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EAST ASIAN MONSOON

EAST ASIAN MONSOON. Anitha Denny Girish Jisung Latha Nuncio Soojin Xiaobin Xiefei. Nearly a third of the world Population is affected. PRECIPITATION CLIMATOLOGY EASM REGION. mm/day. Observation. Standard deviations of June-August precipitation. model. diff. model. diff.

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EAST ASIAN MONSOON

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  1. EAST ASIAN MONSOON Anitha Denny Girish Jisung Latha Nuncio Soojin Xiaobin Xiefei

  2. Nearly a third of the world Population is affected.

  3. PRECIPITATION CLIMATOLOGY EASM REGION mm/day

  4. Observation Standard deviations of June-August precipitation

  5. model diff model diff Difference of June-August precipitation from June-August climatology MRI-CGCM Had-GEM-CC Had-GEM-ES NASA-GISS model diff model diff MPI-ESM-LR NCC-NOR IPSLCM5B-LR CERFACS MPI-ESM-LM NOAA,CM3 MIROC-5 INM-CM4 MIROC-ESM NOAA,esm2g IPSL-5A-LR IPSL-5A-MR MIROC-CHEM NOAA,esm2m

  6. Precip-JJA NINO3.4 SST

  7. SUMMARY Variability biases in the precipitation are strong towards the south of The EASM region. However some models have a better representation of it eg. HadGEM, MPI and GFDL models. SST during JJA is best captured by HadGem models. But DJF SSTs are not well represented. Large uncertainty in simulating northwest Pacific SSTs by all models possibly because of the inadequate representation of Kuroshio dynamics. Tele-connections of ENSO is manifested by Rossby wave trains (Wang, etal., 2001). It need to be seen how these wave trains are represented in models

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