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The Second Symposium 20th Mar 2012


 Conflict on Water Resources
Development between Multiple
Nations in the Nile River Basin
              ○ Masahiro ABE1, Kenji TANAKA2, Toshiharu KOJIRI2,
                         Toshio HAMAGUCHI2 , and Tetsuya SUMI2
                       1Dept. of Urban Management, Kyoto University

             2Water resources Research Center, DPRI, Kyoto University




                                                                  1
The Second Symposium 20th Mar 2012

           Contents
1. Background
2. Methodology
3. Verification
4. Assessment of future climate
5. Water Resources Development
6. Conclusion
7. Database                            2
Background



             3
100

                                                                                                                      Background and purpose
                                                                                                                                      Brundi                               Ethiopia




                                                                     (Irrigated area) / (Irrigation potential) (%)
                                                                                                                     90
                                                                                                                                      Egypt                                Eritoria
                                                                                                                     80               Kenya                                Rwanda
                                                                                                                     70               Sudan and S.Sudan                    Tanzania
                                                                                                                                      Uganda
                                                                                                                     60
1. The Nile River crosses borders among 11 countries.
                50
                40
   Dependency30ratio in Egypt is 96.9%
                                                                                                                     20
                                                                     100
             Dependency ratio of total renewal water resources (%)



                                                                                                                     10            96.9
2. Observed discharge to Aswan High Dam is 72(Gt/year),
                0
             80 1900
                     77.3
                       1920 1940 1960 1980 2000
   Agricultural water use in Egypt is 59(Gt/year)
                                                                         60

                                                                                                                                                         40.9
3. According to aquastat (FAO), irrigated area has been
              40               33.1

   increased since 1980. In the end of 21st century, water
              20
   demand is supposed to be more8.2  than supply
                                              10.1
                                                                                                                                              0                                         0        0
                                                                                                            0




                                                                                                                                                                                                          Tanza…
                                                                                                                                                                               D.R.C…
                                                                                                                                              Ethiopia

                                                                                                                                                          Uganda




                                                                                                                                                                                                 Brundi
                                                                                                                                      Sudan
                                                                                                                           Egypt




                                                                                                                                                                   Kenya




                                                                                                                                                                                        Rwanda

Identifying water shortage problem in the Nile and trying to solve it
Uniqueness of this research

To propose Hybrid of Conflict Analysis and Hydrological Model
                  The previous conflict analysis                  This method
Preference        From knowledge and               Based on output of hydrological model in
order             assumption of researcher         each scenario
Common            Capable to make sure the consequence logically in the case when subjects
advantage         make decision based on rational standard.


Disadvantage      Results are strongly             Capable to analyze with repeatability and
of the previous   influenced by qualitative        quantitative discussion due to objective
& uniqueness      expression                       decision making of preference order


Conclusion part Qualitative discussion             Qualitative and quantitative discussion


 For contribution to decision making in international river basin management
Methodology



              6
Procedure
                                1. Geographical data
                      (altitude, land-cover, routine-network)
2. Meteorological data               3. GCM output          4. Set scenarios
                                                                                Input
      GPCC, GSMaP etc                 MRI-AGCM              Irrigated area
       (1981-2004)                   (2075-2099)             (2075-2099)
                           Bias
                        Collection



                               SiBUC & Hydro-BEAM                              Simulation



         Discharge                       Runoff                  Runoff
        (1981-2004)                   (Scenario #1)           (Scenario #n)     Output

  Calibration

          Observed
       discharge data
        (1998-2002)                             Conflict Analysis              Discussion
Remote Sensing and GCM




                                                                  8
(bougria-tif.blogspot.com)   (Citation: Japan Meteorological Agency)
Input data
    Product            Parameter         Spatial resolution   Time resolution
    SRTM30              Altitude            30 seconds               -
   GLCC ver.2          land cover           30 seconds               -
  ECOCLIMAP               Soil              30 seconds               -
SPOTVEGETATION           NDVI               30 seconds               -
     GPCC             Precipitation         1.0 degree            Monthly
                                           0.1 degree &
    GSMaP             Precipitation                               Hourly
                                           0.25 degree
                      Temperature,
      H08                                   0.5 degree             Daily
                   Radiation, Humidity
                    Wind speed, Air          1.1 degree
JRA25 Reanalysis                                                  6 hours
                       pressure             (horizontal)
  MRI-AGCM          Meteorological 7      0.1875 degree
                                                              Hourly & 3 hours
   (Japan)            parameters             (20km)
SiBUC & Hydro-BEAM




                     10
Land Scheme Model SiBUC (Simple Biosphere Model including Urban Canopy)
                                                                                                                                                (Tanaka, K., 2004)
                               Categorize land surface into green, urban, and water body and
                              calculate water balance, radiation balance, and energy balance.
                                    Boundary conditions are 7 meteorological elements
                                       and 16 parameters are calculated every 1 hour
                      Boundary Condition: Tm em um FL,m(0) Ft,d(0) P
                                             Zm (Reference Height)
                                                                       Mc
Tbr          Mbr                                       Tc




                                                                                     Water level
                                                                  Canopy
               Tbw

