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Water Demand - Impetus

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The GLOWA Volta Project:<br />

An overview<br />

Jens Liebe,<br />

Charles Rodgers,<br />

Nick van de Giesen<br />

and<br />

Paul L.G. Vlek


The Volta Basin:<br />

Major Expansion Challenge of irrigated in the Volta<br />

5005%<br />

Basin for agriculture <strong>Water</strong> Resources<br />

mm 2500 mm +++<br />

Management<br />

42%<br />

• 400,000 km 2<br />

• 6 riparian countries<br />

• 20+ million inhabitants<br />

• 1,000 mm avg. precipitation<br />

potential evaporation<br />

<strong>Demand</strong> for irrigation<br />

4%<br />

6%<br />

3%<br />

40%<br />

Hydropower generation<br />

at Akosombo<br />

Population growth rate:<br />

Burkina Faso 3%<br />

Ghana 2%<br />

2000 mm 1500 mm +


Objectives<br />

• Integrated analysis of the physical and social<br />

determinants of the hydrological cycle<br />

• Scientifically sound Decision Support System for the<br />

assessment, sustainable use and development of the<br />

water resources of the Volta Basin<br />

• Development of “Human Capital“ via advanced education<br />

and training, co-operative research and stakeholder participation


Climate, Land Use, Hydrology<br />

Economics, Institutions, Stakeholders<br />

Environmental<br />

Remote<br />

Sensing<br />

Instrumentation<br />

Land Conversion<br />

Change<br />

<strong>Water</strong><br />

Supply<br />

Hydrology<br />

Field<br />

Investigations<br />

<strong>Water</strong> <strong>Demand</strong><br />

Stakeholder<br />

Dialogue,<br />

Processes of decision<br />

making and information<br />

flows<br />

Knowledge<br />

Exchange,<br />

Capacity<br />

Building<br />

Institutional<br />

Analysis<br />

Institutional Analysis<br />

Mesoscale Climate<br />

Integrated Basin<br />

Model


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Climate Change<br />

• Increase in Temperature (1.2-1.3 °C )<br />

• Greater variability<br />

• rainfall<br />

• runoff<br />

• greater frequency of extremes<br />

• Regional floods and droughts<br />

Onset of the rainy season<br />

• Prolongation of the dry season<br />

• ORS more variable, today up to 30 days<br />

later than 40 years ago<br />

• Increase and intensification of rainfall<br />

at the end of the rainy season<br />

Precipitation Change [%]


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Groundwater<br />

production<br />

Groundwater in the Volta Basin<br />

• in White Volta Basin: annual<br />

recharge 5-8% of annual rainfall<br />

• GW use in Upper East Region of<br />

Ghana ca. 5% of recharge<br />

• Use below the potential


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Surface Runoff Change [%]<br />

Surface water in the Volta Basin<br />

• Slight increase of river flow<br />

• shift in runoff patterns<br />

(later runoff generation)<br />

• increase of extreme events<br />

(floods and droughts)


