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MODELS FOR EARLY DETECTION OF MALARIA EPIDEMIC IN EAST AFRICA Dr. A. K. Githeko PhD Principal Investigator

PowePoint - Early epidemic detection

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Page 1: PowePoint - Early epidemic detection

MODELS FOR EARLY DETECTION OF

MALARIA EPIDEMIC IN EAST AFRICA

Dr. A. K. Githeko PhD

Principal Investigator

Page 2: PowePoint - Early epidemic detection

Epidemic

detection

Intervention

Epidemic

early

prediction

Risk

communication

Intervention

Time

Outbreak

Epidemic

Epidemic detection using

clinical data

Early epidemic prediction

using climate dataEpidemic

prevented

Page 3: PowePoint - Early epidemic detection

Climate Drivers

Increase in mean

temperature

Temperature

variability

Deforestation

Swamp

reclamation

Typical impact on

ambient

temperature

0.5-1oC

1-5oC

1-2oC

Water temp 2-5oC

Ambient temp 1oC

Effects on malaria

transmission

Additive effect to

threshold

transmission

temperature 18oC

18.5-19oC

19-23oC

19-20oC

19oC

Enable

Epidemic

Enable

Enable

Spatial

impacts of

drivers

Increase in mean temp Temp

variability

Deforestation Swamp

reclamation

Regional Local

Greatest impact of drivers on Plasmodium falciparum malaria occurs

in the exponential phase 18-22oC of parasite development in the vector

Page 4: PowePoint - Early epidemic detection

NOTES

Changes in temperature affects both Plasmodium falciparum and

Anopheles gambiae rates of development

Anopheles gambiae the major African malaria vector in

Kenya requires at least 150 mean monthly rainfall for its

population to increase in poorly drained ecosystem and

250-300 mm in well drained ecosystems. Rainfall has no

effects on Plasmodium falciparum development rates.

The highlands lie in the temperature range of 16-19oC. The most sensitive

development phase of Plasmodium falciparum in the mosquito lies between

18-22oC (exponential phase).

The macroclimate and microclimate drivers can interact and

enhance malaria transmission.

Page 5: PowePoint - Early epidemic detection

MODELS DETECT CHANGES IN

MEAN MONTHLY TEMPERATURE

AND RAINFALL IN THE

HIGHLANDS.

THESE CHANGE CAN INITIATE

MALARIA EPIDEMICS

Page 6: PowePoint - Early epidemic detection

1002

xER mm

ii

MT

RT

1002

xER mm

ii

xRT

xRT

10018 xER mm

ii

xRT

xRT

Additive model

Multiplicative

model

Models using climate data

18+C model

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KAKAMEGA 1997: EARLY EPIDEMIC PREDICTION

SEQUENCE

4oCRainfall100.0%Epidemic risk

145.6%

Case

increase1

First signal

Temperature

anomaly

Epidemic

risk

confirmed

EPIDEMIC

OCCURES

FEB-97 MAR APR MAY JUN

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KAKAMEGA 1998: EARLY EPIDEMIC PREDICTION

SEQUENCE

4OC Rainfall81.8%

Epidemic risk

330.1%Case

increase

First signal

Temperature

anomaly

Epidemic

risk

confirmed

EPIDEMIC

OCCURES

AUG-97 SEP OCT NOV DEC JAN_98

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KAKAMEGA 1999: EARLY EPIDEMIC PREDICTION

SEQUENCE

2OCRainfall 40.9%

Epidemic risk

272.7%

Case

increas

e

First signal

Temperatur

e anomaly

Epidemic

risk

confirmed

EPIDEMIC

OCCURES

JAN_99 FEB MAR APR MAY

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KAKAMEGA: ADDITIVE MODEL

Sensitivity 1

Specificity 1

Positive predictive

value

1

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NANDI: MULTIPLICATIVE MODEL

Sensitivity 0.78

Specificity 0.99

Positive predictive

value

0.86

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AUTOMATED KAKAMEGA MODEL FOR USERS

OUTPUT IN GRAPH: INPUTS ARE MEAN MONTHLY TEMPERATURE AND

RAINFALL

KAKAMEGA MALARIA EPIDEMIC EARLY DETECTION SYSTEM

YEAR

MAX TEMP

INPUT

COLUMMLTM max

temp

MAX TEMP

ANOMALY

RAINFALL

INPUT

COLUMMRAINFALL

CODES

TEMP

ANOMALY

CODES

ADDITIVE

MODEL:

Percent

risk

JAN 09 29.5 28.3 1.2 163.8 1 4 #REF!