  Urban
  Canopy                                                  Mg Tg
                    Mug     Tug                                             Ground
                                    Twb                           W1 Surface Layer                     Stage1         Stage2           Stage3       Stage4      Stage5
                   Urban
                   Ground
                                           Tdw           Tdg      W2 Root Zone                     Irrigation             Maximum water level        Minimum water level
       Tdu
                                       Water                                                       Drainage               Optimal water level        Present water level
                                       Body                       W3 Recharge Zone
                                                                                                   Precipitation



                     Schematic image of SiBUC                                                                      Scheme of irrigation in SiBUC


       Capable to estimate irrigated water requirement seasonally
                                                                                                                                                                 11
Outputs of SiBUC January (1998~2002)
Outputs of SiBUC February (1998~2002)
Outputs of SiBUC   March   (1998~2002)
Outputs of SiBUC   April   (1998~2002)
Outputs of SiBUC   May   (1998~2002)
Outputs of SiBUC   June   (1998~2002)
Outputs of SiBUC   July   (1998~2002)
Outputs of SiBUC August   (1998~2002)
Outputs of SiBUC September (1998~2002)
Outputs of SiBUC October (1998~2002)
Outputs of SiBUC November (1998~2002)
Outputs of SiBUC December (1998~2002)
Distributed Runoff Model Hydro-BEAM
                                  (Hydrological River Basin Environmental Assessment Model)
                                                                 Nile delta
                                                                                                    (Kojiri, T., 2006)

Convert outputs of SiBUC to Hydro-BEAM.
 Flow direction is determined by Altitude.
                                                                  Aswan



                                                         Khartoum                                      Atbara
                   Calculate discharge

                                                                                                       Sennar
     Kinematic wave model
                                                                                                       Roseires
                 Surface runoff                 Bahr El-Ghazal
                                                                                               Sobat
 Infiltration                                            Bahr El-Jabal

                                                                                              Lake Victoria
       Sub-surface runoff

    Linear storage model

                Schematic image of Hydro-BEAM
Conflict Analysis



                    25
What is “conflict analysis”?


  Conflict analysis is an analytical method which is developed
            expanding algorithm of metagame theory*
                                                Fraser and Hipel (1979)

Conflict analysis consists of three elements…           Howard (1971)

1. (Player) subject to play game
2. (Option) choice of player
3. (Preference) priority of option


   Results show what kinds of events are possible to occur.
                                                                     26
Algorithm of conflict analysis with example

                Stability Table (with third party)
        (r: rational, s: sequential stability, u: unstable)
Egypt                    ×    ×    E    ×    E    ×    ×    ×    ×    ×    ×   ×   ×   ×   ×
                                                                                                         START
Total stability           r   r    r    r    r    u    u    u    u    u    u   u   u   u   u

Player's stability        3   6    9    12   15   2    5    8    11   14   1   4   7   10 13              UI from          NO
                                                                                                       outcome q for               q is rational for A (r)
Preference vector                                 3    6    9    12   15   3   6   9   12 15             player A?

                                                                                                                YES
Unilateral improvement                                                     2   5   8   11 14
                                                                                                          UI for B         NO
                                                                                                        from A’s UI?              q is unstable for A (u)
Ethiopia
                                                                                                                YES
Player's stability        r   r    r    u    u    u    r    r    r    u    u   u   u   u   u               All UIs                      (Check for
                                                                                                      for B preferred to          simultaneous stability)
Preference vector         7   8    9    4    5    6    13   14   15   1    2   3   10 11 12                q by A?         YES
                                                                                                                 NO
Unilateral improvement                  7    8    9                   7    8   9   13 14 15
                                                                                                         Another UI                  q is sequentially
                                                                                                        from q for A?                 stable for A (s)
                                                                      4    5   6               YES                         NO

Others

Player's stability        r   r    r    r    r    r    u    u    u    u    u   u   r   r   r
                                                                                                     A(B): Player A(B)                                       END
                                                                                                     q: Event
Preference vector        10   11   12   13   14   15   1    2    3    4    5   6   7   8   9         UI: Unilateral Improvement

Unilateral improvement                                 10   11   12   13 14 15



                                                                                                                                                             27
Algorithm of conflict analysis with example

                Stability Table (with third party)
        (r: rational, s: sequential stability, u: unstable)
Egypt                    ×    ×    E    ×    E    ×    ×    ×    ×    ×    ×   ×   ×   ×   ×

Total stability           r   r    r    r    r    u    u    u    u    u    u   u   u   u   u

Player's stability        3   6    9    12   15   2    5    8    11   14   1   4   7   10 13

Preference vector                                 3    6    9    12   15   3   6   9   12 15

Unilateral improvement                                                     2   5   8   11 14

Ethiopia

Player's stability        r   r    r    u    u    u    r    r    r    u    u   u   u   u   u

Preference vector         7   8    9    4    5    6    13   14   15   1    2   3   10 11 12

Unilateral improvement                  7    8    9                   7    8   9   13 14 15

                                                                      4    5   6

Others

Player's stability        r   r    r    r    r    r    u    u    u    u    u   u   r   r   r

Preference vector        10   11   12   13   14   15   1    2    3    4    5   6   7   8   9

Unilateral improvement                                 10   11   12   13 14 15



  Coding for automatic analysis                                                                28
Verification in the Nile Basin



                                 29
Discharge at Aswan High Dam D.S. (m3/s)        12,000

                                               11,000
                                                                                                                                0
                                                                                                                                                                                  Error bar means max and min                                                    12,000

                                                                                                                                                                                                                                                                 11,000
                                                                                                                                                                                                                                                                                                                                                       0


