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Presentation of the 5.5
Demonstration Project
Prof. Dr. János Tamás

1st Workshop
Integrated Drought Management Programme in Central and
Eastern Europe, Slovakia
Date: 15 – 16 October 2013
Policy oriented study on remote sensing
agricultural drought monitoring methods
•
•
•
•
•

Partners of Activity
GWP HUNGARY
University of Debrecen
University of Oradea
Institute of Hydrology of the Slovak Academy of
Sciences
Key qualifications of partners
• Hungary (University of Debrecen and GWP HU):
– Applied hydrological remote sensing and GIS;
– Spatial Decision Supporting Systems
• Romania (University of Oradea):
- Geography and Integrated watershed management
• Slovakia (Institute of Hydrology of the Slovak Academy of Sciences):
- Agricultural water management, Soil hydrology
Task definition
• The drought types: meteorological, hydrological and
agricultural
• The drought indexes of meteorological and hydrological
drought parameters well-measurable and widely tested
(temperature, precipitation, humidity, water level etc.)
• The agricultural drought least quantified in soil-waterplant environment, the most uncertain drought type.
• The main objective of this case study is to formulate
concrete practical agricultural drought monitoring method
and intervention levels with calibrating for the important
crops and fruits (wheat, corn and apple)
1. Analysis of
green and
brown water
status

Finalize OUTPUT 1:
An analysis report on
the role of soil and
crop water content
status in
waterbalance within
different agricultural,
landuse and water
management
practices at rain fed
and irrigated systems
for the most important
crops and fruit (wheat,
corn and apple)

2. RS tools for
2. RS tools for
vegetation indices
vegetation
indices

3. Agricultural
3. Agricultural
drought decision
drought decision
support parameters
support
parameters

Finalize OUTPUT 3:
Report on integration of
RS and GIS tools and
intervention levels into
drought monitoring
system

Sept 2013 – Jun 2014
June 2013-Dec 2013

Finalize OUTPUT 2:
Toolbox with the concrete
identification of remote
sensing and GIS data
tools for agricultural
drought monitoring and
forecast

May 2014 – Jan 2015
Process flow of RS agricultural drought monitoring methods
Meteorological
Data
Calibration
with Drought
Index

Calibration
with available
water content

SDSS
Classification

NDVI
Time
Series

Land
use
mask

Soil Physical
Data

Calibration
with Yield
statistical
data

Plant Specific
Drought Risk
Evaluation

Watch

Varning

Alert
STUDY AREA-SITE SELECTION
The Tisa River Basin is the largest subbasin in the Danube River Basin, covering
157,186 km² (19.5%) of the Danube Basin.

Sk
Drought Risk on Hungarian Great Plain

HU
Ro
Modis Terra/Aqua
Ground res. From 250 m
36 band, Cycle: 1 d

6 Y LONG TIME SERIES of WHEAT NDVI

DROUGHT IMPACT
DROUGHT IMPACT ON NDVI BIOMASS
NDVI
Relation of NDVI Biomass and Drought YIELD LOSS
Biomass -NDVI

Relative Yield
Loss

Potential yield loss is changing in time
End result is depend on climatic, soil
condition
If we calibrate the NDVI TS with real
yield loss data and combined with soil
data, and meteorological Drought
Index, we can estimate the expected
different crops yield loss by region by
region.
Database Building
The case study will utilize the available database prepared for the Tisza River
Basin.
Crop data – Remote sensing time series
Selection of training sites
Spectral data noise filtering
Rectification (UTM system)
Cropping and mosaicing of reference area
Indexing
Statistical time series data of yields
Soil data- digital soil map
Common soil physical database of reference area
Common topology and coordinate system of reference area
Calculation of available water capacity
Calculation of water balance on watersheds
Meteorological data – Drought Index SPI,
fAPAR
Sources: USGS, ESA, Literature, Scientific reports, Publications, Media, Statistical
reports, Owner data,
Winter Wheat - Yield data sources
Winter wheat yield T/County- Tisza Hungarian region

Winter wheat –yield/ area- Hungary
Hectically yield
(Drought effect)

Same Growing Area
Source: AKI, Hungary
Automatic sensors to control soil water on East-Slovakian plan
Tisza river north watershed
Slovakian reference site
Measurements of field soil sensors

Agrometeorological data

Implemented sensor:
Groundwater level
Soil temperature
Available water content
Precipitation
Monitoring panel of soil water content
Available soil water content on remote controlled panel
Water content in different soil layers
CRISURILOR PLAIN – Romanian reference site
•

•

•
•

The Crisuri Plain is situated
in the mid part of the
Western Plain (between
Barcau and Mures rivers).
The total surface area of
the plain is 3600 sqkm.

