Full text: Proceedings, XXth congress (Part 7)

  
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004 
  
(Evrendilek and Doygun, 2000; Wali et al., 2002). For example, 
increasing the amount of land, water and nitrogen fertilizers 
used to meet the ever-increasing food consumption which in 
turn increases environmental degradation leads to an 
unsustainable cycle, for environmental degradation makes it 
more difficult to meet our basic human needs of food and clean 
water in the long-term (Kilic et al., 2003; Kilic et al., 2004). On 
the other hand, multi-temporal high-resolution, remotely sensed 
data and geographic information systems (GIS) have facilitated 
the derivation of ecological inventories and the monitoring of 
LULC changes on the local, regional and global scales 
(Berberoglu, 2003; Berberoglu et al., 2004). In particular, the 
visible to shortwave infrared (VSWIR) bands of Landsat 
Multispectral Scanner (MSS) and Thematic Mapper (TM) data 
have been extensively used for surveys and analyses of forest 
and agricultural resources since the initiation of Landsat 
program in 1972 (Berberoglu et al., 2000; Townshend and 
Justice, 2002). 
This study region was selected because it is located in one of 
the most biologically diverse regions as well as the most water- 
short regions of the Mediterranean Basin. There is a lack of 
quantification and identification of LULC changes in 
ecologically productive and hotspots of the study region. 
Sustainability of vital ecosystems in the region are threatened 
by increased rates of population growth, consumption and waste 
disposals, and the keen competition among LULCs for both 
rate-limited ecological services and stock-limited natural 
resources. For example, draining of the Amik lake and its 
surrounding wetlands has led to continued problems with water 
quality and quantity and escalated flood damages. Preventive 
and mitigative measures are urgently needed in the supply- and 
demand-side managements of natural resources in order to 
assure long-term productivity and health of ecosystems before 
the point of irreversible losses is reached. The main objective of 
this study was to reconstruct past LULC changes over the last 
28 years at the scale of the province of Hatay, Turkey, based on 
a time series of Landsat imagery acquired from 1972, 1987, and 
2000. 
2. MATERIALS AND METHODS 
2.1 Study Region 
The study region is located in the province of Hatay (Turkey) 
(35? 47'-36? 24' E; 35? 48'-36? 37' N) and has a total area of ca. 
3930 knY? with an elevation range from sea level up to 2100 m 
(Figure 1). The study region is delimited by the Mediterranean 
Eel TUE El 
Figure 1. Location of the study region in Turkey. 
  
Sea in the west, by Syria in the south and east, and by the 
province of Gaziantep in the east. The prevalent climate regime 
is Mediterranean climate characterized by a mild winter during 
which about 67% of the annual precipitation of 1124 mm falls, 
and a hot dry summer. Average annual temperature reaches a 
maximum of 44°C in the summer and a minimum of —15°C in 
the winter, with an average annual temperature of 18°C. Parent 
materials in the study region consist mostly of sedimentary 
rocks of highly calcareous clays, limestone, dolomites, and 
sandstones. The major soil orders include entisols, inceptisols, 
vertisols, mollisol, and alfisol (Kilic, 1999). The alluvial soils 
formed in the Amik plain by the Orontes river are the most 
productive soils covering the northeast of the study area. The 
dominant Mediterranean vegetation consists of evergreen 
forests of Pinus brutia, and shrublands composed of maquis, 
and garrigues. Regressive succession stages of evergreen forests 
have taken place under drastic human-induced disturbances 
such as overgrazing, overcutting, and clearance for cultivation. 
2.2 Data Processing 
The following remotely sensed cloud-free data were used in the 
classification of LULCs in the province of Hatay through 
ERDAS Imagine and TNTmips software: Landsat MSS of 
December 15, 1972, Landsat-5 TM of October 1, 1987, and 
Landsat-7 ETM+ of June 22, 2000. The images were 
geometrically corrected and geo-coded to the Universal 
Transverse Mercator (UTM) co-ordinate system, using 1:25 000 
scale topographic maps and aerial photographs taken in 1992. 
Approximately 45 evenly distributed ground control points 
were selected from each image. These were used to spatially 
resample the images using a nearest neighbor algorithm, which 
takes the value of the pixel in the input image that is closest to 
the computed co-ordinate. This method is fast and does not alter 
the original pixel values. The transformation had a root mean 
square (RMS) error of between 0.4 and 0.7 pixel, indicating that 
the image rectification was accurate to within one pixel. The 
acquired Landsat images were classified using a maximum 
likelihood classifier method of ERDAS Imagine and TNTmips 
software. A supervised maximum likelihood classification was 
performed with 2682, 11689 and 8107 pixel training data sets, 
and the images were classified into 6 (1987 and 2000) and 7 
(1972) LULC classes. 
3. RESULTS AND DISCUSSION 
On the basis of a time series of the Landsat images, LULCS of 
the study region was classified into seven categories: evergreen 
forest, shrublands-orchards, the Amik lake and its related 
wetlands, croplands, water bodies, settlements, and bareground 
(Table 1). The study area occupied 392,970 ha. The annual 
rates and cumulative amounts of LULC changes were estimated 
over the two periods: 1972 to 1987 (period 1), and 1987 to 2000 
(period 2). Land use/cover changes were of highest amount in 
croplands, evergreen forests, shrublands-orchards, and the 
Amik lake-related wetlands in the first period and in settlements 
and bareground in the second period. In both periods, 
bareground decreased, while croplands and settlements 
increased. In the first period, the rate of change of the Amik 
lake-its related wetlands, and shrublands-orchards was negative, 
whereas the rate of change of evergreen forests was positive. In 
the second period, a decrease in evergreen forest took place, 
whereas an increase in shrublands-orchards occurred. 
Comparisons of LULCs in 1972, 1987 and 2000 derived from 
the Landsat images indicated that the Amik lake and its 
314 
  
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Table 1. 
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Figure 2. 
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