                                                              Simulation_mean                                                                                                     value




                                                                                                                                                                                                                               Discharge at Atbara D.S. (m3/s)
                                               10,000                                                                           100                                                                                                                              10,000              Simulation_mean                                                   100




                                                                                                                                                                                                                                                                                                                                                                      Rainfall at the basin (mm/month)
                                                                                                                                              Rainfall at the basin (mm/month)
                                                              Observation_max
                                                9,000                                                                                                                                                                                                             9,000              Observation_max
                                                              Observation_mean                                                                                                                                                                                                       Observation_mean
                                                8,000                                                                           200                                                                                                                               8,000                                                                                200
                                                              Observation_min                                                                                                                                                                                                        Observation_min
                                                7,000                                                                                                                                                                                                             7,000

                                                6,000                                                                           300                                                                                                                               6,000                                                                                300

                                                5,000                                                                                                                                                                                                             5,000

                                                4,000                                                                           400                                                                                                                               4,000                                                                                400

                                                3,000                                                                                                                                                                                                             3,000

                                                2,000                                                                           500                                                                                                                               2,000                                                                                500

                                                1,000                                                                                                                             Aswan D.S.                                                                      1,000

                                                   0
                                                        Jan   Feb   Mar   Apr   May   Jun   Jul   Aug   Sep   Oct   Nov   Dec
                                                                                                                                600                                                                  Atbara                                                              0
                                                                                                                                                                                                                                                                              Jan    Feb   Mar   Apr   May   Jun   Jul   Aug   Sep   Oct   Nov   Dec
                                                                                                                                                                                                                                                                                                                                                       600




                                               12,000                                                                           0                                                                                                                            12,000                                                                                    0

                                                                                                                                                                                  Aswan U.S.
     Discharge at Aswan High Dam U.S. (m3/s)




                                               11,000                                                                                                                                                                                                        11,000




                                                                                                                                                                                                                    Discharge at Sennar Dam D.S. (m3/s)
                                                              Simulation_mean
                                               10,000                                                                           100                                                                                                                          10,000                 Simulation_mean                                                    100
                                                              Observation_max




                                                                                                                                               Rainfall at the basin (mm/month)




                                                                                                                                                                                                                                                                                                                                                             Rainfall at the basin (mm/month)
                                                9,000
                                                              Observation_mean                                                                                                                                                                                   9,000              Observation_max
                                                8,000         Observation_min                                                   200                                                                                                                              8,000              Observation_mean                                                   200

                                                7,000                                                                                                                                                                                                            7,000              Observation_min
                                                6,000                                                                           300                                                                                                                              6,000                                                                                 300

                                                5,000                                                                                                                                               Sennar                                                       5,000

                                                4,000                                                                           400                                                                                                                              4,000                                                                                 400

                                                3,000                                                                                                                                                                                                            3,000

                                                2,000                                                                           500                                                                                                                              2,000                                                                                 500

                                                1,000                                                                                                                                                                                                            1,000
                                                   0                                                                            600                                                                                                                                 0                                                                                  600
                                                        Jan   Feb   Mar   Apr   May   Jun   Jul   Aug   Sep   Oct   Nov   Dec                                                                                                                                                Jan    Feb    Mar   Apr   May   Jun   Jul   Aug   Sep   Oct   Nov   Dec




                                                                                                                                                                                                                                                            12,000                                                                                     0




                                                                                                                                                                                                                Discharge at Roseires Dam D.S. (m 3/s)
                                                                                                                                                                                                                                                            11,000
                                                                                                                                                                                                    Roseires                                                10,000                                                                                     100
                                               12,000                                                                           0




                                                                                                                                                                                                                                                                                                                                                             Rainfall at the basin (mm/month)
                                                                                                                                                                                                                                                                 9,000              Simulation_mean
  Discharge at Owen Falls Dam D.S. (m3/s)




                                               11,000
                                                                                                                                                                                                                                                                 8,000
                                                                                                                                                                                                                                                                                    Observation_max                                                    200
                                               10,000                                                                           100                                                                                                                                                 Observation_mean
                                                                                                                                      Rainfall at the basin (mm/month)




                                                                                                                                                                                                                                                                 7,000
                                                9,000                                                                                                                                                                                                                               Observation_min
                                                                                                                                                                                                                                                                 6,000                                                                                 300
                                                8,000                                                                           200
                                                              Simulation_mean                                                                                                                                                                                    5,000
                                                7,000
                                                              Observation_max                                                                                                                                                                                    4,000                                                                                 400
                                                6,000                                                                           300
                                                              Observation_mean                                                                                                                                                                                   3,000
                                                5,000
                                                              Observation_min                                                                                                                                                                                    2,000                                                                                 500
                                                4,000                                                                           400
                                                                                                                                                                                                                                                                 1,000
                                                3,000
                                                                                                                                                                                                                                                                    0                                                                                  600
                                                2,000                                                                           500
                                                                                                                                                                                    Owen Falls                                                                               Jan    Feb    Mar   Apr   May   Jun   Jul   Aug   Sep   Oct   Nov   Dec

                                                1,000

                                                   0                                                                            600
                                                        Jan   Feb   Mar   Apr   May   Jun   Jul   Aug   Sep   Oct   Nov   Dec
                                                                                                                                                                                                                Error is around less than 10 %
Assessment of future climate
by MRI-AGCM and CMIP3



