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Use of Climate-Resilient Plants in Arid and Semi-Arid Lands


            season (Atalay, 2002).  The majority of the areas where the General Directorate of
            Combating Desertification and Erosion (ÇEMGM) carries out planting activities
            are extremely arid and barren lands. Plant adaptation and implementation studies
            conducted in regions such as Ankara, Aksaray, Konya, Karaman, and Kırşehir, where
            drought is a serious problem, continue without irrigation in areas with limited
            or no irrigation facilities. In these areas, plants that experience water deficiency
            during the vegetation season undergo significant water stress. According to the
            last 60 years of data from meteorological stations between Eskişehir and Aksaray,
            water deficiency is observed in the region from May to October, showing a similar
            trend throughout this period. The Konya Basin, which is very arid and threatened
            by desertification due to wind erosion, receives approximately 300 mm of total
            annual precipitation and has an average temperature of 11°C (Yıldız et al., 2018).
            According to the Thornthwaite  Water Balance, when  comparing the Average
            Monthly Total Precipitation (mm) with the Monthly Potential Evapotranspiration
            (PET) (mm) for the Konya region, it is evident that the soil in this area experiences
            water deficiency throughout the growing season of plants (Figure 9).



























                 Figure 9: Thornthwaite water deficit balance; Konya and its surroundings
                                       (Yıldız et al., 2018).
               According to the Thornthwaite method, a water balance table for a location
            is prepared using the monthly average temperature, monthly average
            precipitation, and monthly evapotranspiration values for that location. Tables
            of the water balance, obtained by using these values, show the accumulated
            water in the soil throughout the year, the monthly variations of accumulated
            water, the annual actual evapotranspiration amounts, the water surplus in the
            soil, the water deficit, runoff, and the moisture content.


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