introductory study : water indicators and statistical analysis of the hydrological data east of...

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INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos ,P. Angelidis , V. Hrissanthou , and A. Pechtelidis Democritus University of Thrace - School of Engineering Greece

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Page 1: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS

OF THE HYDROLOGICAL DATA EAST OF

GUADIANA RIVER by

Nikolas Kotsovinos ,P. Angelidis , V. Hrissanthou , and A. Pechtelidis

Democritus University of Thrace -School of Engineering

Greece

Page 2: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

PART II

SOME STATISTICAL ANALYSIS

Page 3: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION

We choose one station (AMARELEJA) to test

rigorously the standardization procedure (probability

transformation) assuming normal, log–normal, and

gamma statistics for precipitation.

Page 4: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA station: Annual precipitation for the period 1932-2005.

Mean annual precipitation = 523 mm

Standard Deviation / mean = 0.30

0

100

200

300

400

500

600

700

800

900

1931

-219

33-4

1935

-619

37-8

1939

-40

1941

-219

43-4

1945

-619

47-8

1949

-50

1951

-219

53-4

1955

-619

57-8

1959

-60

1961

-219

63-4

1965

-619

67-8

1969

-70

1971

-219

73-4

1975

-619

77-8

1979

-80

1981

-219

83-4

1985

-619

87-8

1989

-90

1991

-219

93-4

1995

-619

97-8

1999

-00

2001

-220

03-4

HYDROLOGICAL YEAR

AN

NU

AL

PR

EC

IPIT

AT

ION

(m

m)

ANNUAL PRECIPITATION (mm) MEAN ANNUAL PRECIPITATION (mm)

Page 5: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA station: Mean monthly precipitation and standard deviation for the period 1932-2005

The standard deviation is very high

MEAN MONTHLY PRECIPITATIONAMARELEJA: 1932 -2005

65

53

60

52

38

22

3 3

24

6267

73

0

10

20

30

40

50

60

70

80

JA

N

FE

B

MA

R

AP

R

MA

Y

JO

YN

JO

YL

AU

G

SE

P

OC

T

NO

V

DE

C

PR

EC

IPIT

AT

ION

(m

m)

MEAN MONTHLY PRECIPITATION AVERAGE STANDARD DEVIATION

Page 6: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA station: The ratio of (Standard deviation / Mean monthly precipitation)

for the period 1932-2005.The ratio varies from 0.65 to 2.5.

MONTHLY PRECIPITATIONAMARELEJA: 1932 -2005

0.0

0.5

1.0

1.5

2.0

2.5

JA

N

FE

B

MA

R

AP

R

MA

Y

JO

YN

JO

YL

AU

G

SE

P

OC

T

NO

V

DE

C

ST

AN

DA

RD

DE

VIA

TIO

N /

ME

AN

.

Page 7: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

Data and theoretical cumulative probability distributions formonthly precipitation at AMARELEJA station. Period 1932-2005.We tested three theoretical cumulative probability distributions:GAMMA LOG-NORMAL NORMALThe fit is not very good for the above three theoretical distributions

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

AMARELEJA 1932 - 2005

0,00

0,10

0,20

0,30

0,40

0,50

0,60

0,70

0,80

0,90

1,00

0 50 100 150 200 250 300 350

MONTHLY PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 8: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

PART III

COMPUTING SPI

Page 9: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

The SPI is computed by fitting a probability density function to the frequency distribution of precipitation summed over the time scale of interest. Each probability density function is then transformed into the standardized normal distribution.

Calculation:The monthly precipitation time series are modelled using different statistical distributions.

1. The first is the gamma distribution, whose probability density function is defined as

where

The calculations are quite complicated

2. Another possibility is the log–normal distribution. It has the advantage of simplicity since it is just a logarithmic transformation of the data, i.e. Y = ln(x) (for x > 0), with the assumption that the resulting transformed data are described by a Gaussian distribution.

Page 10: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

3. Normal distribution. The central limit theorem suggests that, as we move to extended time periods in excess of 6 months, the resultant time averaging will tend to shift the observed probability distributions towards normal. Because the gamma distribution tends towards the normal as the shape parameter α tends to infinity, it would be computationally more efficient to standardize the data directly from a fitted normal distribution.

We computed the multi-temporal SPI values by modelling the precipitation data with three different statistical distributions.