                               31
Impact assessment of climate change by MRI-AGCM and CMIP3
               GCM* in the world                                  (2075~2099)/(2003~1979) Ave. Monthly
multi-model               A1B                           DJF
Number   Model Name       Resl. x      Resl. y        Country
  1        BCC-CM1         192           96            China
  2      BCCR-BCM2.0       128           64           Norway
  3         CCSM3          256          128             USA
  4     CGCM3.1(T47)        96           48           Canada
  5     CGCM3.1(T63)       128           64           Canada
  6       CNRM-CM3         128           64            France
  7      CSIRO-Mk3.0       192           96          Australia
  8      CSIRO-Mk3.5       192           96          Australia
  9    ECHAM5/MPI-OM       192           96          Germany
  10        ECHO-G          96           48      Germany/Korea
  11     FGOALS-g1.0       128           60            China
  12      GFDL-CM2.0       144           90             USA
  13      GFDL-CM2.1       144           90             USA                                       [-]
  14       GISS-AOM         90          (Citation: IPCCUSA WG1)
                                         60              AR4
  15        GISS-EH         72           46             USA       (2075~2099)–(2003~1979) Ave. Monthly
  16        GISS-ER         72           46             USA
  17       INGV-SXG        320          160             Italy
  18      INM-CM3.0         72           45            Russia
  19       IPSL-CM4         96           72            France
  20    MIROC3.2(hires)    320          160            Japan
  21   MIROC3.2(medres)    128           64            Japan
  22    MRI-CGCM2.3.2      128           64            Japan
  23          PCM          128           64             USA
  24    UKMO-HadCM3         96           73              UK
  25   UKMO-HadGEM1        192          145              UK
  26    MRI-AGCM3.1S       1920         960            Japan
  27    MRI-AGCM3.2S       1920         960            Japan
                                    *GCM: Global Climate Model
                                     (Citation: IPCC AR4 WG1)                                     [℃]
Study of drought year by MRI-AGCM and CMIP3

                               Utilization of 24 GCM, 485 yearly samples,
                           by MRI-AGCM(2075-2099) and CMIP3(2080-2099)
                          600

                          500                                                             Table. Drought year (yr) in the Nile Basin
Precipitation (mm/year)




                                                                                     Drought year Precipitation (mm/year) Total Runoff (Gt/year)
                          400
                                                                                       Average
                                                                                                           369.3                  207.3
                          300
                                                                                     precipitation
                                                                                      5yr drought          340.9                  188.6
                          200                                                        10yr drought          329.2                  180.8
                                                                                     20yr drought          317.0                  172.8
                          100                                                        50yr drought          305.9                  165.4
                                                                                    100yr drought          294.2                  157.7
                           0
                                0     100      200       300       400        500

                                                                                                     Input of conflict analysis
                                    Ave. 平均降水量
                                         precipitation     10yr  50yr
                                                         10年渇水 50年渇水
                                                5年渇水
                                               5yr drought      20年渇水
                                                               20yr drought    100年渇水
                                                                                100yr drought
Water Resources Development
 in the end of 21st century




                              34
Setting of scenarios (basic elements)

1. 4 players
  ① Egypt, ② Sudan&S.Sudan, ③ Ethiopia,
  ④ Upstream countries in the White Nile

2. 11 options
  Use residual irrigated area on 0%, 10%, … ,100% (11 ways)

3. 2 preference orders
  ① Amount of water use
  ② Residual amount of water in the Nile River

                 Total scenarios:14641 events             35
Water use depending on ratio of expanded irrigation area
                                     100
                                                      Egypt        Sudan&S.
                                                                          Sudan    Ethi a
                                                                                      opi   U pstream countri
                                                                                                            es
                                             90
            Calculated water use (Gt/year)
                                             80
               算定灌漑水使用量 (Gt/year)


                                             70

                                             60

                                             50

                                             40

                                             30

                                             20

                                             10

                                             0
                                                  0   10      20      30   40     50   60   70     80    90      100
                                                              Ratio of expanded irrigation area (%)
                                                                          農業開発度(%)


Calculate requirement for irrigation by hydrological model outputs. If water
    use is more than total runoff (supply), the events are unfeasible.
                                                                                                                       36
100
                                                                                             Analysis 1
Ratio of irrigated water resources development (%)
                                                                                        Egypt
                                                     90
                                                                                        Sudan&S.Sudan
                                                     80
                                                           Averaged ratio of expanded irrigated area of equilibriums
                                                                               Ethiopia
                                                     70                in eachUpstream countries
                                                                                return period of drought
                                                                               MEAN
                                                     60                                                                                               (Unit: %)
                                                     50                        5yr drought      10yr drought       20yr drought   50yr drought   100yr drought

                                                     40         Egypt              54               60                 46             38              51
                                                     30 Sudan&S.Sudan              52               57                 44             37              47
                                                     20        Ethiopia            70               49                 40             30              17
                                                     Upstream
                                                     10            countries       54               52                 50             47              46
                                                      0        Average             57.5    54.5                       45.0           38.0           40.3
                                                           0       1    2
                                                                  5yr 10yr       3      4  5
                                                                               20yr 50yr 100yr                 6

