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A Recent Abrupt Decline in the East African Long Rains Bradfield Lyon and David G. DeWitt Presented by: Tufa Dinku tufa@iri.columbia.edu International Research Institute for Climate and Society The Earth Institute at Columbia University. Outline. The Decline The Driver(?) Modeling experiment.

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  1. A Recent Abrupt Decline in the East African Long RainsBradfield Lyon and David G. DeWittPresented by: Tufa Dinkutufa@iri.columbia.eduInternational Research Institute for Climate and SocietyThe Earth Institute at Columbia University

  2. Outline • The Decline • The Driver(?) • Modeling experiment

  3. Rainfall Decline: Regional CAMS_OPI (mm/day) anomaly for Mar-May 2011 CMAP Mar-May(1999-2010 average) anomaly (from 1979-2010 mean) Mar-May total RR , averaged over (10S-12N, 30-53E) Box..

  4. Apr-May PRCP (1998-2008) – (1979-1996) CMAP GPCP

  5. Rainfall Decline: Ethiopia

  6. Rainfall Decline: Ethiopia Annual Rainfall, country average from different number of stations

  7. Spatial Rainfall pattern Weights for leading mode(16.3% of VAR) of March-May precipitation obtained from EOF analysis of CAMS_OPI data for 1979-2011 Principal component time series for March-May leading mode

  8. What is the driver? March-May SST anomaly averaged from 1999-2011, expressed as a standardized departure from the 1971-2000 mean Loadings for the 2nd mode of March-May SST based on an EOF analysis for the period 1950-2011. Principal component time series (1950-2011)

  9. The Driver: East Africa April-May Rainfall Index and Tropical SST Correlation (1979-2010)

  10. Modeling

  11. Modeling Experiment • Multi-model ensemble mean (72 members) MAM RR anomaly (mm/day) from simulations using observed SSTs, averaged over1999-2009. • Ensemble mean (24 members) ECHAM5 precipitation anomaly (mm/day) from idealized runs forced with observed March-May SST anomalies averaged over 1999-2010 for the tropical Indian Ocean only. • As in b, but for model runs forced with SSTs only for the tropical Pacific. Top legend only for a); bottom legend for b and c.

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