Potential Predictability of the Madden Julian Oscillations (MJO) in the ISVHE multi-model framework

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UCLA Potential Predictability of the Madden Julian Oscillations (MJO) in the ISVHE multi-model framework Neena Joseph Mani 1,2 1 Joint Institute for Regional Earth System Sci. & Engineering / UCLA, USA 2 Jet Propulsion Laboratory, California Institute of Technology, USA June Yi Lee 3,4, Duane Waliser 1,2, Bin Wang 3 and Xianan Jiang1,2 3 International Pacific Research Center, University of Hawaii, Honolulu 4 Pusan National University, South Korea and Participating modeling groups Based on Neena, J.M., J-Yi Lee, D. Waliser, B. Wang and X. Jiang (2014): Predictability of the Madden Julian Oscillation in the Intraseasonal Variability Hindcast Experiment (ISVHE), Accepted for publication in J Climate. AMS 31st Conference on Hurricanes and Tropical Meteorology, 31 March-4 April 2014, San Diego, CA.

CLIVAR/ISVHE Intraseasonal Variability Hindcast Experiment The ISVHE is the FIRST/BEST coordinated multi-institutional ISV hindcast experiment supported by APCC, NOAA CTB, CLIVAR/AAMP & MJO WG/TF, and AMY. ECMWF EC SNU PNU CMCC NCEP JMA CWB GFDL NASA UH IPRC ABOM Supporters CTB Additional support provided to this work by

Numerical Designs and Objectives Control Run Free coupled runs with AOGCMs or AGCM simulation with specified boundary forcing for at least 20 years Daily or 6-hourly output ISV Hindcast EXP ISV hindcast initiated every 10 days on 1st, 11th, and 21st of each calendar month for at least 45 days with more than 6 ensemble members from 1989 to 2008 Daily or 6-hourly output YOTC EXP Additional ISO hindcast EXP from May 2008 to Sep 2009 6-hourly output Better understand the physical basis for ISV prediction develop optimal strategies for multimodel ensemble ISV. Identify model deficiencies in predicting ISV and find ways to improve models convective and other physical parameterization. Determine ISV s modulation of extreme hydrological events and its contribution to seasonal and interannual climate variation. Determine the potential and practical predictability of MJO in a multi-model frame work.

Presentation Objectives Primary Objective Present Estimates of MJO Predictability Employ better & more models Use community standard (WH 04) MJO index Consider ensemble as a better MJO model Revisit e.g. Waliser et al. (2003), Fu et al. (2007), Pegion and Kirtman (2008) Secondary Objectives Quantify gap between predictability and prediction skill Examine ensemble fidelity on enhancement of prediction skill Definitions: Predictability characteristic of a natural phenomena often estimated with models Prediction skill characteristic of a model and its forecast fidelity against observations Ensemble - only refers to single model s ensemble of forecasts not MME

Signal to Error ratio estimate of MJO/ISV predictability Control run Perturbed Forecasts Initial Condition Differences Based On Forecasts 1 Day Apart Signal (L=25 days) Mean square Error Signal Error As in Waliser et al. (2003, 2004); Liess et al. (2005); Fu et al. (2007) Except using a combined RMM1 & RMM2 index Bivariate estimates of Signal and Error 2 k1 k2 2 k1 k2 2 E ij=(rmm1ij RMM1ij ) +(RMM2ij RMM2ij ) L S =1/51 ( RMM1i k j+t ) +( RMM2i k j+t ) 2 ijk 2 t = L 2

MJO Predictability & Prediction Skill Estimates Single Member Approach Error -- Difference between hindcast combined RMM1 and RMM2 values for two ensemble members. Comparison Provides Ensemble Mean Approach Prediction Skill Predictability A measure of the enhanced skill provided by the given center s/model s ensemble An improved(?) estimate based on a better MJO/ISV forecast model Error -- Difference between hindcast combined RMM1 and RMM2 values for an individual ensemble member and the ensemble mean of all other members. Signal Error X ij = 0 Predictability = Model Control Prediction Skill = Observations Mean square Error

Description of Models and Experiments One-Tier System ISO Hindcast Model Period Ens No Initial Condition ABOM1 POAMA 1.5 & 2.4 (ACOM2+BAM3) 1980-2006 10 The first day of every month ABOM2 POAMA 2.4 (ACOM2+BAM3) 1989-2009 11 The 1st and 11th day of every month ECMWF ECMWF (IFS+HOPE) 1989-2008 5 The first day of every month CMCC CMCC (ECHAM5+OPA8.2) 1989-2007 5 The 1st 11th and 21st day of every month JMA JMA CGCM 1989-2008 5 Every 15th day NCEP/CPC CFS v1 (GFS+MOM3) 1981-2008 5 The 2nd 12th and 22nd day of every month NCEP/CPC CFS v2 1999-2010 5 The 1st 11th and 21st day of every month SNU SNU CM (SNUAGCM+MOM3) 1990-2008 4 The 1st 11th and 21st day of every month

MJO Predictability in the ISVHE models Single Member predictability estimates 24 days Ensemble Mean predictability estimates 43 days Signal- Red curve Single member error- Blue curve Ensemble mean error-black

MJO prediction vs predictability----where do we stand? * Predictability estimates are shown as +/- 5 day range Skill ~ 2 weeks Skill ~ 2-3 weeks Pred ~ 3-4 weeks Pred ~ 5-7 weeks Significant skill remaining to be exploited by improving MJO forecast systems (e.g. ICs, data assimilation, model fidelity) High-quality ensemble prediction systems crucial for MJO forecasting.

Predictability dependence on MJO phase and Primary/Secondary a) Hindcasts are grouped according to the RMM phase during hindcast initiation b) Hindcasts are grouped into those associated with primary/secondary MJO events using the RMM index based classification of Straub (2012) Only 3 (of 8) models exhibit predictability phase dependence (ABOM1, ABOM2,ECMWF) -> E. Hemisphere convection more predictable (e.g. Phases 2,3,6,7) Hindcasts initiated from secondary MJO events indicate (~5 days) greater predictability than those from primary events in 4 (of 8) models. (ABOM2, ECMWF, JMAC,CFS1)

Ensemble fidelity and improvement in prediction skill for MJO In a statistically consistent ensemble, the RMS forecast error of the ensemble mean (dashed) should match the standard deviation of the ensemble members (ensemble spread) (solid). Ensemble Fidelity measures the level of dispersion for MJO -average difference between the solid and dashed curves over the first 25 days hindcast Prediction systems with greater level of dispersion for MJO show more improvement in the ensemble mean prediction skill over the individual ensemble member hindcast skill!

Summary The predictability of winter MJO is investigated in the ISVHE hindcasts of eight coupled models. Predictability estimates are made for the individual ensemble member hindcast as well as for the ensemble mean hindcasts. Most models show a 20-30 day predictability for indiviual ensemble member hindcasts while the ensemble mean hindcasts show a 40-50 day predictability. The predictability of MJO is not very sensitive on the MJO phase at the time of hindcast initiation. Three of the eight models show a higher predictability for MJO phases over the Indian Ocean and Western Pacific. Present day MJO prediction capabilities can be extended further by at least one week for individual ensemble forecasts in most models. Ensemble mean prediction skill improvement holds more promise. In addition to improving the dynamic models, devising ensemble generation approaches tailored for the MJO would have a great impact on MJO prediction. Neena J.M., J-Yi Lee, D. Waliser, B. Wang and X. Jiang, 2014: Predictability of the Madden Julian Oscillation in the Intraseasonal Variability Hindcast Experiment (ISVHE), J Climate (Accepted for publication).

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