Abstract:
A case sweep simulation of winter MJOs through
2003 - 2012, including the two MJO cases observed in CINDY/DYNAMO, is conducted
using a global non-hydrostatic model NICAM (Satoh et al. 2008), powered by the
new peta-flops computer "K" (RIKEN AICS,
Kobe, Japan). A total of 54 initial dates are objectively chosen for 19 winter (October
– March) MJO cases based on Real-time Multivariate MJO index 1 (RMM1) and RMM2
diagrams (Wheeler and Hendon 2004). The average skill limit of the MJO
reproduction was measured by bivariate correlations (Lin et al. 2008, Gottschalck et al. 2010). The duration of reproduction
skill (the duration that the bivariate correlation between
observation/reanalysis and NICAM stays above 0.6) was as long as 27 days.
Figure 1 shows OLR Hövmoller diagrams of an MJO case
observed intensively in CINDY/DYNAMO field campaign. The NICAM simulation is
successful in reproducing the eastward migration of the highly convective
envelope throughout the 40 day integration. On the other hand, there were also
cases in which NICAM produced relatively poor or no eastward propagation of the
MJO. The MJO ensemble dataset allows our studies to proceed beyond case studies
and distinguish the essence of the MJO from case-to-case varieties.
Fig. 1. Equatorial Hovmöller
diagrams of OLR averaged over 5S - 5N, date starting from 15 Nov 2011. Left)
NOAA satellite and right) NICAM.