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4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS...

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4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT REGIONAL SCALE HYDROLOGIC ANALYSIS AND MODELING OF RGG WATER RESOURCES AT REGIONAL AND TEMPORAL SCALES P. ANGELIDIS AND N. KOTSOVINOS DEPARTMENT OF CIVIL ENGINEERING DEMOCRITUS UNIVERSITY OF THRACE 67100 XANTHI, GREECE
Transcript
Page 1: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

4th MEETING SADMOSEVILLE, SPAIN, FEBRUARY 2008

WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF

GUADIANA RIVER AT REGIONAL SCALEHYDROLOGIC ANALYSIS AND MODELING OF RGG WATER

RESOURCES AT REGIONAL AND TEMPORAL SCALES

P. ANGELIDIS AND N. KOTSOVINOS

DEPARTMENT OF CIVIL ENGINEERINGDEMOCRITUS UNIVERSITY OF THRACE

67100 XANTHI, GREECE

Page 2: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

DUTH RESEARCH OBJECTIVES

• REGIONAL STATISTICAL – HYDROLOGIC ANALYSIS OF THE PRECIPITATION DATA

• WATER RESOURCES INDICATORS AT REGIONAL SCALES AND VARIOUS TIME SCALES

• TEST FOR THE APPROPRIATE PROBABILITY DENSITY DISTRIBUTION TO DERIVE THE STANDARDIZED PRECIPITATION INDEX (SPI) AT REGIONAL SCALE FOR VARIOUS TIME SCALES; KOLMOGOROV-SMIRNOV GOODNESS-OF-FIT TEST

Page 3: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

STANDARDIZED PRECIPITATION INDEX (SPI) FOR VARIOUS TIME SCALES AT MANY STATIONS COVERING THE REGION UNDER STUDY, USING THREE DIFFERENT PROBABILITY DENSITY DISTRIBUTIONS

TREND LINE OF SPI

REGIONAL STATISTICAL ANALYSIS OF TEMPERATURE AND EVAPORATION

ADDITIONAL DROUGHT INDICATORS COMBINING HYDROLOGIC, EVAPOTRANSPIRATION AND VEGETATION DATA

Page 4: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

Meteorological stations in the area under study

(Guadiana)

-9 -8.8 -8.6 -8.4 -8.2 -8 -7.8 -7.6 -7.4 -7.2 -737

37.2

37.4

37.6

37.8

38

38.2

38.4

38.6

38.8

39

ALANDROAL

ALCARIA LONGA

ALCOUTIM

ALDEIA NOVA DE SÃO BENTO

ALGODÔR

AMARELEJA

AMIEIRA

ARRONCHES

BARRANCOS

CORUJOS

HERDADE DE VALADA

JUROM ENHA

MARTIM LONGO

M ESQUITA

MINAS DE SÃO DOMINGOS

M ONTE DA PATA ESTRELA

M ONTE DA TORRE

MOURA

M ÉRTOLA

PEDROGÃO DO ALENTEJO

PEREIRO

PORTEL

REGUENGOS

SALVADA

SANTA IRIA

SANTIAGO M AIOR

SANTO ALEIXO DA RESTAURAÇÃO

SERPA

SO BRAL DA ADIÇA

VIDIGUEIRA

VILA VERDE DE FICALHO

VILA VIÇOSA

VALE DE CAM ELOS

FIGUEIRAISFARO

BEJA

SETUBAL

EVO RA

SANTAREM

PO RTALEG RE

BEJA

EVO RASETUBAL

FARO

SPAIN

Page 5: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

WE MADE TWO DIFFERENT STATISTICAL ANALYSIES FOR COMPUTATION OF THE STANDARDIZED PRECIPITATION INDEX (SPI) FOR VARIOUS TIME SCALES AT MANY STATIONS COVERING THE REGION UNDER STUDY:

The precipitation timeseries completed after correlation, but not extended. So timeseries of variant meteorologic stations have not the same time period

The precipitation timeseries completed after correlation, and extended to have all the same chronicle basis 1931 - 2007

THE RESULTS ARE QUITE DIFFERENT AS WE WILL SEE NEXT.

