Title: MJO Simulation Diagnostics Application of Diagnostics to Models Part II
1MJO Simulation Diagnostics Application of
Diagnostics to ModelsPart II
Eric D. Maloney1 and the US CLIVAR MJO Working
Group2 1Oregon State University 2http//www.uscliv
ar.org/Organization/MJO_WG.html
Special thanks Daehyun Kim
2Application to climate models
Motivation for Diagnostics
- Level 1
- Basic indication of spatial and temporal
intraseasonal variability that can be easily
understood and/or calculated by the non-MJO
expert. - Ease of use dictated that the analytic procedures
be as simple as possible. - Level 2
- Provide a more comprehensive diagnosis of the MJO
- Physical relationships
3Application to climate models
Goals/Motivation of this Talk
- Demonstrate ability of diagnostics to distinguish
between good and bad MJO simulations - No models are perfect, and so I will tend to be
evenhanded in criticism of models - The SP-CAM and ECHAM models appear to produce the
most realistic MJO simulations of the models we
analyzed
4Application to climate models
Outline
- Multivariate EOF-based indices (e.g. Wheeler and
Hendon 2004) - Composite structure in several variables
- Others, if time
- Conclusions
5Application to climate models
Combined EOF Indices, NCEP 1 and AVHRR
EOF1
U200
Variance Explained
U850
OLR
EOF2
6Application to climate models
Combined EOF Indices, Models
SP-CAM
CAM3.5
7Application to climate models
Variance Explained
SP-CAM
CM2.1
Obs
ECHAM
CFS
8Application to climate models
Lag Correlation of Leading PCS
SP-CAM
CM2.1
Obs
CFS
ECHAM
9Application to climate models
Coher2, Phase Between the Leading uPCs
Projections of EOFs Onto Unfiltered Data
CM2.1
SP-CAM
Obs
ECHAM
CFS
10Application to climate models
Phase Diagram Relating PC1 and PC2 Observations
Selection Criteria
PC2
PC1
11Application to climate models
November-April U850 Composites NCEP1
Phase 1
Phase 2
Phase 3
Phase 4
Phase 5
Phase 6
Phase 7
Phase 8
12Application to climate models
November-April U850 Composites Models
SP-CAM
CM2.1
13Application to climate models
May-October U850 Composites NCEP1
Local E. Pacific Maximum
Northward and Eastward propagation
14Application to climate models
May-October U850 Composites Models
CAM3.5
SP-CAM
15Application to climate models
November-April Precip Composites GPCP
16Application to climate models
November-April Precip Composites Models
ECHAM
GEOS5
17Application to climate models
May-October Precip Composites GPCP
18Application to climate models
May-October Precip Composites Models
ECHAM
CFS
19Application to climate models
Specific Humidity Composite Observations
Kiladis et al. (2005)
1.1 g kg-1
20Application to climate models
Specific Humidity Composite NCEP1 Models
ECHAM
NCEP1
SP-CAM
21Application to climate models
Omega Composite NCEP1 Models
CM2
SP-CAM
NCEP1
22Application to climate models
OLR and LHFLX Composites NCEP1/AVHRR Models
NCEP1
ECHAM
CAM3.5
23Application to climate models
Conclusions
- Demonstrate ability of diagnostics to distinguish
between good and bad MJO simulations - No models are perfect, although a couple of
models have nice successes at simulating the MJO
(SP-CAM, ECHAM) - Diagnostics allow first-glance looks at physical
relationships underlying good and less-good MJO
simulations
24Thanks!
25Application to climate models
OLR and SST Composites TMI/AVHRR Model
CFS
TMI/AVHRR
26Application to climate models
Coher2 and Phase, Symmetric OLR vs. U850
SP-CAM
NCEP1 U850/AVHRR
27Application to climate models
Climate models