Management of Rainwater and Small Reservoir for Multiple Uses
1. SCIENCE WORKSHOP : Volta Basin
Development Challenge of the CPWF
Annual reflection meeting
Hydrological Modeling-CPWFV3
03th-05th july , 2012
Presented by
Frank ANNOR, KNUST-TUDelft
FOWE TAZEN, 2iE Foundation
2. Presentation Outline
1. Background
2. Methodology
i. Instrumentation
ii. Modeling
3. Initial Results
4. Way forward
Andes • Ganges • Limpopo • Mekong • Nile • Volta
3. Background
Morphometric characteristics of
Boura catchment
Surface area (km²) : 155.3
Perimeter (m)
: 59.6
Compactness index : 1.34
Mean elevation (m) : 300
Specific elevation(m) : 37.24
Mean slope (m/km) : 3.4%
Global slope index(m/km) : 4
Andes • Ganges • Limpopo • Mekong • Nile • Volta
Morphometric characteristics of
Binaba catchment
Surface area (km²): 11.8
Perimeter (m)
: 14.6
Compactness index : 1.2
Mean elevation (m) : 225
Specific elevation (m) : 23.80
Mean slope (m/km) : 0.35%
Global slope index (m/km) : 6.9
4. Background
× No hydrological monitoring
– Boura and Binaba watersheds
are ungauged
• No records of streamflow,
evaporation, water level etc
• Difficult to calibrate a
hydrological model in the
basin at a small watershed
without these records
× Management (allocation) of
water has not been streamlined
especially for the dry season
Objectives
Physical and hydrological
characterization of watersheds of
both sites
Building of the monthly
streamflow time series
Establish the water budget of
each reservoir
Determine the heat balance of
the reservoir
Model GW-SW interactions
Andes • Ganges • Limpopo • Mekong • Nile • Volta
5. TU-Delft
2IE
Developing a Hydrological model
(Yates, GIRARD & GR2M)
Developing a water allocation
model using WEAP at a smaller
watershed level (Boura and
Binaba) using the water balance
Water Use
Other components of the water
balance i.e Runoff, P,ET, etc
Evaporation and seepage losses
in lakes in the Volta basin using
water and heat balance
Detailed study in Binaba &
(Boura?)
Regionalising for the basin using
remote sensing (Images through
the TIGER project)
Groundwater surface water
interactions (natural Isotopes)
Andes • Ganges • Limpopo • Mekong • Nile • Volta
7. Water budget of the reservoir
Boura only
?
?
?
Andes • Ganges • Limpopo • Mekong • Nile • Volta
8. Getting the water balance right ..1
gauge plates
Rain gauge
Evaporation pan
Monitoring well
DTS
EC
Andes • Ganges • Limpopo • Mekong • Nile • Volta
9. Getting the water balance right …2
Thalimedes
Water Sampling Points
for Isotope analyses
Rainfall Sampling
Andes • Ganges • Limpopo • Mekong • Nile • Volta
16. Some initial results
Water Temperature at bottom of lake
600
25
500
20
400
15
300
10
200
5
100
0
0
Date/Time
Binaba reservoir
Andes • Ganges • Limpopo • Mekong • Nile • Volta
Water level (m)
700
30
Temperature (oC)
35
17. Way Forward
More data collection
Calibration and verification of models
Scenario
building
(climate
change, water uses, cropping pattern)
Andes • Ganges • Limpopo • Mekong • Nile • Volta
18. Thank you for
your attention
Andes • Ganges • Limpopo • Mekong • Nile • Volta