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Analysis and modelling of the 2010 Pakistan heavy precipitation events Milind Mujumdar Centre for Climate Change Research (CCCR), Indian Institute of Tropical Meteorology (IITM), Pune. http://www.tropmet.res.in P. Priya, T.P. Sabin, R. Krishnan
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2010 Pakistan floods 2011 - Hauz et.al., Webster et. al., Hong et. al, Lau and Kim, Saeed et. al.
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TRMM Rainfall anomalies for JJAS 2010 (mm) Clim+ 0.5 σ Hong et al. (GRL, 2011)
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TRMM (Rainfall) and NCEP (Moisture Transport) JJAS Climatology TRMM (Rainfall) and NCEP (Moisture Transport) “2010” JJAS Anomalies
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Asian summer monsoon response to La Nina events under warming climate Mujumdar et al. (2012) - Meteorological Applications Special issue on Asian summer monsoon Composite SST anomaly (12 La Nina cases ) (mm) ( 0 C) NCEP OI-SST Anomaly for JJAS 2010 ( 0 C)
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JJAS mean sea level pressure (hPa) 2010 CLIM (JJAS mslp 2010) – (cmp La nina) Anomalies hPa
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2010 JJAS OLR anomalies Composite of olr anomaly (La Nina)
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Zonal Circulation Red : Climatology Black : 2010 Anomalous Zonal Circulation : 2010 Averaged over 10N-20N
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La Niña events 2010 Total – 20 / JJAS - 12 Total – 45 / JJAS > 30 Rainfall - ~ 108% of LPA Rainfall - ~ 101% of LPA Extended Analysis
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Averaged Rainfall over Indo-Pak region (65-76 E; 28-36 N) during JJAS Intense Rainfall events Accumulated La Nina event
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EOF-MSLP-JJAS PC1
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b) without ENSO component a) with ENSO component SST anomaly for JJAS 2010
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LMDZ-AGCM “CLIM” ensemble JJAS mean Rainfall and moisture transport LMDZ-AGCM “2010” ensemble JJAS anomalies Rainfall and moisture transport
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LMDZ-AGCM “2010” ensemble JJAS mean Rainfall and moisture transport LMDZ-AGCM “with ENSO” ensemble JJAS anomalies (Excluding SST warming trend) Rainfall and moisture transport
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LMDZ-AGCM “without La Nina” JJAS anomalies (retaining Indian ocean warming trend) Rainfall and moisture transport LMDZ-AGCM “2010” ensemble JJAS anomalies Rainfall and moisture transport
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Summary 1.West ward shift of WPSH - Asian summer monsoon response to La Nina events under warming climate. 2.Westward shift of monsoon circulation and large-scale suppression of convection over Indo-Pacific sector during La Nina episodes. 3.Northward transport of moisture over northwest Indo-Pak region from Indian Ocean 4. Complex interactions between tropical and sub-tropical circulations – extreme rainfall events over subtropical Indo-Pak region. Scope for future work Ensemble simulation experiments for understanding the role of La Nina episodes under warming climate in the evolution of heavy flood events over South Asia. CORDEX-SA - cccr.tropmet.res.in
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Thank you
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La Niña events 2010 Total – 20 / JJAS - 12 Total – 45 / JJAS > 30 Rainfall - ~ 108% of LPA Rainfall - ~ 101% of LPA Extended Analysis
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EOF-OLR(-240)-dly-clm-jjas EOF-dOLRa-lanina-jjas
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850 hPa wind JJAS anomalies La Nina Composite 200 hPa wind 2010
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850 hPa wind JJAS anomalies 200 hPa wind 2010
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