End of Basin issues in Mekong Basin Issues facing those living in Tonle Sap /Delta Bio-physical...
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Transcript of End of Basin issues in Mekong Basin Issues facing those living in Tonle Sap /Delta Bio-physical...
End of Basin issues in Mekong Basin
• Issues facing those living in Tonle Sap /Delta • Bio-physical causes /origins of these problems• Who is affected? • What are their long-term development
objectives?
Issues facing those living in Tonle Sap/Delta
• Natural resource degradation– Declining fish population – Salinity intrusion and acidity– River bank erosion– Sedimentation– Imbalance water flow in dry and wet season
• Water shortage in dry season– Competing demand for water
• Flood and inundation• Deforestation
Seawater Intrusion in Mekong Delta (2/3)Seawater Intrusion in Mekong Delta (2/3)Jan. 2003Upstream Discharge into
Mekong Delta is Key Factor !
Upper Limit of Maximum Salinity in 1985
20g/l
25g/l
0g/l 5g/l10g/l15g/l
April
0g/l5g/l10g/l
June
Flood and inundation
Tidal effect at Delta
0.8 m above sea
Flood-Hazard Areas in the Lower Mekong Basin
Issues facing those living in Tonle Sap/Delta
• Natural resource degradation– Declining fish population – Salinity intrusion and acidity– River bank erosion– Sedimentation– Imbalance water flow in dry and wet season
• Water shortage in dry season– Competing demand for water
• Flood and inundation• Deforestation
24
Despite being heavily forested, deforestation rate in Cambodia is at present very high. In 1989-92, it reached almost 3% per year.
Forest clearance in Viet Nam has resulted in severe soil erosion and an increased incidence of floods as many upper watersheds areas have been cleared.
Deforestation
Bio-physical causes / origins of these problems
• Population pressure • Development interventions • Over-fishing • Increasing water demand in sector
development • Increasing use of chemicals• Change of hydrological regime • Climate change• Deforestation
Who is affected?
• All people in the sub-areas (directly and indirectly)
• The ecology in the sub-area
• The biodiversity in the sub-area
What are the long-term development objectives of those at the end of the Basin system?
• Economic growth
• Poverty alleviation
• Prosperous and peaceful basin
• Mutual benefit and understanding, and cooperation
Irrigation growthIrrigation growthTotal dry season irrigated cropped areasirrigated cropped areas (ha)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
mill
ion
hect
ares
1985 1990 1995 2000
Cambodia Lao PDR Thailand Viet Nam
Indicative dry season water balanceAverage Flows at Kratie
MCM/month
-
20,000
40,000
60,000
80,000
100,000
120,000
J F M A M J J A S O N D
Dry Season Water Balance MCM
-
25,000
50,000
75,000
100,000
125,000
150,000
1985 2000Dry season runoff Irrigation 90 Irrigation 70
On average 10,400 MCM/month in dry
season
13-17%13-17% of Kratie flow
52%52%
Basin irrigation efficiencies of 90%90% and 70%70%
40%40%
9
Mekong Fisheries
Total 2 million tonnes Capture Fisheries
1.75 million tonnes Aquaculture 0.25 million
tonnes
Total value: $1,400 million
40 million people involved full or part-time
Non-fish products (shellfish, frogs, insects, aquatic plants)
Flooding
• 2000 flood– 800 people died– $400 million damage
• 2002 flood and drought– impact on food security
and health
Key Factor of Water Utilization in Mekong DeltaKey Factor of Water Utilization in Mekong Delta
Fishery
Water Utilization inMekong Delta
Agriculture
Navigation Domestic
Vital Role of Mekong Deltain Vietnam Economy :
39,000 km2, 6.4% of LMRB 16 millions of population Huge potential of agriculture (2.9
million ha, 74% of delta) Irrigated for paddy (1.4 million ha) More than half of paddy
production
Key Issues on Water Use inMekong Delta:
Water Shortage in the Dry Season Seawater Intrusion Acidification (acid sulphate soils)
HydrologicalCharacteristics in Mekong
Delta (see next picture)
Changes in overall paddy areas and production - 1990 to 2000
80%80%
60%60%
40%40%
20%20%
ProductionArea
Cambodia Lao PDR Thailand Viet NamCambodia Lao PDR Thailand Viet Nam