The Impact of a Stochastically Perturbing Microphysics Scheme on an Idealized Supercell Storm

Author:

Qiao Xiaoshi1,Wang Shizhang2,Min Jinzhong2

Affiliation:

1. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, and Key Laboratory of Transportation Meteorology, China Meteorological Administration, Nanjing, and Shenyang Central Meteorological Observatory, Shenyang, China

2. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Meteorological Disaster of Ministry of Education, Nanjing University of Information Science and Technology, and Jiangsu Research Institute of Meteorological Science, Nanjing, China

Abstract

Abstract The concept of stochastic parameterization provides an opportunity to represent spatiotemporal errors caused by microphysics schemes that play important roles in supercell simulations. In this study, two stochastic methods, the stochastically perturbed temperature tendency from microphysics (SPTTM) method and the stochastically perturbed intercept parameters of microphysics (SPIPM) method, are implemented within the Lin scheme, which is based on the Advanced Regional Prediction System (ARPS) model, and are tested using an idealized supercell case. The SPTTM and SPIPM methods perturb the temperature tendency and the intercept parameters (IPs), respectively. Both methods use recursive filters to generate horizontally smooth perturbations and adopt the barotropic structure for the perturbation r, which is multiplied by tendencies or parameters from this parameterization. A double-moment microphysics scheme is used for the truth run. Compared to the multiparameter method, which uses randomly perturbed prescribed parameters, stochastic methods often produce larger ensemble spreads and better forecast the intensity of updraft helicity (UH). The SPTTM method better predicts the intensity by intensifying the midlevel heating with its positive perturbation r, whereas it performs worse in the presence of negative perturbation. In contrast, the SPIPM method can increase the intensity of UH by either positive or negative perturbation, which increases the likelihood for members to predict strong UH.

Funder

the Foundation of Beiji Ge

National Natural Science Foundation of China

the National Natural Science Foundation of China

the Major State Basic Research Development Program of China

The Startup Foundation for Introducing Talent of NUIST

a Project Funded by the Priority Academic Program Development (PAPD) of Jiangsu Higher Education Institutions

Publisher

American Meteorological Society

Subject

Atmospheric Science

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