                                                     The numbers in table indicate “the average of situation which
                                                     is possible to occur”.
                                                     As a result, in the case that all basin countries develop 40%
                                                     of remained potential field for irrigated area, some discussion
                                                     will be required on the water allocation for 20 years drought
                                                     situation.
Analysis 2 ~Visualization of equilibrium points~

              Definition of quadrants                         Visualize the end of vectors
1.5                                                           1.5
              2

  1                                                             1
                        2                     1
0.5      (Sudan&S.Sudan)                (Egypt)               0.5


  0                                                             0


                                                              -0.5
-0.5

                        3                     4
                                       (Upstream               -1
 -1
                  (Ethiopia)
                                       countries)
-1.5                                                          -1.5
       -1.5        -1       -0.5   0    0.5       1   1.5            -1.5   -1   -0.5   0   0.5   1   1.5



                  Set 4 axes for each player                Unit: ratio of expanded irrigated area
Analysis 2 ~Visualization of equilibrium points~

20 years drought             100 years drought




                         According to distribution map, Egyptian side
                            has substantial advantage rapidly, and
                         Ethiopian side has remarkable disadvantage
Analysis 3 ~Refinement~

Take off events whose difference between maximum and minimum
                      ratio is more than 70%

     20 years drought               100 years drought
Analysis 3 ~Refinement~
           After 70% refinement
                                                                                    5yr drought         10yr drought                                                          20yr drought     50yr drought      100yr drought

                                                                Egypt                   66                    59                                                                  41                30                   29
                                                      Sudan&S.Sudan                     63                    56                                                                  37                28                   25
                                                               Ethiopia                 62                    48                                                                  43                34                   25
                                                     Upstream countries                 60                    54                                                                  45                37                   36
                                                               Average                  62.6                54.6                                                                  41.2              32.3                 28.8




                                                                                                                   Ratio of irrigated water resources development (%)
                                                     100                                                                                                                100
Ratio of irrigated water resources development (%)




                                                                                         Egypt                                                                                                                Egypt
                                                      90                                                                                                                90
                                                                                         Sudan&S.Sudan                                                                                                        Sudan&S.Sudan
                                                      80                                 Ethiopia                                                                       80                                    Ethiopia

                                                      70                                 Upstream countries                                                             70                                    Upstream countries
                                                                                         MEAN                                                                                                                 MEAN
                                                      60                                                                                                                60

                                                      50                                                                                                                50

                                                      40                                                                                                                40

                                                      30                                                                                                                30

                                                      20                                                                                                                20

                                                      10                                                                                                                10

                                                       0                                                                                                                 0
                                                           0      5yr
                                                                   1      10yr
                                                                            2    20yr
                                                                                  3     50yr
                                                                                         4          100yr
                                                                                                      5       6                                                               0      1
                                                                                                                                                                                    5yr        2
                                                                                                                                                                                             10yr     3
                                                                                                                                                                                                     20yr      4
                                                                                                                                                                                                              50yr         5
                                                                                                                                                                                                                         100yr     6
Conclusion

1. Hybrid of Conflict Analysis and Hydrological Model is
   proposed and applied to the whole Nile River Basin
   for international river management.
2. Assessment of future climate is conducted in each
   sub-basin by MRI-AGCM and CMIP3.
3. Plural equilibrium points are analyzed. As a result, in
   the case of 20 years drought situation, 40% of
   remained potential field for irrigated area is
   recommended as the maximum ratio for all basin
   countries. These recommended ratio depends on
   cooperative return period of drought.                  42
Database of JE-HydroNet




                          43
Database of JE-HydroNet (tentative)
Database of JE-HydroNet (tentative)
Summary of database

1. Purposes
 (1) To introduce JE-HydroNet project to the public
 (2) To share hydrological information between project members
2. Contents
  (1) Introduction of JE-HydroNet
 (2) Announcement of next symposium
 (3) Reports of the previous symposium
 (4) Download data (only for project members)
3. How to manage this website
  (1) Need to discuss for the near future
                                                                  45
                                            Thank you for kind attention.

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Masahiroabe..Nile .River basin Crisis

