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Table 7 Sutluk thornthwaite water balance (Çetin 2020)

From: Topography and climate of Mount Karanfil (Pozantı/Adana)

 

J

F

M

A

M

J

J

A

S

O

N

D

An

Par

 AYT

0.5

1.9

4.5

9.1

13.2

16.6

18.7

18.6

15.8

11.4

7.0

2.9

10.02

 ASI

0.03

0.23

0.85

2.48

4.35

6.15

7.37

7.31

5.71

3.48

1.66

0.44

40.06

 DPEa

1.52

6.89

18.25

40.42

61.53

79.71

91.2

90.64

75.39

52.14

30.06

11.11

 DPE

1.38

6.06

18.8

43.25

71.37

92.46

107.62

102.42

76.9

51.1

27.05

10.0

608.41

 ATY

84.0

70.0

67.0

63.0

61.0

44.0

25.0

21.0

31.0

55.0

66.0

95.0

682.0

 BSAD

0.0

0.0

0.0

0.0

− 41.17

0.0

0.0

3.9

38.95

57.15

 Bir.Su

100.0

100.0

100.0

100.0

89.63

41.17

0.0

0.0

0.0

3.9

42.85

100.0

 Etr

1.38

6.06

18.8

43.25

71.37

92.46

66.17

21.0

31.0

51.1

27.05

10.0

439.64

 Sn

0.0

0.0

0.0

0.0

0.0

0.0

41.45

81.42

45.9

0.0

0.0

0.0

168.77

 Sf

82.62

63.94

48.2

19.75

0.0

0.0

0.0

0.0

0.0

0.0

0.0

27.85

242.36

 A

55.24

73.28

56.07

33.97

9.88

0.0

0.0

0.0

0.0

0.0

0.0

13.93

242.37

 NO

59.87

10.55

2.56

0.46

− 0.15

− 0.52

− 0.77

− 0.79

− 0.6

0.08

1.44

8.5

  1. AYT-Total monthly precipitation ASI- Monthly average temperature (ºC), ASD—Monthly temperature value, DPEa- Unadjusted PE, DPE- Adjusted PE, BSAD-Monthly accumulated water change, Bir.Su- Accumulated water-, Etr- Actual Evapotranspiration, Sn—Water shortage. Moderate water shortages are observed in the dairy during the summer season (Fig. 18). High levels of evapotranspiration during the summer may cause oxidative stress in plants, particularly affecting their physiology. The difference observed at the Sutluk station may be attributed to topographic factors, climatic changes, and emissions (Çetin 2020)