Application of a Hybrid Dynamical-Statistical Model for Week 3 and 4 Forecast of Atlantic/Pacific Tropical Storm and Hurricane Activity Jae-Kyung E. Schemm.

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Presentation transcript:

Application of a Hybrid Dynamical-Statistical Model for Week 3 and 4 Forecast of Atlantic/Pacific Tropical Storm and Hurricane Activity Jae-Kyung E. Schemm and Hui Wang Climate Prediction Center, NCEP/NWS/NOAA NGGPS External PI Meeting July 17, 2015 NCWCP, College Park, MD 1

Tropical Storm Activity Prediction at CPC NOAA Hurricane Season Outlooks for ATL/ENP basins issued since CFS-based hybrid dynamical-statistical prediction system developed in Dynamic prediction system with the T382 CFS introduced in 2009; one of early CTB projects - The dynamic system upgraded to the T382 CFSv2 in 2014 Experimental Intra-seasonal TS activity prediction introduced in 2015 to support CPC Global Tropics Hazards Outlooks; development partly funded by CPO/MAPP program - Week 1 – 4 TS activity prediction based on the CFSv2 45-day forecast - Model TS statistics and false alarm climatology constructed with the CFSv2 45-day hindcast 2

The use of dynamical models since 2008, especially the CFS, has contributed to a large improvement in outlook accuracy.

Hindcast Results Storm Count Anomaly Correlations for Week ENP, WNP, SI and SP show highest week 1 values ( ) ATL brought down by two bad years (2002 and 2003) 2005 also seems to be a difficult year in many basins (but surprisingly not ATL) Currently looking into wind shear forecasts to account for dips in skill Horizontal lines represent average correlation

Climatological storm track genesis skill as function of lag time in days with the CFSv2 hindcast runs for Lag days -6 to -1 (left of day 0) show the model’s ability to predict both storm genesis and track Lag days 0 to 8 (right of black line) show the model’s ability to predict the storm track. At 0, storm is present in initial conditions.

Project Objective 1. Develop a hybrid dynamical-statistical model for weeks 3 and 4 TS and hurricane activity forecast with the CFSv2 45-day hindcast data for A hybrid prediction system has been in operation since 2009 at CPC for the NOAA Hurricane Season Outlooks. 2. Test the hybrid model for real-time prediction for the 2016 hurricane season. 3.Implement the model into operations at CPC in Contribute towards CPC’s effort for developing Week 3 and 4 forecast products. 6

Hybrid Dynamical-Statistical Prediction System A Multiple regression relationship established between weekly tropical storm activity over the Atlantic/Pacific basins and predicted circulation variables. Predictors: Weekly wind shear (U200-U850), SST, mean sea level pressure, 500hPa height and relative humidity, and two MJO indices Predictands: Weekly total number of named storms and hurricanes CFSv2 Hindcast data: Period; IC Months; April through November Hindcast evaluations will be performed in a cross-validation mode Ref: Wang, H., J. E. Schemm, A. Kumar, W. Wang, L. Long, M. Chelliah, G. D. Bell, and P. Peng, 2009: A Statistical Forecast Model for Atlantic Seasonal Hurricane Activity Based on the NCEP Dynamical Seasonal Forecast., J. Climate, 22, 4481–

Project Work Plan Year 1 1. Establish a multiple regression relationship among TS activity, SST and atmospheric circulation variable indices. 2. Develop the hybrid forecast model for weeks 3 and 4 TS activity prediction based on the CFSv2 45-day hindcast for , including the cross-validated evaluations. Year 2 1. Real-time forecast test during the 2016 hurricane season 2. Operational implementation at CPC for the 2017 season 8

Some Results from Preliminary Analyses 9

List of Utilized Data CFSR for 1999 – 2014 NOAA OISST v2 for 1999 – 2014 Best Track TC data from NHC and JTWC CFSv2 45-day hindcast data for 1999 –

 Correlation between weekly TC activity and corresponding weekly SST/atmospheric circulation fields  Weekly mean data: 7-day average from Sunday to Saturday  Total 34 weeks from May to December  Weekly SST: NOAA OISST v2  Atmospheric fields (CFSR): vertical wind shear U200–U850, 500- mb height and relative humidity, sea level pressure  Weekly TC activity: sum of the days of each TC over the 7-day period  Relationship between Weekly TC activity and the MJO phase A similar correlation analysis will be performed using the observed weekly TC activity and the SST/circulation from the CFSv2 45-day hindcasts. The regions of high correlations will be used to make up for area-averaged indices as potential predictors. Observational Analysis

