The Hyrdrology of Floods in Malawi Cities
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Transcript of The Hyrdrology of Floods in Malawi Cities
THE HYDROLOGY OF FLOODS
IN MALAWI CITIESTHE ROLE OF WETLANDS
Kenneth Wiyo, Bunda Campus, LUANAR
Seminar OutlineFlooding in Malawi January 2015
Introduction
Flood definition
Hydrology of flooding
Underlying drivers of floods
Case of cities of Blantyre & Lilongwe
Role of Wetlands/ Dambos in cities
Conclusions
Flooding DefinitionFlooding in Malawi January 2015
Def: Excess surface runoff exceeding the capacity of channels, streams and rivers resulting in the channel bursting its banks/ overflowing
Destruction of life, livestock, crops, property, infrastructure
Destructive force
Hydrology of Flooding (multi-facetted)
Excessive surface runoff
(SRO)
High rainfall within or
outside the catchment,
prolonged
Climate change effects
resulting in extreme
rainfall within or outside
the catchment (Jan 2015
floods)
Land use changes in the catchment resulting in low infiltration and high SRO
Underlying Drivers of Floods
Reduced capacity of channels/rivers to contain the excess SRO
Soil erosion, reduced infiltration, high SRO
Siltation and sedimentation
(A)Extreme or high rainfall events (natural or climate change)
(B) Destruction of the Environment
land pressure for agric
River bank cultivation
Cultivation of marginal lands
Deforestation-trees cut in river banks and forest reserves
Population pressure- more land for human settlements
And then came the floods (3)
Flooding, water
everywhere
Too much SRO nowhere
to go
Rivers/channels burst
their banks
Flooding everywhere, water everywhere
Life, livestock, crops property destroyed
Roads, infrastructure
damaged
Flooding in Malawi Cities (LL & BT)
Flooding in the cities of Blantyre and Lilongwe was very rare in the past
Now increasingly common (Ndirande, Area 36, Biwi).
What has changed? Land Use has changed
Land Use Changes Within Cities
Blantyre City Lilongwe City
Population growth, demand for human settlements
Housing in steep marginal areas (e.g Ndirande, Soche hills)
Forest reserves converted to settlements, agriculture
Houses close to river banks (Nasolo)
Storm drains sewers blocked by solid waste
Population growth, demand for human settlements
Gmelina forests converted to housing (areas 36, 22, 23 etc)
Prime agriculture land converted to housing- LL expanding eastwards
Settlements have now expanded into protected wetlands/ dambos (Kawale, Area 47, Kauma etc).
Hydrology of flooding in cities
Housing settlements, Infrastructure reduce infiltration and increase SRO (more roofs, impermeable surfaces)
Storm drains, culverts designed to take a certain design SRO flow. If SRO increases, capacity of storm drains, culverts exceeded
More SRO, more flooding
Role of Wetlands/Dambos in Flood Control
Functions of Wetlands Destruction of Dambos
Provide extra storage capacity for excess SRO
Thus act as a buffer zone for floods, slowly releasing the water , ameliorating peak flows
Can trap sediments, less enter the rivers
Clean the water, and trap pollutants
Encourage biodiversity in our cities, areas of wildlife refuge.
Protected Lilongwe City dambos encroached and destroyed-housing settlements.
Flood control/buffer function no longer there
More flooding in Lilongwe City
Summary of Flooding in Cities
Causes of Floods in General
Flood Drivers in Cities
Floods are multi-facetted.
Can either be caused by prolonged high rainfall events or extreme events due to climate change resulting in excess SRO.
Land use changes in a catchment can trigger floods by increasing erosion, decreasing infiltration and increasing SRO.
Increase in housing settlements into marginal forested areas, dambo and river banks.
Conversion of forested areas into human settlements.
Housing into protected wetlands/ dambos- no flood buffer.
Expect more flooding in Lilongwe and Blantyre Cities
FLOOD MITIGATION REQUIRE
TEAM WORK
THANK YOU