A21M-02
Evaluating MJO Event Initiation and Decay in the Skeleton Model using an RMM-like Index

Tuesday, 15 December 2015: 08:15
3008 (Moscone West)
Justin P Stachnik1,2, Duane E Waliser1, Andrew Majda3, Samuel N Stechmann4 and Sulian Thual3, (1)NASA Jet Propulsion Laboratory, Pasadena, CA, United States, (2)University of California, Los Angeles, Joint Institute for Regional Earth System Science and Engineering, Los Angeles, CA, United States, (3)New York University, Courant Institute of Mathematical Sciences, New York, NY, United States, (4)University of Wisconsin Madison, Madison, WI, United States
Abstract:
The Madden-Julian oscillation (MJO) skeleton model is a low-order dynamic model that is capable of simulating many of the observed features of the MJO. This study develops a model- based “MJO” index that is similar to the well-known real-time multivariate MJO (RMM) index to better facilitate comparison between the skeleton model and observational data. Multivariate and univariate empirical orthogonal function (EOF) analyses were performed on the convective heating and zonal wind data taken from the skeleton model for simulations forced with an idealized warm pool and observed sea surface temperatures (SSTs). The leading EOF modes indicated a wavenumber-1 convectively-coupled circulation anomaly with zonal asymmetries that closely resembled the observed RMM EOFs, especially when the model was forced with observed SSTs.  

The RMM-like index was used to compute an MJO climatology and document the occurrence of primary, continuing, and terminating MJO events in the skeleton model. The overall amount of MJO activity and event lengths compared reasonably well to observations for such a simple model. Attempts at reconciling the observed geographic distribution of MJO events were not successful for the stochastic simulations, though the introduction of stochasticity to the convective parameterization was necessary in order to produce composite MJOs that initiate and decay with time scales similar to observations. Finally, analysis indicates that the existence of higher-frequency, eastward travelling waves with larger wavenumbers (k ≈ 12) embedded within the large-scale flow often precedes MJO termination in the skeleton model.