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Surface water:<br />

Agricultural & hydropower<br />

development<br />

BURKINA FASO<br />

Lery Reservoir<br />

Volume: 0.6 km³<br />

1976<br />

MALI<br />

Ziga Reservoir<br />

Volume: 0.2 km³<br />

2000<br />

B U R K I N A F A S O<br />

NIGER<br />

Bagre Reservoir<br />

Volume: 1.7 km³<br />

1992<br />

Small Reservoirs<br />

Volume: 0.6 km³<br />

Tono Reservoir<br />

Volume: 0.1 km³<br />

1980<br />

Kompienga Reservoir<br />

Volume: 2.0 km³<br />

1984<br />

BENIN<br />

GHANA<br />

Bui Reservoir<br />

Volume: 12.3<br />

km³<br />

2009/2010<br />

IVORY COAST<br />

lake<br />

Volta<br />

TOGO<br />

Lake Volta<br />

Volume: 148 km³<br />

1964<br />

Small Reservoirs<br />

Volume: 0.1 km³<br />

G H A N A<br />

Kpong Reservoir<br />

Volume: 0.2 km³<br />

1982


MIKE Basin Setup<br />

1. 23 hydro-economic catchments for the Volta<br />

Basin (specific discharge time series are<br />

generated for each catchment) according to<br />

national boundaries and large reservoirs.<br />

2. large reservoirs: Akosombo, Bagre, Kompienga,<br />

Ziga, (Bui), including hydropower and large<br />

reservoir abstractions for irrigation and<br />

portable water.<br />

Area [km^2]<br />

Volume [10^6m^3]<br />

Area, Volume<br />

3000<br />

2000<br />

1000<br />

0<br />

215 220 225 230 235 240<br />

3. water user (sector) per catchment:<br />

domestic use<br />

industrial use<br />

small scale irrigation (small reservoirs)<br />

<strong>Water</strong> demand<br />

[m^3/s]<br />

Deficit carry-over fraction [()]<br />

Groundwater use fraction [()]<br />

Groundwater use absolute [m^3/s]<br />

Elevation [m asl]<br />

abstraction<br />

60<br />

40<br />

20<br />

0<br />

1991 1992 1993 1994 1995 1996 1997 1998 1999 2000<br />

year


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Domestic water demand<br />

Agricultural water demand<br />

<strong>Water</strong> demand for hydropower<br />

Urban Energy demand, Ghana<br />

Rural<br />

Burkina Faso<br />

Ghana<br />

Industrial water demand<br />

Burkina Faso<br />

Urban<br />

Rural<br />

Ghana


M³ WATER hydro-economic model<br />

Multi-country Multi-sector Multi-use<br />

COUNTRIES:<br />

SECTORS:<br />

USES:<br />

Ghana / Burkina Faso<br />

Agriculture / Domestic / Industry / Hydropower<br />

(Non) - Consumptive / Environmental<br />

W ater<br />

A llocation<br />

T echnology for the<br />

E fficient management of<br />

R esources in the Volta Basin


M³ WATER MODEL STRUCTURE<br />

simulated specific discharge<br />

g<br />

time series (MM5/WaSiM-ETH)<br />

5//WaSiM-ETH)<br />

water supply<br />

ply<br />

transformation<br />

tio<br />

on<br />

Hydrological HgHydrolog Hgical Hg<br />

model<br />

(MIKE Basin)<br />

Hg<br />

Optimization:<br />

Allocation of water resources that maximizes<br />

the total net benefits to society.<br />

Economic model<br />

(GAMS)<br />

transformation<br />

ti<br />

on<br />

water demand<br />

demographic and economic indices<br />

water use policies<br />

simulated i l t d areal l precipitation p<br />

it ti and d<br />

potential potrapotenpotrapoten<br />

evapotranspiration<br />

p<br />

potransspiration<br />

(MM5/WaSiM-ETH)<br />

pote<br />

5 M


The Climate Generator<br />

High-resolution Regional Climate and Hydrological Modelling for the Volta Basin of<br />

West Africa (Harald Kunstmann and Gerlinde Jung, IMK-IFU, Garmisch-<br />

Partenkirchen, Germany)<br />

• Two time slices (1991-2000 and 2030-2039) of the ECHAM4 scenario IS92a were<br />

dynamically downscaled with MM5 to a spatial resolution of 9 km x 9 km.<br />

• The distributed process-based hydrological model WASIM-ETH was run with the<br />

MM5 generated climate data for the time slices 1991-2000 and 2030-2039 with a<br />

1 km x 1km resolution.


• expansion of irrigated agriculture<br />

• increase in fertilizer use<br />

• self sufficiency in rice


Example: Expansion of irrigated agriculture


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Capacity building<br />

• capacity building<br />

• students<br />

• networking<br />

• workshops<br />

• Volta Basin Authority


Env. Change – <strong>Water</strong> Supply – <strong>Water</strong> <strong>Demand</strong> – Stakeholders/Capacity – Decision Support<br />

Example GVP Geoportal<br />

Data search<br />

– find and assess<br />

– download<br />

Interactive geodata<br />

compose, view and<br />

analyze on map<br />

download from map<br />

Publish and share data<br />

index and administrate<br />

assign use rights<br />

upload for distribution


Services


Hydro Argos stations are linked to the GLOWA Volta Geoportal<br />

Lawra<br />

Chache<br />

Yarugu<br />

Pwalugu<br />

Sabari


Decision Support<br />

Decision Support Systems<br />

Decision Support Tools<br />

Decision Support<br />

Characteristics of DST’s/DSS’s<br />

• Foster understanding and assist decision making<br />

• Link decision making, scientific information, and analytical tools<br />

• Help experts to model the expected outcomes of certain actions<br />

• Decision support tools solution tool<br />

• Still require experts<br />

In the Volta Basin: attain consensus/avoid conflict over<br />

water allocation, respecting each<br />

countries policy and development goals


Scales addressed in GVP Decision Support<br />

West Africa Volta Basin Regional Local Independent<br />

MM5<br />

Geoportal<br />

Joint Climate-Hydrology Simulation<br />

Geodatabase<br />

Prediction: Onset of the Rainy Season<br />

Weather forecast<br />

M³ Hydro-Economic Model<br />

Soil moisture model<br />

Institutional Map<br />

Land Cover Change/LUCC detection<br />

Agent based Energy & Land Use Model<br />

Groundwater Recharge<br />

Reservoir storage<br />

Evaporation (Makkink, SEBAL, EC)<br />

RS based runoff<br />

GV-LUDAS<br />

www.glowa-volta.de<br />

LAMPT<br />

Knowledge M’ment<br />

Workshops/Training<br />

Capacity Development and Network building


Conclusions<br />

• Research networks have formed, capacity building was successful<br />

• Data scarcity is reduced<br />

• Environmental change leads to greater variability in precipitation, runoff<br />

• Population growth leads to increased demand, competition for water<br />

• GVP provides Decisions Support Resources at different levels<br />

• GVP supports the Volta Basin Authority

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