Climate of the Meningitis Belt Sylwia Trzaska 1 , Pietro Ceccato 1 , - - PowerPoint PPT Presentation

climate of the meningitis belt
SMART_READER_LITE
LIVE PREVIEW

Climate of the Meningitis Belt Sylwia Trzaska 1 , Pietro Ceccato 1 , - - PowerPoint PPT Presentation

Climate of the Meningitis Belt Sylwia Trzaska 1 , Pietro Ceccato 1 , Michael Bell 1 , Alessandra Gianinni 1 , Lisa Goddard 1 , M. Ben Mohammed 2 1 The International Research Institute for Climate and Society, Columbia,University, Palisades, NY USA


slide-1
SLIDE 1

Climate of the Meningitis Belt

Sylwia Trzaska1, Pietro Ceccato1, Michael Bell1, Alessandra Gianinni1, Lisa Goddard1, M. Ben Mohammed2

1 The International Research Institute for Climate and Society, Columbia,University,

Palisades, NY USA

2 Université de Niamey, Niger

slide-2
SLIDE 2

Meningitis and Climate

Predicted Probability of Meningitis Epidemics

Molesworth et al., 2003

Dry, dusty environment

slide-3
SLIDE 3

Meningitis and Climate

Predicted Probability of Meningitis Epidemics

Molesworth et al., 2003

Mean rainfall

Rainfall seasonal!!! July-September

slide-4
SLIDE 4
slide-5
SLIDE 5
  • Seasonal reversal of winds
  • In summer, southwesterly flows

bring moisture inland

  • Atlantic Ocean – main source of

moisture

Seasonal cycle of Atmospheric circulation

Mean Low level wind

slide-6
SLIDE 6

West African Monsoon – in brief…

strong decadal variability

strong precipitation gradients

Regional scale Sub-regional scale Finer scales

Space :

Complex structures

  • nset

Louvet et al. 2003

Time :

Northward shift then retreat

slide-7
SLIDE 7

Time Scales of Variability

slide-8
SLIDE 8

West African Monsoon – Impact of Sea Surface Temperatures

SST – principal cause of inter-annual

and decadal-scale variability

Interannual and decadal variability

captured by General Circulation Models Giannini, A, R Saravanan, P Chang, 2003. Science, 320, 1027-1030

slide-9
SLIDE 9

Atmospheric dust production on Seasonal, Interannual and multidecadal Time Scales in the West African Sahel

time series of estimated average monthly dust mass concentrations for

  • Sahara (top)
  • Sahel (bottom)

zones of Niger 1975-99 1950-74 1975-99 1950-74

Ben Mohamed et al. 2007 (subm)

slide-10
SLIDE 10

Climate Change – lots of uncertainties

XX – Pre_ind Future-present

Biasutti and Giannini, GRL 2006

The models that were successful in reproducing the late 20th ceintury drought in Sahel disagree as to future projections in Sahel

Do not reproduce

correctly the main modes of variability and teleconnections (Joly et

  • al. 2006)
slide-11
SLIDE 11

Conclusions

Mean Rainfall

Strong gradients

Seasonality of rain and circulations

  • northward – southward movement of rainy belt and wind convergence

Rainfall variability

Different scales

  • Strong Interannual/Decadal variability linked to SST, reproduced in GCM
  • Climate Change – models disagreement
slide-12
SLIDE 12

Environmental Factors

E.g. TOMS w 1-20

  • Northaward progression
  • f Meningitis linked to

highest temperatures, in the region of convergence between Harmattan and southwesterlies

  • Highest dustiness (not

shown)

  • NOT lowest humidity
  • Termination linked to

arrival of moister, cooler and cleaner air