FEB 30.6 29.2 1.4 8.0 0 4 18.2

MAR 31.1 29.1 2.0 125.7 0 4 18.2

APR 27.6 27.3 0.3 267.0 5 1 40.9

MAY 27.2 26.4 0.8 210.2 3 1 18.2

JUN 27.7 25.8 1.9 132.1 0 4 4.5

JUL 26.9 25.6 1.2 91.0 0 4 18.2

AUG 27.6 26.1 1.5 180.5 0 4 18.2

SEP 27.4 26.9 0.5 227.4 2 1 27.3

OCT 26.7 27.0 -0.3 124.9 4 0 22.7

NOV 27.5 26.9 0.7 98.2 0 1 0.0

DEC 29.7 27.5 2.1 178.3 0 9 4.5

JAN 10 28.8 28.3 0.6 38.7 2 1 50.0

FEB

MAR

APR

MAY

JUN

JUL

AUG

SEP

OCT

NOV

DEC

Malaria early epidemic prediction: Kakamega

0

10

20

30

40

50

60

JAN

09

MAR MAY JUL SEP NOV JAN

10

MAR MAY JUL SEP NOV

Time (Month)

Ep

ide

mic

ris

k

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OTHER DRIVERS OF MALARIA

Topography and drainage

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FLAT BOTTOMED “U” SHAPED VALLEY POOR DRAINAGE, GOOD FOR MOSQUITO

BREEDING

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3D SATELLITE IMAGE OF “U” SHAPED VALLEY

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NARROW “V” SHAPED VALLEY WITH FAST FLOWING STREAM

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“U” SHAPED VALLEY HAVE 2.9-FOLD MORE

MALARIA MOSQUITOES THAN “V” SHAPED

VALLEYS

THIS AFFECTS MALARIA TRANSMISSION

AND IMMUNITY TO MALARIA

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ASSESSING MALARIA PREVALENCE AND IMMUNE RESPONSE IN “U” AND “V”

SHAPED ECOSYSTEMS

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MANY EPISODES OF MALARIA PER YEAR IN “U” SHAPED VALLEY

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FEW EPISODES OF MALARIA IN “V” SHAPED VALLEY ECOSYSTEM

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CSP-MSP Antibody positive children

0

0.1

0.2

0.3

0.4

0.5

0.6

MAY JUNE JULY AUG SEPT OCT NOV DEC JAN

Time

Pro

po

rtio

n +

ve

MARANI "V"

FORTTERNAN "V"

SHIKONDI "plateau"

IGUHU "U"

EMUTETE "U"

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SENSITIVITY OF HIGHLAND ECOSYSTEMS TO MALARIA EPIDEMIC:

RAINFALL

“U” shaped ecosystems require mean rainfall

of 150mm/month for mosquito populations to

increase

“V” shaped valleys require mean rainfall of

250-300mm/month for mosquito population

to increase

Page 32: PowePoint - Early epidemic detection

Vector breeding and population size in the U and V shaped

valleys

The U shaped valleys has more that twice

the size of breeding habitats compared to the

V shaped valley

The U shaped valley has 3 time more adult

Anopheles gambiae females that the V

shaped valley

Page 33: PowePoint - Early epidemic detection

SENSITIVITY OF HIGHLAND ECOSYSTEMS TO MALARIA EPIDEMICS

IMMUNE PROFILE

The ratio of immune response to malaria

parasites antigens (CSP & MSP) is 1:2.2

between the “V” shaped and “U” shaped

valleys ecosystem

2.2 more people in the “U” shaped valley

have an immune response to malaria

compared to the “V” shaped valley

ecosystem

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CONCLUSION

Human populations in the “V” shaped valleys

are less immune to malaria due to lower

transmission rates and low immunity

Heavy rains are required to precipitate

epidemics in the “V” shaped ecosystems

Plateau ecosystems have a similar response

to malaria as the “V” shaped ecosystems

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TRAINING AND CAPACITY BUILDING FOR USE OF THE MODELS:

NATIONAL EXPERTS TRAINING WORKSHOP, NAIROBI

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PROVINCIAL TRAINING WORKSHOP: KISUMU

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DISTRICT LEVEL TRAINING: DAR ES SALAAM TANZANIA

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District level end user training workshop Uganda

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MODELS USED AT THE SEASONAL CLIMATE OUTLOOK FORUM OF THE GREATER HORN

OF AFRICA TO FOR SIMULATION OF MALARIA EPIDEMICS

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MSC TRAINING

2 MSc students from Tanzania

1 MSc student from Uganda

1 MSc student from Kenya

Page 41: PowePoint - Early epidemic detection

Collaborators• Dr. Andrew K. Githeko (KEMRI)

• Dr. Martha Lemnge (NIMR, Tanzania)

• Mr. Michael Okia (MOH, Uganda)

• Prof. Laban Ogallo (ICPAC)

• COHESU (NGO)

• Dr. John Waitumbi (WRP)

• Dr. John I Githure (ICIPE)

Collaborating Institutions 1. Kenya Medical Research Institute

2. National Institute for Medical Research (NIMR) Tanzania

3. Ministry of Health Uganda

4. Igad Climate Prediction and Application Centre (ICPAC)

5. Community Health Support Program (COHESU)

6. Walter Reed Project, (WRAIR) Kenya International Centre for

7. Insect Physiology and Ecology (ICIPE)