Page 6: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: ALDEIA NOVA DE SΓO BENTO station: 1931 - 1973

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: ALDEIA NOVA DE SΓO BENTO station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 7: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: ALDEIA NOVA DE SΓO BENTO station: 1931 - 1973

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: ALDEIA NOVA DE SΓO BENTO station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 8: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: HERDADE DE VALADA station: 1968 - 2007

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: HERDADE DE VALADA station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 9: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: MINAS DE SΓO DOMINGOS station: 1931 - 1968

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: MINAS DE SΓO DOMINGOS station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 10: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: MOURA station: 1932 - 1941

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

MONTHLY PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: MOURA station: 1931 - 2007

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

MONTHLY PRECIPITATION (mm)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 11: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure), except log-normal

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: SANTA IRIA station: 1980 - 2007

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

MONTHLY PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: SANTA IRIA station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 12: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: SOBRAL DA ADIHA station: 1980 - 2007

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: SOBRAL DA ADIΗA station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 13: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: VILA VERDE DE FICALHO station: 1980 - 1985

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

MONTHLY PRECIPITATION (mm)

CU

MU

LA

TIV

E P

RO

BA

BIL

ITY

.

DATA GAMMA LOG-NORMAL NORMAL

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: VILA VERDE DE FICALHO station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 14: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATIONSALVADA station: 1957 - 2007

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: SALVADA station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 15: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: MESQUITA station: 1980 - 2007

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: MESQUITA station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 16: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

TESTING THREE THEORETICAL CUMULATIVE PROBABILITY DISTRIBUTIONS FOR MONTHLY PRECIPITATION

Theoretical distributions seems to fit better to the larger timeseries (right figure)

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

PORTEL station: 1939 - 2007

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

CUMULATIVE PROBABILITYFOR MONTHLY PRECIPITATION

Guadiana: PORTEL station: 1931 - 2007

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)C

UM

UL

AT

IVE

PR

OB

AB

ILIT

Y

.

DATA GAMMA LOG-NORMAL NORMAL

Page 17: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

COMPARISON OF THE STANDARDIZED PRECIPITATION

INDEX SPI 12

a) Each one of the precipitation timeseries has its own chronicle basis

b) The precipitation timeseries have all the same chronicle basis 1931 - 2007

Page 18: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

ALDEIA NOVA DE SΓO BENTO station: a) 1931–1973, b) 1931–2007

SPI 12 y = 0.001x - 0.2542

-4

-3

-2

-1

0

1

2

31

93

2

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

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0005x + 0.2308

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 19: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

HERDADE DE VALADA station: a) 1968 - 2007, b) 1931–2007

SPI 12 y = 3E-05x - 0.0059

-3

-2

-1

0

1

2

31

96

9

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

20

06

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0005x + 0.2262

-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

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19

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19

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19

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19

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19

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19

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19

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19

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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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 20: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MINAS DE SΓO DOMINGOS station: a) 1931 - 1968, b) 1931–2007

SPI 12 y = 0.003x - 0.6633

-4

-3

-2

-1

0

1

2

31

93

2

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

Linear(GAMMA)

SPI 12 y = -0.0003x + 0.1309

-3

-2

-1

0

1

2

3

4

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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 21: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MONTE DA TORRE station: a) 1961 - 1971, b) 1931–2007

SPI 12 y = -0.0041x + 0.2236

-3

-2

-1

0

1

2

31

96

2

19

63

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0006x + 0.2734

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 22: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MOURA station: a) 1932 - 1941, b) 1931–2007

SPI 12 y = 0.0261x - 1.641

-2

-1

0

1

21

93

2

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0004x + 0.1877

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 23: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

SANTA IRIA station: a) 1980 - 2007, b) 1931–2007

SPI 12 y = 0.0019x - 0.2966

-3

-2

-1

0

1

2

31

98

1

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

20

06

20

07

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0005x + 0.2219

-4

-3

-2

-1

0

1

2

3

4

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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 24: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