•GAMMA•LOG-NORMAL•NORMAL

We concluded, that we can use for simplicity LOG-NORMAL or NORMAL distribution instead of GAMMA producing almost the same results

Page 11: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

SPI OF 24 MONTHS

Page 12: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Data and three theoretical cumulative probability distributions

for the running sum of 24 months. The fit seems quite good for all the three theoretical distributions.

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 24 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

0 200 400 600 800 1000 1200 1400 1600 1800 2000

RUNNING SUM OF 24 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 13: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005SPI 24 for GAMMA, LOG-NORMAL and NORMAL distribution.

The results are very close

SPI 24

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05GAMMA

SPI 24

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05LOG-NORMAL

SPI 24

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

NORMAL

Page 14: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Comparison of SPI 24 for GAMMA, LOG-NORMAL

and NORMAL distribution.The results are essentially coincided

SPI 24

-4

-3

-2

-1

0

1

2

3

41

93

21

93

31

93

41

93

51

93

61

93

71

93

81

93

91

94

01

94

11

94

21

94

31

94

41

94

51

94

61

94

71

94

81

94

91

95

01

95

11

95

21

95

31

95

41

95

51

95

61

95

71

95

81

95

91

96

01

96

11

96

21

96

31

96

41

96

51

96

61

96

71

96

81

96

91

97

01

97

11

97

21

97

31

97

41

97

51

97

61

97

71

97

81

97

91

98

01

98

11

98

21

98

31

98

41

98

51

98

61

98

71

98

81

98

91

99

01

99

11

99

21

99

31

99

41

99

51

99

61

99

71

99

81

99

92

00

02

00

12

00

22

00

32

00

42

00

5

GAMMA LOG-NORMAL NORMAL

Page 15: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION: Comparison of SPI 24 for GAMMA distribution:a) Period 1932-2005b) Period 1932-1968c) Period 1969-2005

Trend in SPI values indicates that the drought conditions has changed significantly during last decades

SPI 24

-3.00

-2.00

-1.00

0.00

1.00

2.00

3.0019

3219

3319

3419

3519

3619

3719

3819

3919

4019

4119

4219

4319

4419

4519

4619

4719

4819

4919

5019

5119

5219

5319

5419

5519

5619

5719

5819

5919

6019

6119

6219

6319

6419

6519

6619

6719

6819

6919

7019

7119

7219

7319

7419

7519

7619

7719

7819

7919

8019

8119

8219

8319

8419

8519

8619

8719

8819

8919

9019

9119

9219

9319

9419

9519

9619

9719

9819

9920

0020

0120

0220

0320

0420

05

GAMMA 1932-2005 GAMMA 1932-1968 GAMMA 1969-2005 Linear (GAMMA 1932-2005)

Page 16: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

SPI OF 12 MONTHS

Page 17: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Data and three theoretical cumulative probability distributions

for the running sum of 12 months. The fit seems quite good for all the three theoretical distributions

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 12 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

0 100 200 300 400 500 600 700 800 900 1000

RUNNING SUM OF 12 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 18: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005SPI 12 for GAMMA, LOG-NORMAL and NORMAL distribution.

The results are very close

SPI 12

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

GAMMA

SPI 12

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

LOG-NORMAL

SPI 12

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05NORMAL

Page 19: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Comparison of SPI 12 for GAMMA, LOG-NORMAL and

NORMAL distribution.The results are essentially coincided

SPI 12

-4

-3

-2

-1

0

1

2

3

41

93

21

93

31

93

41

93

51

93

61

93

71

93

81

93

91

94

01

94

11

94

21

94

31

94

41

94

51

94

61

94

71

94

81

94

91

95

01

95

11

95

21

95

31

95

41

95

51

95

61

95

71

95

81

95

91

96

01

96

11

96

21

96

31

96

41

96

51

96

61

96

71

96

81

96

91

97

01

97

11

97

21

97

31

97

41

97

51

97

61

97

71

97

81

97

91

98

01

98

11

98

21

98

31

98

41

98

51

98

61

98

71

98

81

98

91

99

01

99

11

99

21

99

31

99

41

99

51

99

61

99

71

99

81

99

92

00

02

00

12

00

22

00

32

00

42

00

5

GAMMA LOG-NORMAL NORMAL

Page 20: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION:Comparison of SPI 12 for GAMMAdistribution:a) Period 1932-2005b) Period 1932-1968c) Period 1969-2005

