Stochasticity of Convection in Giga-LES Data

Monday, 18 April 2016: 4:30 PM
Ponce de Leon C (The Condado Hilton Plaza)
Boualem Khouider, Univ. of Victoria, Victoria, BC, Canada; and M. De La Chevrotière and A. J. Majda

The poor representation of tropical convection in general circulation models (GCMs) is believed to be responsible for much of the uncertainty in the predictions of weather and climate in the tropics. The stochastic multicloud model (SMCM) was recently developed by Khouider et al. (2010) to represent the missing variability in GCMs due to unresolved features of organized tropical convection. The SMCM is based on three cloud types (congestus, deep and stratiform), and transitions between these cloud types are formalized in terms of probability rules that are functions of the large-scale environment convective state and a set of seven arbitrary cloud timescale parameters. Here, a statistical inference method based on the Bayesian paradigm is applied to estimate these key cloud timescales from the Giga-LES dataset, a 24-hr large-eddy simulation (LES) of deep tropical convection over a domain comparable to a GCM gridbox (Khairoutdinov et al, 2009.) A sequential learning strategy is used where the Giga-LES domain is partitioned into a few subdomains, , and atmospheric time series obtained on each subdomain are used to train the Bayesian procedure incrementally. Convergence of the marginal posterior densities for all seven parameters is demonstrated for two different grid partitions, and sensitivity tests to other model parameters are also presented. A single column model simulation using the SMCM parameterization with the Giga-LES inferred parameters reproduces many important statistical features of the Giga-LES run, without any further tuning. In particular it exhibits intermittent dynamical behavior in both the stochastic cloud fractions and the large scale dynamics, with periods of dry phases followed by a coherent sequence of congestus, deep, and stratiform convection, varying on timescales of a few hours consistent with the Giga-LES time series. The chaotic variations of the cloud area fractions were captured fairly well both qualitatively and quantitatively demonstrating the stochastic nature of convection in the Giga-LES simulation.


Khairoutdinov MF, Krueger SK, Moeng CH, Bogenschutz PA, Randall DA (2009): Large-eddy simulation of maritime deep tropical convection. Journal of Advances in Modeling Earth Systems 1(12)

Khouider B, Biello J, Majda AJ (2010) A stochastic multicloud model for tropical convection. Communications in Mathematical Sciences 8(1):187-216

- Indicates paper has been withdrawn from meeting
- Submission entered in competition