Altitudes vary between 90180 m.
Along Barcau, Crisul Alb,
Crisul Negru, Cigher rivers.
CRISURILOR PLAIN – Meteorological data
12,5

12,5

0C

0C

Oradea

12

12

Linear (Oradea)

11,5

Holod
Linear (Holod)

11,5

11

11

10,5

10,5

10

10

9,5

9,5

9
y = 0,032x + 9,7834
R2 = 0,2155

8,5

9
y = 0,0386x + 9,6294
R2 = 0,306

8,5

8

19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

8

12

12,5
0C

12
11,5

0C

11,5

Săcueni
Linear (Săcueni)

11

11

Chişineu Criş
Linear (Chişineu Criş)

10,5

10,5
10

10

9,5

9,5

9

9
8,5

y = 0,0354x + 9,7966
2

8,5

y = 0,0164x + 9,9476
2

R = 0,0809

R = 0,2504
8
19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

8

AIR TEMPERATURE
at Oradea (up left),
Holod
(up
right),
Săcueni (down left),
Chişineu Criş (down
right)
meteorological
Station from 1975-1980
to present.
CRISURILOR PLAIN –Meteorological Data
950

mm
850

Linear (Oradea)

MEAN
ANNUAL
RAINFALL at Oradea (up
left), Holod (up right),
Săcueni
(down
left),
Chişineu Criş (down right)
meteorological Station from
1994-

mm
Holod

Oradea

Linear (Holod)

850

750
750

650

650

550

550

450
y = 0,2548x + 687,37
R2 = 0,0005

y = 1,5343x + 588,36
R2 = 0,0181

350

19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

350

a

850

19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

450

mm

800

Săcueni

950

mm

Chișineu Criş
Linear (Chișineu Criş)

Linear (Săcueni)

750

850
700

750

650
600

650

550

550

450
400

y = 2,4334x + 536
R2 = 0,0528

19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

350

b

450

y = 6,2134x + 488,47
R2 = 0,2042

350
19
71
19
73
19
75
19
77
19
79
19
81
19
83
19
85
19
87
19
89
19
91
19
93
19
95
19
97
19
99
20
01
20
03
20
05
20
07

500
CRISURILOR PLAIN LANDUSE
Nr.
crt.

Type of land use

Surface (ha)

Percentage (%)

1

Unirrigated agricultural land

193633,017

55,784

2

Secondary pastures

69458,290

20,010

3

Discontinuous urban and rural space

18086,764

5,211

4

Deciduous forests

17770,277

5,119

5

Swamps

15760,909

4,541

6

Predominant agricultural land mixed with natural vegetation

12894,911

3,715

7

Complex agricultural crops

6057,103

1,745

8

Industrial and commercial bodies

4340,424

1,250

9

Vineyards

3004,937

0,866

10

Water bodies

2367,766

0,682

11

Rivers

1246,070

0,359

12
13
14

Natural pastures
Transition shrub areas
Rice fields

563,606
548,625
372,402

0,162
0,158
0,107

15

Orchards

243,782

0,070

16

Continuous urban space

222,456

0,064

17

Airfields

136,557

0,039

18

Waste dumps

132,569

0,038

19

Recreational areas

131,535

0,038

20

Coniferous forests

76,446

0,022

Green urban areas

61,998

0,018

21

(source :Institutul Naţional de Cercetare-Dezvoltare „Delta Dunării”: http://www.indd.tim.ro) ) 100,000
347110,444
CRISURILOR PLAIN - SOIL DATA
Main soil classes
(SourceOSPA Bihor)

Main soil types
CRISURILOR PLAIN
The distribution of cernoziom soil within
Crisurilor Plain
(source, Harta Solurilor României, scale 1:
200.000, I.G.F.C.O.T., Bucureşti)
Physical Implementation of different stake holder
intervention points
- Watch: When a plant water stress is observed in sensitive
phenological phases
- Early Warning: When relevant a plant water stress is observed,
available soil moisture is close to critical, Predicted potential yield loss
<10%- Preparation to intervention
Warning: When this plant stress translates into significant biomass
damage
Potential yield loss <20%
Alert: when these two conditions are accompanied by an anomaly in
the irreversible vegetation damage Potential yield loss <30%
Catastrophe: When have to mitigate serious damages. Potential yield
loss <40%
SUMMARY
• The status of 5.5 activity based on Gantt table of
IDMP is correct
• Partners almost done data acquisition
• Further work focus on data coherency to integrate all
data
• End of this year we start the 10 years long time series
analysis (green and brown water) on reference site
THANK YOU FOR ATTENTION