  • 1. The Second Symposium 20th Mar 2012 Conflict on Water Resources Development between Multiple Nations in the Nile River Basin ○ Masahiro ABE1, Kenji TANAKA2, Toshiharu KOJIRI2, Toshio HAMAGUCHI2 , and Tetsuya SUMI2 1Dept. of Urban Management, Kyoto University 2Water resources Research Center, DPRI, Kyoto University 1
  • 2. The Second Symposium 20th Mar 2012 Contents 1. Background 2. Methodology 3. Verification 4. Assessment of future climate 5. Water Resources Development 6. Conclusion 7. Database 2
  • 4. 100 Background and purpose Brundi Ethiopia (Irrigated area) / (Irrigation potential) (%) 90 Egypt Eritoria 80 Kenya Rwanda 70 Sudan and S.Sudan Tanzania Uganda 60 1. The Nile River crosses borders among 11 countries. 50 40 Dependency30ratio in Egypt is 96.9% 20 100 Dependency ratio of total renewal water resources (%) 10 96.9 2. Observed discharge to Aswan High Dam is 72(Gt/year), 0 80 1900 77.3 1920 1940 1960 1980 2000 Agricultural water use in Egypt is 59(Gt/year) 60 40.9 3. According to aquastat (FAO), irrigated area has been 40 33.1 increased since 1980. In the end of 21st century, water 20 demand is supposed to be more8.2 than supply 10.1 0 0 0 0 Tanza… D.R.C… Ethiopia Uganda Brundi Sudan Egypt Kenya Rwanda Identifying water shortage problem in the Nile and trying to solve it
  • 5. Uniqueness of this research To propose Hybrid of Conflict Analysis and Hydrological Model The previous conflict analysis This method Preference From knowledge and Based on output of hydrological model in order assumption of researcher each scenario Common Capable to make sure the consequence logically in the case when subjects advantage make decision based on rational standard. Disadvantage Results are strongly Capable to analyze with repeatability and of the previous influenced by qualitative quantitative discussion due to objective & uniqueness expression decision making of preference order Conclusion part Qualitative discussion Qualitative and quantitative discussion For contribution to decision making in international river basin management
  • 7. Procedure 1. Geographical data (altitude, land-cover, routine-network) 2. Meteorological data 3. GCM output 4. Set scenarios Input GPCC, GSMaP etc MRI-AGCM Irrigated area (1981-2004) (2075-2099) (2075-2099) Bias Collection SiBUC & Hydro-BEAM Simulation Discharge Runoff Runoff (1981-2004) (Scenario #1) (Scenario #n) Output Calibration Observed discharge data (1998-2002) Conflict Analysis Discussion
  • 8. Remote Sensing and GCM 8 (bougria-tif.blogspot.com) (Citation: Japan Meteorological Agency)
  • 9. Input data Product Parameter Spatial resolution Time resolution SRTM30 Altitude 30 seconds - GLCC ver.2 land cover 30 seconds - ECOCLIMAP Soil 30 seconds - SPOTVEGETATION NDVI 30 seconds - GPCC Precipitation 1.0 degree Monthly 0.1 degree & GSMaP Precipitation Hourly 0.25 degree Temperature, H08 0.5 degree Daily Radiation, Humidity Wind speed, Air 1.1 degree JRA25 Reanalysis 6 hours pressure (horizontal) MRI-AGCM Meteorological 7 0.1875 degree Hourly & 3 hours (Japan) parameters (20km)
  • 11. Land Scheme Model SiBUC (Simple Biosphere Model including Urban Canopy) (Tanaka, K., 2004) Categorize land surface into green, urban, and water body and calculate water balance, radiation balance, and energy balance. Boundary conditions are 7 meteorological elements and 16 parameters are calculated every 1 hour Boundary Condition: Tm em um FL,m(0) Ft,d(0) P Zm (Reference Height) Mc Tbr Mbr Tc Water level Canopy Tbw Urban Canopy Mg Tg Mug Tug Ground Twb W1 Surface Layer Stage1 Stage2 Stage3 Stage4 Stage5 Urban Ground Tdw Tdg W2 Root Zone Irrigation Maximum water level Minimum water level Tdu Water Drainage Optimal water level Present water level Body W3 Recharge Zone Precipitation Schematic image of SiBUC Scheme of irrigation in SiBUC Capable to estimate irrigated water requirement seasonally 11
  • 12. Outputs of SiBUC January (1998~2002)
  • 13. Outputs of SiBUC February (1998~2002)
  • 14. Outputs of SiBUC March (1998~2002)
  • 15. Outputs of SiBUC April (1998~2002)
  • 16. Outputs of SiBUC May (1998~2002)
  • 17. Outputs of SiBUC June (1998~2002)
  • 18. Outputs of SiBUC July (1998~2002)
  • 19. Outputs of SiBUC August (1998~2002)
  • 20. Outputs of SiBUC September (1998~2002)
  • 21. Outputs of SiBUC October (1998~2002)
  • 22. Outputs of SiBUC November (1998~2002)
  • 23. Outputs of SiBUC December (1998~2002)
  • 24. Distributed Runoff Model Hydro-BEAM (Hydrological River Basin Environmental Assessment Model) Nile delta (Kojiri, T., 2006) Convert outputs of SiBUC to Hydro-BEAM. Flow direction is determined by Altitude. Aswan Khartoum Atbara Calculate discharge Sennar Kinematic wave model Roseires Surface runoff Bahr El-Ghazal Sobat Infiltration Bahr El-Jabal Lake Victoria Sub-surface runoff Linear storage model Schematic image of Hydro-BEAM
