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Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science & Engineering (JIFRESSE) / UCLA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 7 th Latent Heating Workgroup / NASA PMM Science Team Meeting, Aug 05, 2014

Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

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Page 1: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations

UC

LA

Xianan Jiang

Joint Institute for Regional Earth System Science & Engineering (JIFRESSE) / UCLAJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA

7th Latent Heating Workgroup / NASA PMM Science Team Meeting, Aug 05, 2014

Page 2: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Wang (2005)

x(East)

PBL

z

y(South)

EQ

R-Low

K-Low

SinkingSinking

Warm

R-Low

CONV

Wave-CISK

Ekman-CISK

WISHE

Role of Diabatic Heating for the MJO

“Stratiform-instability”

“Radiation-convection feedback”

Page 3: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Jiang et al. 2011MJO Phases

hPa

Observed Q1 of the MJO

Page 4: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

20 Yr Climatological Simulations(1991-2010 if AGCM)

6-hr, Global OutputVertical Structure, Physical Tendencies

Commitments: About 24 Modeling Groups with 27 AGCM and/or CGCMs

Model MJO FidelityVertical structure

Multi-scale Interactions:(e.g., TCs, Monsoon, ENSO)

UCLA/JPLX. Jiang

D. Waliser

2-Day MJO HindcastsYOTC MJO Cases E & F (winter 2009)*Time Step, Indo-Pacific Domain Output

Very Detailed Physical/Model Processes

Heat and moisture budgetsModel Physics Evaluation

(e.g. Convection/Cloud/BL) Short range Degradation

Met OfficeP. XavierJ. Petch

20-Day MJO HindcastsYOTC MJO Cases E & F (winter 2009)*

3-hr, Global OutputElements of I & II

MJO Forecast SkillState Evolution/Degradation

Elements of I & II

NCAS/Walker in.N. KlingamanS. Woolnough

*DYNAMO Case TBD

I.

II.

III.

Model Experiment Science Focus Exp. POC

Vertical Structure and Diabatic Processes of the MJO: Global Model Evaluation Project

MJO Task Force/YOTC and GASS

www.ucar.edu/yotc/mjodiab.html

Page 5: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Model Horizontal Resolution Vertical Resolution Cumulus Scheme Notes

1 01_NASAGMAO_GEOS5 0.625o lon x 0.5o lat 72 RAS (RAS; Moorthi & Suarez 1992)

2 03a_SPCCSM (CAM3 + POP) T42 (~2.8o) 30 Super-parameterization (Khairoutdinov & Randall 2003)

3 03b_SPCAMP_AMIP T42 30 (Khairoutdinov & Randall 2001) 1986-2003

4 04_GISS_ModelE2 2.75o lon x 2.2o lat 40 Kim et al. (2012), Del Geino et al. (2012)

5 05_EC_GEM ~1.4o 64

6 07_MIROC T85 (~1.5o) 40 Chikira scheme (Chikira and Sugiyama 2010) AMIP SST 1986-2005

7 10_MRI-GCM T159 48 (Pan and Randall 1998)

8 11_CWB_GFS T119 (~1o) 40 (RAS; Moorthi & Suarez 1992)

9 14_PNU_CFSv1 T62 (~2o) 64 (RAS; Moorthi & Suarez 1992)

10 16_MPI_ECHAM6 (ECHAM6 + MPIOM) T63 ( ~2o) 47 (Tiedtke 1989; Nordeng 1994)11 17_MetUM_GA312 21_NCAR_CAM513 22_NRL_NAVGEMv.01 T359 (37km) 42 (Hong and Pan 1996; Han and Pan 2011)14 24_UCSD_CAM T42 (~ 2.8o) 30 (Zhang & McFarlane 1995)15 27_NCEPCPC_CFSv2 T126 (~ 1o) 64 (Hong & Pan 1998)16 31a_CNRM_AM

T127 (~1.4o) 31 Bougeault (1985) 17 31b_CNRM_CM (CNRM_AM+ NEMO)

18 31c_CNRM_ACM

19 34_CCCma_CanCM4 T63(?) 35(?) (Zhang & McFarlane 1995)

20 35_BCCAGCM2.1 T42 (~2.8 deg) 26 (Wu et al 2011)21 36_FGOALS2.0-s R42 (2.8olonx1.6olat) 26 (Tiedtke 1989; Nordeng 1994)22 37_NCHU_ECHAM5-SIT T63 31 (Tiedtke 1989; Nordeng 1994)

23 39_TAMU_Modi-CAM4 (CCSM4) 2.5 o lon x 1.9 o lat 26 (Zhang & McFarlane 1995) Idealized tilted heating

24 40_ACCESS (modified METUM) 1.875o lon x 1.25o lat 85 (Gregory and Rowntree 1990)25 43_ISUGCM T42 (~ 2.8o) 18 (Zhang & McFarlane 1995)26 44_LLNL_CAM5ZMMicro27 45_SMHI_ecearth3 T255(80km) 91 IFS cy36r4

Participating GCMs for Climate Simulation (Exp Component I)

Page 6: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Lag-regression of rainfall with Indian Ocean (70-90E; 5S-5N) base point

20-100day filtered

dash line – 5 m/s

Jiang et al. 2014

Page 7: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Skill Score by Rainfall Lag-Regression Pattern(Indian Ocean & western Pacific averaged)

Top 25% models Bottom 25% models

Page 8: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

Vertical MJO Structures in Good and Poor GCMs

u’ (m/s) T’ (k) w’ (hPa/s) Q’ (k/day) q’(g/kg)

(10oS-10oN)

Good GCMs

Poor GCMs

ERA-Interim

Jiang, X., et al., 2014: Vertical Structure and Physical Processes of the Madden-Julian Oscillation: Exploring Key Model Physics in Climate Simulations, JGR-Atmos, submitted.

Page 9: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

GPM Rain/LH for MJO studies

• 0.1 deg, 30mins, 60S-60N GPM• Improved rainfall observations, algorithms for

LH estimates, to depict MJO processes and constrain GCM physics

Page 10: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science
Page 11: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

“Pre-conditioning” of the Eastward Propagating MJO

Rain (mm day-1)

Divergence (s-1)

Cloud water (10-5 kg kg-1)Q’ (k/day)

Specific humidity (g/kg)

Rain (mm day-1)

Jiang et al. 2011

MJO Phase 3

Page 12: Vertical Heating Structure of the MJO Based on TRMM Estimates and Multi-model Simulations UCLA Xianan Jiang Joint Institute for Regional Earth System Science

u’ (m/s) T’ (k) w’ (hPa/s) Q’ (k/day) q’(g/kg)

Vertical structures of the MJO (ERA-Interim; lag-0 regression)

Corr=0.79

Corr=0.77 Corr=0.51 Corr=0.78 Corr=0.70 Corr=0.65

Pattern Correlations of Vertical Profiles

MJO

Sco

re

MJO

Sco

re

Average Pattern Correlations of Five Variables

Model Skill in Vertical Structure vs MJO Fidelity u’ T’ w’ Q’ q’

Jiang et al. 2014