Correlation between Weekly SST and Weekly TC Activity Weekly TC activity smoothed Example of Atlantic weekly TC activity Smoothed vs. Unsmoothed Color shadings (correlation > 0.1): Above the 95% significance level /cpc/namecpt/hui/2015_R2O/SST

Correlation between Weekly SST and Weekly TC Activity Weekly TC activity unsmoothed Example of Atlantic weekly TC activity Smoothed vs. Unsmoothed The correlations of SST with the unsmoothed TC activity are weaker.

Correlation between Weekly Wind Shear and Weekly TC Activity Weekly TC activity smoothed Vertical wind shear = U200 – U850

Correlation between Weekly Wind Shear and Weekly TC Activity Weekly TC activity unsmoothed Unlike SST field, vertical wind shear is also highly correlated with the unsmoothed TC activity.

Correlation between Weekly Sea Level Pressure and Weekly TC Activity Weekly TC activity smoothed The weekly TC activity is negatively correlated with local SLP.

Effect of MJO on Weekly TS Activity  Daily MJO index  Weekly MJO index (7-day average of daily MJO index)  Composite of weekly TCs based on 8 MJO phases

MJO (Wheeler and Hendon 2004) Combined EOFs of u850, u200, and OLR Averaged over 15 o S–15 o N Daily data, 01 Jan 1999–31 Dec 2014 NOAA Interpolated OLR, 1999–2013 CFSR OLR for 2014 CFSR u850 and u200, 1999–2014 Anomaly w.r.t daily climatology 20–100-day band-pass filter prior to EOF OLR U850 U200 PC1 PC2 Daily MJO Index Normalized PC1 and PC2 Weak MJO Weak MJO: (PC1 2 + PC2 2 ) 1/2 < 1

PC2 Weak MJO Phase 1 Phase 2 Phase 3 Phase 4 Phase 5 Phase 6Phase 7 Phase 8 PC1 MJO Phases: 8 7-day mean index Normalized May – December 35 weeks (1 May – 31 December)

Composite of OLR Anomaly for Different MJO Phases Based on Weekly MJO Index May – Dec, 1999 – 2014 Weekly OLR anomaly: unfiltered

Composites of TC Genesis and TC Activity Based on MJO Phase

CFSv2 45-day Hindcast Evaluation 22

Wind shear: U200 – U850  Anomaly correlation between CFSv2 45-day hindcasts and CFSR  Weekly data: 7-day average from Sunday to Saturday  May – November: 31 weeks  1999 – 2012  Different leads: week 1 to week 4 Correlation between observed weekly TC activity and CFSv2 45-day hindcast wind shear  Atlantic, E. Pacific, W. Pacific TC activities  OBS: CFSR  CFSv2 45-day hindcasts: from week 1 to week 4  Potential predictors: area-average over regions with high correlations

Sea Level Pressure (SLP)  Anomaly correlation between CFSv2 45-day hindcasts and CFSR  Weekly data: 7-day average from Sunday to Saturday  May – November: 31 weeks  1999 – 2012  Different leads: week 1 to week 4 Correlation between observed weekly TC activity and CFSv2 45-day hindcast SLP  Atlantic, E. Pacific, W. Pacific TC activities  OBS: CFSR  CFSv2 45-day hindcasts: from week 1 to week 4  Potential predictors: area-average over regions with high correlations

Summary Evaluation of the CFSv2 45-day hindcasts for the hybrid model formulation for Weeks 1 – 4 TS activity prediction in progress. Multiple regression relationship for the weekly TS activity will be established based on the CFSv2 hindcast data for The hybrid model performance will be evaluated in cross-validation mode with the hindcast experiment. It is planned to start the real-time prediction experiment based on this hybrid system during the 2016 tropical storm season. It is hoped to complement the dynamic weekly TS activity prediction system based on CFSv2. This project contributes towards the NGGPS/R2O objective on the development of forecast products for Week 3 and 4. CFSv2 diagnostics conducted in this project will contribute towards development of the next version of CFS. 33