Development of ensemble neural network convection parameterizations for climate models using ARM data

 

Authors

Yefim Kogan — University of Oklahoma - CIMMS
Philip Rasch — Pacific Northwest National Laboratory
Michael Fox-Rabinovitz — University of Maryland
Alexei Belochitski — University of Maryland
Vladimir Krasnopolsky — National Oceanic and Atmospheric Administration

Category

Modeling

Description

The neural network (NN) approach is formulated and used for development of a NN ensemble stochastic convection parameterization for climate models. This fast parameterization is built based on data from Cloud Resolving Model (CRM) simulations initialized with and forced by TOGA-COARE data. The SAM (System for Atmospheric Modeling), developed by D. Randall, M. Khairoutdinov, and their collaborators, has been used for CRM simulations. The observational data are also used for validation of model simulations. CRM-simulated data have been averaged and projected onto the GCM space of atmospheric states to implicitly define a stochastic convection parameterization. This parameterization is emulated using an ensemble of NNs. An ensemble of NNs with different NN parameters has been trained and tested. The inherent uncertainty of the stochastic convection parameterization derived in such a way is estimated. Due to these inherent uncertainties, the NN ensemble is used to constitute a stochastic NN convection parameterization. The major results and challenges of development of the stochastic NN convection parameterizations are discussed. The developed NN convection parameterization has been tested in a diagnostic CAM (CAM-NN) run versus the control CAM run. The obtained results are encouraging: total precipitation (P) and cloudiness (CLD) time series, diurnal cycles, and distributions for the tropical Pacific Ocean for the parallel CAM-NN and CAM runs show similarity and consistency. The P and CLD distributions for the tropical area for the parallel runs have been analyzed first for the TOGA-COARE boreal winter season (November 1992–February 1993) and then for the winter seasons of the follow-up parallel decadal simulations. A NN bias correction procedure was introduced and resulted in a measurable improvement of the CAM-NN simulation. The next steps of the project will include development of the stochastic NN convection parameterizations using SAM-simulated data forced by: (a) the long-term ARM SGP (Southern Great Planes) data set for testing NN convection over land, and (b) CAM-simulated data for testing NN convection over the entire globe. These NN convection stochastic parameterizations will be then validated and analyzed using the parallel CAM-NN and the control CAM simulations. Acknowledgments: The investigators would like to thank Prof. Marat Khairoutdinov (SUNY) for providing SAM and consultations and Dr. Peter Blossey (UWA) for consultations on SAM.