1st WORKSHOP IDMP, SLOVAKIA

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IDMP CEE Activity 5.5 by Janos Tamás

  • 1. Presentation of the 5.5 Demonstration Project Prof. Dr. János Tamás 1st Workshop Integrated Drought Management Programme in Central and Eastern Europe, Slovakia Date: 15 – 16 October 2013
  • 2. Policy oriented study on remote sensing agricultural drought monitoring methods • • • • • Partners of Activity GWP HUNGARY University of Debrecen University of Oradea Institute of Hydrology of the Slovak Academy of Sciences
  • 3. Key qualifications of partners • Hungary (University of Debrecen and GWP HU): – Applied hydrological remote sensing and GIS; – Spatial Decision Supporting Systems • Romania (University of Oradea): - Geography and Integrated watershed management • Slovakia (Institute of Hydrology of the Slovak Academy of Sciences): - Agricultural water management, Soil hydrology
  • 4. Task definition • The drought types: meteorological, hydrological and agricultural • The drought indexes of meteorological and hydrological drought parameters well-measurable and widely tested (temperature, precipitation, humidity, water level etc.) • The agricultural drought least quantified in soil-waterplant environment, the most uncertain drought type. • The main objective of this case study is to formulate concrete practical agricultural drought monitoring method and intervention levels with calibrating for the important crops and fruits (wheat, corn and apple)
  • 5. 1. Analysis of green and brown water status Finalize OUTPUT 1: An analysis report on the role of soil and crop water content status in waterbalance within different agricultural, landuse and water management practices at rain fed and irrigated systems for the most important crops and fruit (wheat, corn and apple) 2. RS tools for 2. RS tools for vegetation indices vegetation indices 3. Agricultural 3. Agricultural drought decision drought decision support parameters support parameters Finalize OUTPUT 3: Report on integration of RS and GIS tools and intervention levels into drought monitoring system Sept 2013 – Jun 2014 June 2013-Dec 2013 Finalize OUTPUT 2: Toolbox with the concrete identification of remote sensing and GIS data tools for agricultural drought monitoring and forecast May 2014 – Jan 2015
  • 6. Process flow of RS agricultural drought monitoring methods Meteorological Data Calibration with Drought Index Calibration with available water content SDSS Classification NDVI Time Series Land use mask Soil Physical Data Calibration with Yield statistical data Plant Specific Drought Risk Evaluation Watch Varning Alert
  • 7. STUDY AREA-SITE SELECTION The Tisa River Basin is the largest subbasin in the Danube River Basin, covering 157,186 km² (19.5%) of the Danube Basin. Sk Drought Risk on Hungarian Great Plain HU Ro
  • 8. Modis Terra/Aqua Ground res. From 250 m 36 band, Cycle: 1 d 6 Y LONG TIME SERIES of WHEAT NDVI DROUGHT IMPACT
  • 9. DROUGHT IMPACT ON NDVI BIOMASS NDVI
  • 10. Relation of NDVI Biomass and Drought YIELD LOSS Biomass -NDVI Relative Yield Loss Potential yield loss is changing in time End result is depend on climatic, soil condition If we calibrate the NDVI TS with real yield loss data and combined with soil data, and meteorological Drought Index, we can estimate the expected different crops yield loss by region by region.
  • 11. Database Building The case study will utilize the available database prepared for the Tisza River Basin. Crop data – Remote sensing time series Selection of training sites Spectral data noise filtering Rectification (UTM system) Cropping and mosaicing of reference area Indexing Statistical time series data of yields Soil data- digital soil map Common soil physical database of reference area Common topology and coordinate system of reference area Calculation of available water capacity Calculation of water balance on watersheds Meteorological data – Drought Index SPI, fAPAR Sources: USGS, ESA, Literature, Scientific reports, Publications, Media, Statistical reports, Owner data,
  • 12. Winter Wheat - Yield data sources Winter wheat yield T/County- Tisza Hungarian region Winter wheat –yield/ area- Hungary Hectically yield (Drought effect) Same Growing Area Source: AKI, Hungary
  • 13. Automatic sensors to control soil water on East-Slovakian plan Tisza river north watershed Slovakian reference site
