS84 coordinate system, zone 31N with Clarke 1866
Spheroid. Nearest-neighbor re-sampling method was used to
correct the data geometrically.