SOBRAL DA ADIHA station: a) 1980 - 2007, b) 1931–2007

SPI 12 y = 0.0017x - 0.2687

-3

-2

-1

0

1

2

31

98

1

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

20

06

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0005x + 0.2142

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 25: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

VILA VERDE DE FICALHO station: a) 1980 - 1985, b) 1931–2007

SPI 12 y = 0.0529x - 1.3748

-3

-2

-1

0

1

2

1981

1982

1983

1984

1985

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0005x + 0.2222

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 26: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

SALVADA station: a) 1957 - 2007, b) 1931–2007

SPI 12

y = -0.0005x + 0.1505

-4

-3

-2

-1

0

1

2

31

95

8

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

20

06

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0004x + 0.1989

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 27: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MESQUITA station: a) 1980 - 2007, b) 1931–2007

SPI 12 y = -0.0003x + 0.0547

-3

-2

-1

0

1

2

31

98

1

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

20

06

20

07

GAMMA

Linear(GAMMA)

SPI 12 y = -0.0002x + 0.0816

-4

-3

-2

-1

0

1

2

3

4

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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 28: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

COMPARISON OF THE STANDARDIZED PRECIPITATION

INDEX SPI 24

a) Each one of the precipitation timeseries has its own chronicle basis

b) The precipitation timeseries have all the same chronicle basis 1931 - 2007

Page 29: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

ALDEIA NOVA DE SΓO BENTO station: a) 1931–1973, b) 1931–2007

SPI 24 y = 0.0015x - 0.3932

-4

-3

-2

-1

0

1

2

31

93

2

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

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0007x + 0.3328

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 30: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

HERDADE DE VALADA station: a) 1968 - 2007, b) 1931–2007

SPI 24

y = 0.0005x - 0.1

-3

-2

-1

0

1

2

3

41

97

0

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

20

06

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0006x + 0.3001

-3

-2

-1

0

1

2

3

4

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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 31: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MINAS DE SΓO DOMINGOS station: a) 1931 - 1968, b) 1931–2007

SPI 24 y = 0.0043x - 0.9847

-4

-3

-2

-1

0

1

2

31

93

2

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

Linear(GAMMA)

SPI 24 y = -0.0004x + 0.1652

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 32: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MONTE DA TORRE station: a) 1961 - 1971, b) 1931–2007

SPI 24

y = -0.0009x + 0.0432

-3

-2

-1

0

1

21

96

3

19

64

19

65

19

66

19

67

19

68

19

69

19

70

19

71

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0008x + 0.3682

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 33: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MOURA station: a) 1932 - 1941, b) 1931–2007

SPI 24 y = 0.0326x - 2.2491

-3

-2

-1

0

1

21

93

2

19

33

19

34

19

35

19

36

19

37

19

38

19

39

19

40

19

41

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0006x + 0.2801

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 34: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

SANTA IRIA station: a) 1980 - 2007, b) 1931–2007

SPI 24 y = 0.0022x - 0.3345

-3

-2

-1

0

1

2

31

98

2

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

20

06

20

07

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0006x + 0.2853

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 35: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

SOBRAL DA ADIHA station: a) 1980 - 2007, b) 1931–2007

SPI 24 y = 0.0019x - 0.2897

-3

-2

-1

0

1

2

31

98

2

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

20

06

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0006x + 0.2811

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 36: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

VILA VERDE DE FICALHO station: a) 1980 - 1985, b) 1931–2007

SPI 24 y = 0.0844x - 1.6876

-3

-2

-1

0

1

2

1982

1983

1984

1985

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0006x + 0.2958

-3

-2

-1

0

1

2

3

4

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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 37: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

SALVADA station: a) 1957 - 2007, b) 1931–2007

SPI 24

y = -0.0007x + 0.1957

-3

-2

-1

0

1

2

31

95

9

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

20

06

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0004x + 0.2063

-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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 38: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