  • 14. Measurements of field soil sensors Agrometeorological data Implemented sensor: Groundwater level Soil temperature Available water content Precipitation
  • 15. Monitoring panel of soil water content Available soil water content on remote controlled panel Water content in different soil layers
  • 16. CRISURILOR PLAIN – Romanian reference site • • • • The Crisuri Plain is situated in the mid part of the Western Plain (between Barcau and Mures rivers). The total surface area of the plain is 3600 sqkm. Altitudes vary between 90180 m. Along Barcau, Crisul Alb, Crisul Negru, Cigher rivers.
  • 17. CRISURILOR PLAIN – Meteorological data 12,5 12,5 0C 0C Oradea 12 12 Linear (Oradea) 11,5 Holod Linear (Holod) 11,5 11 11 10,5 10,5 10 10 9,5 9,5 9 y = 0,032x + 9,7834 R2 = 0,2155 8,5 9 y = 0,0386x + 9,6294 R2 = 0,306 8,5 8 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 8 12 12,5 0C 12 11,5 0C 11,5 Săcueni Linear (Săcueni) 11 11 Chişineu Criş Linear (Chişineu Criş) 10,5 10,5 10 10 9,5 9,5 9 9 8,5 y = 0,0354x + 9,7966 2 8,5 y = 0,0164x + 9,9476 2 R = 0,0809 R = 0,2504 8 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 8 AIR TEMPERATURE at Oradea (up left), Holod (up right), Săcueni (down left), Chişineu Criş (down right) meteorological Station from 1975-1980 to present.
  • 18. CRISURILOR PLAIN –Meteorological Data 950 mm 850 Linear (Oradea) MEAN ANNUAL RAINFALL at Oradea (up left), Holod (up right), Săcueni (down left), Chişineu Criş (down right) meteorological Station from 1994- mm Holod Oradea Linear (Holod) 850 750 750 650 650 550 550 450 y = 0,2548x + 687,37 R2 = 0,0005 y = 1,5343x + 588,36 R2 = 0,0181 350 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 350 a 850 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 450 mm 800 Săcueni 950 mm Chișineu Criş Linear (Chișineu Criş) Linear (Săcueni) 750 850 700 750 650 600 650 550 550 450 400 y = 2,4334x + 536 R2 = 0,0528 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 350 b 450 y = 6,2134x + 488,47 R2 = 0,2042 350 19 71 19 73 19 75 19 77 19 79 19 81 19 83 19 85 19 87 19 89 19 91 19 93 19 95 19 97 19 99 20 01 20 03 20 05 20 07 500
  • 19. CRISURILOR PLAIN LANDUSE Nr. crt. Type of land use Surface (ha) Percentage (%) 1 Unirrigated agricultural land 193633,017 55,784 2 Secondary pastures 69458,290 20,010 3 Discontinuous urban and rural space 18086,764 5,211 4 Deciduous forests 17770,277 5,119 5 Swamps 15760,909 4,541 6 Predominant agricultural land mixed with natural vegetation 12894,911 3,715 7 Complex agricultural crops 6057,103 1,745 8 Industrial and commercial bodies 4340,424 1,250 9 Vineyards 3004,937 0,866 10 Water bodies 2367,766 0,682 11 Rivers 1246,070 0,359 12 13 14 Natural pastures Transition shrub areas Rice fields 563,606 548,625 372,402 0,162 0,158 0,107 15 Orchards 243,782 0,070 16 Continuous urban space 222,456 0,064 17 Airfields 136,557 0,039 18 Waste dumps 132,569 0,038 19 Recreational areas 131,535 0,038 20 Coniferous forests 76,446 0,022 Green urban areas 61,998 0,018 21 (source :Institutul Naţional de Cercetare-Dezvoltare „Delta Dunării”: http://www.indd.tim.ro) ) 100,000 347110,444
  • 20. CRISURILOR PLAIN - SOIL DATA Main soil classes (SourceOSPA Bihor) Main soil types
  • 21. CRISURILOR PLAIN The distribution of cernoziom soil within Crisurilor Plain (source, Harta Solurilor României, scale 1: 200.000, I.G.F.C.O.T., Bucureşti)
  • 22. Physical Implementation of different stake holder intervention points - Watch: When a plant water stress is observed in sensitive phenological phases - Early Warning: When relevant a plant water stress is observed, available soil moisture is close to critical, Predicted potential yield loss <10%- Preparation to intervention Warning: When this plant stress translates into significant biomass damage Potential yield loss <20% Alert: when these two conditions are accompanied by an anomaly in the irreversible vegetation damage Potential yield loss <30% Catastrophe: When have to mitigate serious damages. Potential yield loss <40%
  • 23. SUMMARY • The status of 5.5 activity based on Gantt table of IDMP is correct • Partners almost done data acquisition • Further work focus on data coherency to integrate all data • End of this year we start the 10 years long time series analysis (green and brown water) on reference site
  • 24. THANK YOU FOR ATTENTION 1st WORKSHOP IDMP, SLOVAKIA