  • 26. What is “conflict analysis”? Conflict analysis is an analytical method which is developed expanding algorithm of metagame theory* Fraser and Hipel (1979) Conflict analysis consists of three elements… Howard (1971) 1. (Player) subject to play game 2. (Option) choice of player 3. (Preference) priority of option Results show what kinds of events are possible to occur. 26
  • 27. Algorithm of conflict analysis with example Stability Table (with third party) (r: rational, s: sequential stability, u: unstable) Egypt × × E × E × × × × × × × × × × START Total stability r r r r r u u u u u u u u u u Player's stability 3 6 9 12 15 2 5 8 11 14 1 4 7 10 13 UI from NO outcome q for q is rational for A (r) Preference vector 3 6 9 12 15 3 6 9 12 15 player A? YES Unilateral improvement 2 5 8 11 14 UI for B NO from A’s UI? q is unstable for A (u) Ethiopia YES Player's stability r r r u u u r r r u u u u u u All UIs (Check for for B preferred to simultaneous stability) Preference vector 7 8 9 4 5 6 13 14 15 1 2 3 10 11 12 q by A? YES NO Unilateral improvement 7 8 9 7 8 9 13 14 15 Another UI q is sequentially from q for A? stable for A (s) 4 5 6 YES NO Others Player's stability r r r r r r u u u u u u r r r A(B): Player A(B) END q: Event Preference vector 10 11 12 13 14 15 1 2 3 4 5 6 7 8 9 UI: Unilateral Improvement Unilateral improvement 10 11 12 13 14 15 27
  • 28. Algorithm of conflict analysis with example Stability Table (with third party) (r: rational, s: sequential stability, u: unstable) Egypt × × E × E × × × × × × × × × × Total stability r r r r r u u u u u u u u u u Player's stability 3 6 9 12 15 2 5 8 11 14 1 4 7 10 13 Preference vector 3 6 9 12 15 3 6 9 12 15 Unilateral improvement 2 5 8 11 14 Ethiopia Player's stability r r r u u u r r r u u u u u u Preference vector 7 8 9 4 5 6 13 14 15 1 2 3 10 11 12 Unilateral improvement 7 8 9 7 8 9 13 14 15 4 5 6 Others Player's stability r r r r r r u u u u u u r r r Preference vector 10 11 12 13 14 15 1 2 3 4 5 6 7 8 9 Unilateral improvement 10 11 12 13 14 15 Coding for automatic analysis 28
  • 29. Verification in the Nile Basin 29
  • 30. Discharge at Aswan High Dam D.S. (m3/s) 12,000 11,000 0 Error bar means max and min 12,000 11,000 0 Simulation_mean value Discharge at Atbara D.S. (m3/s) 10,000 100 10,000 Simulation_mean 100 Rainfall at the basin (mm/month) Rainfall at the basin (mm/month) Observation_max 9,000 9,000 Observation_max Observation_mean Observation_mean 8,000 200 8,000 200 Observation_min Observation_min 7,000 7,000 6,000 300 6,000 300 5,000 5,000 4,000 400 4,000 400 3,000 3,000 2,000 500 2,000 500 1,000 Aswan D.S. 1,000 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 600 Atbara 0 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 600 12,000 0 12,000 0 Aswan U.S. Discharge at Aswan High Dam U.S. (m3/s) 11,000 11,000 Discharge at Sennar Dam D.S. (m3/s) Simulation_mean 10,000 100 10,000 Simulation_mean 100 Observation_max Rainfall at the basin (mm/month) Rainfall at the basin (mm/month) 9,000 Observation_mean 9,000 Observation_max 8,000 Observation_min 200 8,000 Observation_mean 200 7,000 7,000 Observation_min 6,000 300 6,000 300 5,000 Sennar 5,000 4,000 400 4,000 400 3,000 3,000 2,000 500 2,000 500 1,000 1,000 0 600 0 600 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 12,000 0 Discharge at Roseires Dam D.S. (m 3/s) 11,000 Roseires 10,000 100 12,000 0 Rainfall at the basin (mm/month) 9,000 Simulation_mean Discharge at Owen Falls Dam D.S. (m3/s) 11,000 8,000 Observation_max 200 10,000 100 Observation_mean Rainfall at the basin (mm/month) 7,000 9,000 Observation_min 6,000 300 8,000 200 Simulation_mean 5,000 7,000 Observation_max 4,000 400 6,000 300 Observation_mean 3,000 5,000 Observation_min 2,000 500 4,000 400 1,000 3,000 0 600 2,000 500 Owen Falls Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 1,000 0 600 Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Error is around less than 10 %
  • 31. Assessment of future climate by MRI-AGCM and CMIP3 31
  • 32. Impact assessment of climate change by MRI-AGCM and CMIP3 GCM* in the world (2075~2099)/(2003~1979) Ave. Monthly multi-model A1B DJF Number Model Name Resl. x Resl. y Country 1 BCC-CM1 192 96 China 2 BCCR-BCM2.0 128 64 Norway 3 CCSM3 256 128 USA 4 CGCM3.1(T47) 96 48 Canada 5 CGCM3.1(T63) 128 64 Canada 6 CNRM-CM3 128 64 France 7 CSIRO-Mk3.0 192 96 Australia 8 CSIRO-Mk3.5 192 96 Australia 9 ECHAM5/MPI-OM 192 96 Germany 10 ECHO-G 96 48 Germany/Korea 11 FGOALS-g1.0 128 60 China 12 GFDL-CM2.0 144 90 USA 13 GFDL-CM2.1 144 90 USA [-] 14 GISS-AOM 90 (Citation: IPCCUSA WG1) 60 AR4 15 GISS-EH 72 46 USA (2075~2099)–(2003~1979) Ave. Monthly 16 GISS-ER 72 46 USA 17 INGV-SXG 320 160 Italy 18 INM-CM3.0 72 45 Russia 19 IPSL-CM4 96 72 France 20 MIROC3.2(hires) 320 160 Japan 21 MIROC3.2(medres) 128 64 Japan 22 MRI-CGCM2.3.2 128 64 Japan 23 PCM 128 64 USA 24 UKMO-HadCM3 96 73 UK 25 UKMO-HadGEM1 192 145 UK 26 MRI-AGCM3.1S 1920 960 Japan 27 MRI-AGCM3.2S 1920 960 Japan *GCM: Global Climate Model (Citation: IPCC AR4 WG1) [℃]
