drought monitoring and mitigation in the horn of africa drought monitoring and mitigation in the...
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Drought Monitoring and Mitigationin the Horn of Africa
Are we prepared?
Somalia Water and Land Information Management System
Z. Balint, Chief Technical AdvisorP. Muchiri, Meteorologist
FAO SWALIM
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Integrated drought management
Whatto do ?
Whoshould do it?
Howto do?
Can we manage drought?Natural phenomena
Impacts of drought
Mitigating the impacts of drought
WHAT can we use?Tools, measures, facilities
HOW can we use?Response systems,
Preparedness
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WHAT? HOW?
• Drought resistant crops• Irrigation• Storage systems• Market systems• etc.
• Long term plans for sustainable production• Short term plans for adaptation• Rapid response plans for mitigating the impacts
MONITORING
Long term trends
Real-time drought evolution
Early warning
Impacts
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SOLUTION(example)
Proper identification:Env. Degradation
•export charcoal prod•plant degradation•soil erosion
Altern. income generationLand conservationLand use planningFarm development
Food distribution
Local market pricedown
SUSTAINABLE SUPPLY OF FOOD
SHORT TERMLONG TERM
DEPENDENCY
FUNDS
Based on Measurements
& analysis
More difficult to get
Relatively easy to mobilise
“DROUGHT”
Food shortage causedby drought or
env. degradation
Production stops(incl. seeds)
Skills degrade
SHORT + LONG TERM
Why monitor drought? Proper diagnosis is needed for proper response
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Drought is a frequent, recurrent event in the Horn of Africa. - Despite its frequency it always seems to be a surprise, causing an emergency.
Are we prepared?Do we have the common understanding of drought?
Do we know what to observe and do we have the equipment for that?
Do we have monitoring systems?
Do we have methodologies how to interpret the observations?
Do we have the pre-set mechanisms, the standard procedures how to react in a real emergency situation?
Do we know the measures, tools, how to mitigate the impacts of drought?
Do we have long term visions how to adapt the production system to show more resilience to drought?
There is a long way to go.
We can start with better understanding the drought and join our efforts in developing methodologies for monitoring, forecasting and mitigating its impacts.
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What is drought?
Animals die
overgrazing
Population growth
hail, cold rain
diseaseCrop failure
drought
armed conflicts
market problemsMalnutrition
grows
Food shortage
Armed conflicts
Market problems
drought
drought
disease
wrong crop type
drought
Drought – short term (end foreseen) – temporary deviation
Land degradation – long term - difficult to reverse
Treatment is much different
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Serious anomaly - Long duration
What is drought?
Drought is an extended period, during which, fresh water availability and accessibility for the ecosystem at a given time and place is below normal, due to unfavourable spatial and temporal distribution of rainfall, temperature, soil moisture and wind characteristics.
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region are:
•Rainfall amount
•Rainfall temporal distribution
•Soil moisture
•Soil moisture temporal distribution
•Temperature
•Temperature temporal distribution
•Wind characteristics
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How to measure the severity of drought?
Physical indices (water balance)Palmer’s Drought indices, namely, Palmer Drought Severity Index (PDSI), Palmer Hydrological Drought Index(PHDI), Palmer Z-index (PZI) and Crop Moisture Index (CMI)
Surface Water Supply Index (SWSI)
Reclamation Drought Index (RDI)
Statistical indexes (time series analysis)Percent Normal Drought Index (PNDI)
Standardized Precipitation Index (SPI)
Precipitation Decile Index
Weighted Anomaly Standardized Precipitation (WASP)
Drought indices analysed
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Multiple parameter
precipitation temperature soil moisture wind
Combined effect
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miVDImiTDImiPDImi VDIwTDIwPDIwCDI ,2,2,, ***
It is an index that measures how much the present conditions deviate from the reference level, which is the multi-year long-term average for a selected time duration (X dekads, Y months).
IP in the cessdeficit/excont oflength LTM
IP in the cessdeficit/excont oflength Actual*
IPfor LTM
IPfor average Actual DI
Step 1: Three different, individual drought indices are calculated, each reflecting the quantity deviation from LTM and the persistence of the deviation
Step 2: The combined effect is calculated in the CDI
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drought index
Temperature drought index
Vegetation drought index
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For more information please consult the CDIbrochure and the attached CDI calculator CD
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Kenyan stations
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Hargeisa
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
1982 1983 1984 1985 1986 1987 1988 1989 1990 NO DATA 2005 2006 2007 2008 2009 2010
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(-) PDI VDI CDI Threshold
Baidoa
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
5.0
1982 1983 1984 1985 1986 1987 1988 NO DATA 2004 2005 2006 2007 2008 2009 2010
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PDI VDI CDI Threshold
Afgooye
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
5.0
5.5
6.0
6.5
1982 1983 1984 1985 1986 1987 1988 1989 1990 NO DATA 2005 2006 2007 2008 2009 2010
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PDI VDI CDI Threshold
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Debrecen – Hungary, Europe
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CDI trends and comparison with drought reports 1
Year Month Kakamega Kisumu Lodwar Embu Dagoretti Wajiir Mandera County
Western Kenya North Kenya Central Kenya North East Kenya
1999 10 1.32 1 0.6 0.46 1.05 0.88 0.9 0.89
1999 11 1.08 0.9 0.69 0.81 1.21 0.65 0.78 0.87
1999 12 0.96 1.04 0.79 1.07 1.57 0.74 0.86 1
2000 1 0.77 1.06 0.71 1.37 1.47 0.9 1.06 1.05
2000 2 0.67 0.87 0.59 1.31 1.06 0.96 1.02 0.93
2000 3 0.42 0.68 0.42 0.64 0.58 0.63 0.61 0.56
2000 4 0.34 0.51 0.46 0.49 0.52 0.5 0.62 0.51
2000 5 0.49 0.49 0.33 0.31 0.51 0.34 0.89 0.56
2000 6 0.63 0.61 0.31 0.32 0.62 0.33 0.99 0.64 2000 7 0.75 0.82 0.25 0.34 0.67 0.45 1.53 0.86 2000 8 0.7 0.93 0.31 0.53 0.65 0.63 0.56 0.62 2000 9 0.6 0.95 0.36 0.65 0.66 1.22 0.42 0.66 2000 10 0.71 0.93 1.25 0.52 0.8 0.76 1.05 0.94
2000 11 0.86 1.12 1.77 0.48 0.72 0.53 1.09 1.03
2000 12 1.07 1.34 1.91 0.42 0.73 0.32 0.83 1
2001 1 1.33 1.91 1.55 0.68 1.42 0.34 0.45 1.1
2001 2 1.53 1.86 1.65 1.03 1.88 0.5 0.43 1.23
2001 3 1.14 1.3 1.7 1.34 2.57 0.85 0.61 1.36
Drought severity legend
Extreme
Severe
Moderate Mild None
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The CDI reflects: rainfall amount deficit and its critical duration
air temperature excess and its critical duration
NDVI deficit and its critical duration
It provides a time series of the indices that can be further analysed with statistical methods
Further research is suggested on
• Howe to use it for short time early warning
• How to extent it from point data series to spatial analysis
SUMMARY CONCLUSIONS ON CDI
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Somalia Water and Land Information Management System
Thank you for your attention