Trend in SPI values indicates that the drought conditions has changed significantly during last years

SPI 12

-4.00

-3.00

-2.00

-1.00

0.00

1.00

2.00

3.00

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

GAMMA 1932-2005 GAMMA 1932-1968 GAMMA 1969-2005 Linear (GAMMA 1932-2005)

Page 21: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

SPI OF 6 MONTHS

Page 22: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Data and three theoretical cumulative probability distributions

for the running sum of 6 months.The fit seems quite good for all the three theoretical distributions

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 6 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

0 100 200 300 400 500 600 700

RUNNING SUM OF 6 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 23: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005SPI 6 for GAMMA, LOG-NORMAL and NORMAL distribution.

The results are to close, especially for GAMMA and LOG-NORMAL distributions

SPI 6

-5

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

GAMMA

SPI 6

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

LOG-NORMAL

SPI 6

-4

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

19

72

19

73

19

74

19

75

19

76

19

77

19

78

19

79

19

80

19

81

19

82

19

83

19

84

19

85

19

86

19

87

19

88

19

89

19

90

19

91

19

92

19

93

19

94

19

95

19

96

19

97

19

98

19

99

20

00

20

01

20

02

20

03

20

04

20

05

NORMAL

Page 24: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Comparison of SPI 6 for GAMMA, LOG-NORMAL

and NORMAL distribution.The results are essentially coincided,

especially for GAMMA and LOG-NORMAL distributions

SPI 6

-6

-5

-4

-3

-2

-1

0

1

2

3

41

93

21

93

31

93

41

93

51

93

61

93

71

93

81

93

91

94

01

94

11

94

21

94

31

94

41

94

51

94

61

94

71

94

81

94

91

95

01

95

11

95

21

95

31

95

41

95

51

95

61

95

71

95

81

95

91

96

01

96

11

96

21

96

31

96

41

96

51

96

61

96

71

96

81

96

91

97

01

97

11

97

21

97

31

97

41

97

51

97

61

97

71

97

81

97

91

98

01

98

11

98

21

98

31

98

41

98

51

98

61

98

71

98

81

98

91

99

01

99

11

99

21

99

31

99

41

99

51

99

61

99

71

99

81

99

92

00

02

00

12

00

22

00

32

00

42

00

5

GAMMA LOG-NORMAL NORMAL

Page 25: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

SPI OF 3 MONTHS

Page 26: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -2005Empirical and three theoretical cumulative probability distributions

for the running sum of 3 months. The fit is not very good for Log-normal distribution.

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 3 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

0 100 200 300 400 500 600 700

RUNNING SUM OF 3 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 27: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELESA STATION. Period 1932 -2005SPI 3 for GAMMA, LOG-NORMAL and NORMAL distribution.

