Extended range prediction during 2013 season Using Ensemble Prediction System based in CFSv2 And

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Extended range prediction during 2013 season Using Ensemble Prediction System based in CFSv2 And GFSv2 forced with Bias corrected CFSv2 forecasted SST Extended Range Prediction Group Indian Institute of Tropical Meteoro

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Extended range prediction during 2013 season Using Ensemble Prediction System based in CFSv2 And GFSv2 forced with Bias corrected CFSv2 forecasted SST. Extended Range Prediction Group Indian Institute of Tropical Meteorology. Strategy:. Ensemble Prediction using CFS/GFSv2 (T126). - PowerPoint PPT Presentation

Transcript of Extended range prediction during 2013 season Using Ensemble Prediction System based in CFSv2 And

Page 1: Extended range prediction during 2013 season Using Ensemble Prediction System based in CFSv2 And

Extended range prediction during 2013 season

Using Ensemble Prediction System based in CFSv2

AndGFSv2 forced with Bias corrected CFSv2 forecasted SST

Extended Range Prediction GroupIndian Institute of Tropical Meteorology

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Ensemble Prediction using CFS/GFSv2 (T126)

• Ocean and Atmospheric Initial conditions (IC) are obtained from NCEP.

• Technique was developed to perturb ICs to generate 11 members. (Abhilash et al., 2013)

• Model has been integrated for 45 days for each 11 ICs at five day intervals starting from 1st May (Eg: 01May, 06May, 11May, 16May, 21May, 26May,31May, 05Jun........etc).Climatology has been calculated from 10-year hindcast climatology.

• Bias correction in daily forecasted SST from CFSv2 for each lead time has been done by removing the daily mean bias for corresponding lead time (model climatology-observed climatology) from forecasted daily SST. (Sahai et al., 2013; Abhilash et al., 2013)

Strategy:

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Daily evolution of rainfall and wind at 850hPaCFS forecast based on IC=21 May 2013

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Daily evolution of rainfall and wind at 850hPabias corrected CFS forecasted SST forced GFS Forecast based on IC=21 May 2013

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Daily evolution of rainfall and wind at 200hPaCFS forecast based on IC=21 May 2013

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Daily evolution of rainfall and wind at 200hPabias corrected CFS forecasted SST forced GFS Forecast based on IC=21 May 2013

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CFS forecast based on IC=21 May 2013

Actual Anomaly

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GFS forecast based on IC=21 May 2013

Actual Anomaly

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CFS-GFS Forecast Over Homogenous RegionsMZI, CEI, NEI, NWI & SPI

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CFS GFS

MZI

P1

P2

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CFS GFS

MZI

P3

P4

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CFS GFS

CEI

P1

P2

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CFS GFS

CEI

P3

P4

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CFS GFS

NEI

P1

P2

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CFS GFS

NEI

P3

P4

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CFS GFS

NWI

P1

P2

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CFS GFS

NWI

P3

P4

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CFS GFS

SPI

P1

P2

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SPI

CFS GFS

P3

P4

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How MISO is computed: (ref: Suhas etal., 2012)

Extended EOF analysis is carried out similar to Wheeler and Hendon 2004 using standardized rainfall anomalies up to lag -15 days, averaged between 60-95E for the latitudes -12 to 30. The rainfall anomalies for the lag days are appended side by side to create the extended data matrix.

The EOF analysis is carried out using IMD-TRMM merged data from 1998-2011. The real time data for 2013 is projected onto the EOFs created from the 14 years of past data.

The amplitude of EOF1 and EOF2 (PC1 and PC2 ) are plotted in a PC1/PC2phase space similar to Wheeler Hendon 2004 to get an idea of the evolutionof ISO and its strength.

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Composite Rainfall anomalies in different phases

Phase1:Peninsular India

Phase2:Central India

Phase3:Central India

Phase4:North India

Phase5:Foothills

Phase6:South Indian Ocean

Phase7:Indian Ocean

Phase8:Southern tip

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CFS GFS(bias corrected)

MISO monitoring and forecast for next 25 days

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CFS GFS(bias corrected)

MISO monitoring and forecast for next 25 days