MESQUITA station: a) 1980 - 2007, b) 1931–2007

SPI 24 y = -0.0012x + 0.1748

-3

-2

-1

0

1

2

31

98

2

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

20

06

20

07

GAMMA

Linear(GAMMA)

SPI 24 y = -0.0002x + 0.0785

-4

-3

-2

-1

0

1

2

3

4

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

20

06

20

07

GAMMA

Linear(GAMMA)

Page 39: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

REGIONAL DISTRIBUTION OF SPI FOR TIME SCALE EQUAL TO:

3 MONTHS 6 MONTHS12 MONTHS24 MONTHS

Page 40: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

LINEAR TREADLINE SLOPE COEFFICIENT FOR GAMMA DISTRIBUTIONOF THE SPI 3, SPI 6, SPI 12 and SPI 24

Only in 2 stations among 21 stations, possitive treadline slope appears for SPI 3, SPI 6, SPI 12 and SPI 24

Page 41: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

The slope of trend line for the SPI-3 months-9 -8.8 -8.6 -8.4 -8.2 -8 -7.8 -7.6 -7.4 -7.2 -7

37

37.2

37.4

37.6

37.8

38

38.2

38.4

38.6

38.8

39

FAR O

BEJA

SETU BAL

EVO R A

SAN TAR EM

PO R TALEG R E

BEJA

EVO RASETU BAL

FAR O

SPAIN

-0 .00042-0.0004-0.00038-0.00036-0.00034-0.00032-0.0003-0.00028-0.00026-0.00024-0.00022-0.0002-0.00018-0.00016-0.00014-0.00012-0.0001-8E-005-6E-005-4E-005-2E-00502E-0054E-0056E-0058E-0050.0001

Page 42: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

The slope of trend line for the SPI-6 months-9 -8.8 -8.6 -8.4 -8.2 -8 -7.8 -7.6 -7.4 -7.2 -7

37

37.2

37.4

37.6

37.8

38

38.2

38.4

38.6

38.8

39

FAR O

BEJA

SETU BAL

EVO R A

SAN TAR EM

PO R TALEG R E

BEJA

EVO R ASETU BAL

FAR O

SPAIN

-0.0007-0.00065-0.0006-0.00055-0.0005-0.00045-0.0004-0.00035-0.0003-0.00025-0.0002-0.00015-0.0001-5E-00505E-0050.00010.000150.00020.000250.0003

Page 43: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

The slope of trend line for the SPI-12 months-9 -8.8 -8.6 -8.4 -8.2 -8 -7.8 -7.6 -7.4 -7.2 -7

37

37.2

37.4

37.6

37.8

38

38.2

38.4

38.6

38.8

39

FAR O

BEJA

SETU BAL

EVO R A

SAN TAR EM

PO R TALEG R E

BEJA

EVO R ASETU BAL

FAR O

SPAIN

-0.0014

-0.0013

-0.0012

-0.0011

-0.001

-0.0009

-0.0008

-0.0007

-0.0006

-0.0005

-0.0004

-0.0003

-0.0002

-0.0001

0

0.0001

0.0002

0.0003

Page 44: 4th MEETING SADMO SEVILLE, SPAIN, FEBRUARY 2008 WATER RESOURCES INDICATORS AND STATISTICAL ANALYSIS OF THE HYDROLOGICAL DATA EAST OF GUADIANA RIVER AT.

The slope of trend line for the SPI-24 months-9 -8.8 -8.6 -8.4 -8.2 -8 -7.8 -7.6 -7.4 -7.2 -7

37

37.2

37.4

37.6

37.8

38

38.2

38.4

38.6

38.8

39

FAR O

BEJA

SETU BAL

EVO R A

SAN TAR EM

PO R TALEG R E

BEJA

EVO R ASETU BAL

FAR O

SPAIN

-0.0018

-0.0016

-0.0014

-0.0012

-0.001

-0.0008

-0.0006

-0.0004

-0.0002

0

0.0002

0.0004

0.0006


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