The results for GAMMA and LOG-NORMAL are very close

SPI 3

-5

-4

-3

-2

-1

0

1

2

3

4

1932

1933

1934

1935

1936

1937

1938

1939

1940

1941

1942

1943

1944

1945

1946

1947

1948

1949

1950

1951

1952

1953

1954

1955

1956

1957

1958

1959

1960

1961

1962

1963

1964

1965

1966

1967

1968

1969

1970

1971

1972

1973

1974

1975

1976

1977

1978

1979

1980

1981

1982

1983

1984

1985

1986

1987

1988

1989

1990

1991

1992

1993

1994

1995

1996

1997

1998

1999

2000

2001

2002

2003

2004

2005

GAMMA

SPI 3

-4

-3

-2

-1

0

1

2

3

1932

1933

1934

1935

1936

1937

1938

1939

1940

1941

1942

1943

1944

1945

1946

1947

1948

1949

1950

1951

1952

1953

1954

1955

1956

1957

1958

1959

1960

1961

1962

1963

1964

1965

1966

1967

1968

1969

1970

1971

1972

1973

1974

1975

1976

1977

1978

1979

1980

1981

1982

1983

1984

1985

1986

1987

1988

1989

1990

1991

1992

1993

1994

1995

1996

1997

1998

1999

2000

2001

2002

2003

2004

2005

LOG-NORMAL

SPI 3

-4.00

-3.00

-2.00

-1.00

0.00

1.00

2.00

3.00

1932

1933

1934

1935

1936

1937

1938

1939

1940

1941

1942

1943

1944

1945

1946

1947

1948

1949

1950

1951

1952

1953

1954

1955

1956

1957

1958

1959

1960

1961

1962

1963

1964

1965

1966

1967

1968

1969

1970

1971

1972

1973

1974

1975

1976

1977

1978

1979

1980

1981

1982

1983

1984

1985

1986

1987

1988

1989

1990

1991

1992

1993

1994

1995

1996

1997

1998

1999

2000

2001

2002

2003

2004

2005

NORMAL

Page 28: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

CONCLUSIONS

We concluded, that we can use for simplicity LOG-NORMAL or NORMAL distribution instead of GAMMA producing almost the same results.

We had analyzed a long data series of monthly precipitation for the period 1932 – 2005. Are the above conclusion valid for sorter data series?

In order to answer this question, we made the same analysis:a) For the half data series (1932-1968)b) For the 10% of the data series, e.g. 1932 – 1939.

Page 29: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

LETS TAKE THE HALF DATA SETS 1932 - 1968

Page 30: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -1968Data and three theoretical cumulative probability distributions

for the running sum of 24 months. The fit seems quite good for all the three theoretical distributions

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 24 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

600 800 1000 1200 1400 1600 1800

RUNNING SUM OF 24 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 31: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -1968Comparison of SPI 24 for GAMMA, LOG-NORMAL

and NORMAL distribution.The SPI values are essentially coincided

SPI 24

-3

-2

-1

0

1

2

3

419

3219

3319

3419

3519

3619

3719

3819

3919

4019

4119

4219

4319

4419

4519

4619

4719

4819

4919

5019

5119

5219

5319

5419

5519

5619

5719

5819

5919

6019

6119

6219

6319

6419

6519

6619

6719

68

GAMMA LOG-NORMAL NORMAL

Page 32: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -1968Data and three theoretical cumulative probability distributions

for the running sum of 12 months. The fit is good enough for all the three theoretical distributions

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 12 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

0 100 200 300 400 500 600 700 800 900 1000

RUNNING SUM OF 12 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 33: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -1968Comparison of SPI 12 for GAMMA, LOG-NORMAL

and NORMAL distribution.The SPI values are essentially coincided

SPI 12

-3

-2

-1

0

1

2

3

19

32

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

19

42

19

43

19

44

19

45

19

46

19

47

19

48

19

49

19

50

19

51

19

52

19

53

19

54

19

55

19

56

19

57

19

58

19

59

19

60

19

61

19

62

19

63

19

64

19

65

19

66

19

67

19

68

GAMMA LOG-NORMAL NORMAL

Page 34: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

LETS TAKE ONLY 10% OF THE DATA SETS

1932 - 1939

Page 35: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -1939Data and three theoretical cumulative probability distributions

for the running sum of 12 months.The fit is not very good for all the three theoretical distributions

CUMULATIVE PROBABILITYFOR RUNNING SUM OF 12 MONTHS

0.00

0.10

0.20

0.30

0.40

0.50

0.60

0.70

0.80

0.90

1.00

0 100 200 300 400 500 600 700 800 900 1000

RUNNING SUM OF 12 MONTHS PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

Page 36: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

AMARELEJA STATION. Period 1932 -1939SPI 12 for GAMMA, LOG-NORMAL and NORMAL distribution.

The SPI values are essentially coincided

SPI 12

-3

-2

-1

0

1

2

3

1932

1933

1934

1935

1936

1937

1938

1939GAMMA

SPI 12

-3

-2

-1

0

1

2

3

1932

1933

1934

1935

1936

1937

1938

1939

LOG-NORMAL

`

SPI 12

-3

-2

-1

0

1

2

3

1932

1933

1934

1935

1936

1937

1938

1939

NORMAL

Page 37: INTRODUCTORY STUDY : WATER INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER by Nikolas Kotsovinos,P. Angelidis, V. Hrissanthou,

CONCLUSIONS

We can use for simplicity LOG-NORMAL or NORMAL distributions instead of GAMMA, producing almost the same results, especially with GAMMA and LOG-NORMAL.

This conclusion was verified not only for very long data series, but also for sorter ones.

The verification was made for SPI values of 24, 12, 6 and 3 months.?????/////