  • 33. Study of drought year by MRI-AGCM and CMIP3 Utilization of 24 GCM, 485 yearly samples, by MRI-AGCM(2075-2099) and CMIP3(2080-2099) 600 500 Table. Drought year (yr) in the Nile Basin Precipitation (mm/year) Drought year Precipitation (mm/year) Total Runoff (Gt/year) 400 Average 369.3 207.3 300 precipitation 5yr drought 340.9 188.6 200 10yr drought 329.2 180.8 20yr drought 317.0 172.8 100 50yr drought 305.9 165.4 100yr drought 294.2 157.7 0 0 100 200 300 400 500 Input of conflict analysis Ave. 平均降水量 precipitation 10yr 50yr 10年渇水 50年渇水 5年渇水 5yr drought 20年渇水 20yr drought 100年渇水 100yr drought
  • 34. Water Resources Development in the end of 21st century 34
  • 35. Setting of scenarios (basic elements) 1. 4 players ① Egypt, ② Sudan&S.Sudan, ③ Ethiopia, ④ Upstream countries in the White Nile 2. 11 options Use residual irrigated area on 0%, 10%, … ,100% (11 ways) 3. 2 preference orders ① Amount of water use ② Residual amount of water in the Nile River Total scenarios:14641 events 35
  • 36. Water use depending on ratio of expanded irrigation area 100 Egypt Sudan&S. Sudan Ethi a opi U pstream countri es 90 Calculated water use (Gt/year) 80 算定灌漑水使用量 (Gt/year) 70 60 50 40 30 20 10 0 0 10 20 30 40 50 60 70 80 90 100 Ratio of expanded irrigation area (%) 農業開発度(%) Calculate requirement for irrigation by hydrological model outputs. If water use is more than total runoff (supply), the events are unfeasible. 36
  • 37. 100 Analysis 1 Ratio of irrigated water resources development (%) Egypt 90 Sudan&S.Sudan 80 Averaged ratio of expanded irrigated area of equilibriums Ethiopia 70 in eachUpstream countries return period of drought MEAN 60 (Unit: %) 50 5yr drought 10yr drought 20yr drought 50yr drought 100yr drought 40 Egypt 54 60 46 38 51 30 Sudan&S.Sudan 52 57 44 37 47 20 Ethiopia 70 49 40 30 17 Upstream 10 countries 54 52 50 47 46 0 Average 57.5 54.5 45.0 38.0 40.3 0 1 2 5yr 10yr 3 4 5 20yr 50yr 100yr 6 The numbers in table indicate “the average of situation which is possible to occur”. As a result, in the case that all basin countries develop 40% of remained potential field for irrigated area, some discussion will be required on the water allocation for 20 years drought situation.
  • 38. Analysis 2 ~Visualization of equilibrium points~ Definition of quadrants Visualize the end of vectors 1.5 1.5 2 1 1 2 1 0.5 (Sudan&S.Sudan) (Egypt) 0.5 0 0 -0.5 -0.5 3 4 (Upstream -1 -1 (Ethiopia) countries) -1.5 -1.5 -1.5 -1 -0.5 0 0.5 1 1.5 -1.5 -1 -0.5 0 0.5 1 1.5 Set 4 axes for each player Unit: ratio of expanded irrigated area
  • 39. Analysis 2 ~Visualization of equilibrium points~ 20 years drought 100 years drought According to distribution map, Egyptian side has substantial advantage rapidly, and Ethiopian side has remarkable disadvantage
  • 40. Analysis 3 ~Refinement~ Take off events whose difference between maximum and minimum ratio is more than 70% 20 years drought 100 years drought
  • 41. Analysis 3 ~Refinement~ After 70% refinement 5yr drought 10yr drought 20yr drought 50yr drought 100yr drought Egypt 66 59 41 30 29 Sudan&S.Sudan 63 56 37 28 25 Ethiopia 62 48 43 34 25 Upstream countries 60 54 45 37 36 Average 62.6 54.6 41.2 32.3 28.8 Ratio of irrigated water resources development (%) 100 100 Ratio of irrigated water resources development (%) Egypt Egypt 90 90 Sudan&S.Sudan Sudan&S.Sudan 80 Ethiopia 80 Ethiopia 70 Upstream countries 70 Upstream countries MEAN MEAN 60 60 50 50 40 40 30 30 20 20 10 10 0 0 0 5yr 1 10yr 2 20yr 3 50yr 4 100yr 5 6 0 1 5yr 2 10yr 3 20yr 4 50yr 5 100yr 6
  • 42. Conclusion 1. Hybrid of Conflict Analysis and Hydrological Model is proposed and applied to the whole Nile River Basin for international river management. 2. Assessment of future climate is conducted in each sub-basin by MRI-AGCM and CMIP3. 3. Plural equilibrium points are analyzed. As a result, in the case of 20 years drought situation, 40% of remained potential field for irrigated area is recommended as the maximum ratio for all basin countries. These recommended ratio depends on cooperative return period of drought. 42
  • 44. Database of JE-HydroNet (tentative)
  • 45. Database of JE-HydroNet (tentative) Summary of database 1. Purposes (1) To introduce JE-HydroNet project to the public (2) To share hydrological information between project members 2. Contents (1) Introduction of JE-HydroNet (2) Announcement of next symposium (3) Reports of the previous symposium (4) Download data (only for project members) 3. How to manage this website (1) Need to discuss for the near future 45 Thank you for kind attention.