Direct Bayesian model reduction of smaller scale convective activity conditioned on large-scale dynamics

IF 1.7 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
R. Polzin, A. Müller, H. Rust, P. Névir, P. Koltai
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引用次数: 1

Abstract

Abstract. We pursue a simplified stochastic representation of smaller scale convective activity conditioned on large-scale dynamics in the atmosphere. For identifying a Bayesian model describing the relation of different scales we use a probabilistic approach by Gerber and Horenko (2017) called Direct Bayesian Model Reduction (DBMR). This is a Bayesian relation model between categorical processes (discrete states), formulated via the conditional probabilities. The convective available potential energy (CAPE) is applied as a large-scale flow variable combined with a subgrid smaller scale time series for the vertical velocity. We found a probabilistic relation of CAPE and vertical up- and downdraft for day and night. This strategy is part of a development process for parametrizations in models of atmospheric dynamics representing the effective influence of unresolved vertical motion on the large-scale flows. The direct probabilistic approach provides a basis for further research on smaller scale convective activity conditioned on other possible large-scale drivers.
大尺度动力学条件下小尺度对流活动的直接贝叶斯模型约简
摘要我们追求在大气大尺度动力学条件下的小尺度对流活动的简化随机表示。为了确定描述不同尺度关系的贝叶斯模型,我们使用了Gerber和Horenko(2017)的概率方法,称为直接贝叶斯模型约简(DBMR)。这是一个分类过程(离散状态)之间的贝叶斯关系模型,通过条件概率来表述。采用对流有效势能(CAPE)作为大尺度流动变量,结合子网格小尺度时间序列表示垂直速度。我们发现了CAPE与白天和夜间垂直上升和下降气流的概率关系。这一策略是大气动力学模式参数化发展过程的一部分,这些模式代表了未解决的垂直运动对大尺度流动的有效影响。直接概率方法为进一步研究其他可能的大尺度驱动条件下的小尺度对流活动提供了基础。
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来源期刊
Nonlinear Processes in Geophysics
Nonlinear Processes in Geophysics 地学-地球化学与地球物理
CiteScore
4.00
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: Nonlinear Processes in Geophysics (NPG) is an international, inter-/trans-disciplinary, non-profit journal devoted to breaking the deadlocks often faced by standard approaches in Earth and space sciences. It therefore solicits disruptive and innovative concepts and methodologies, as well as original applications of these to address the ubiquitous complexity in geoscience systems, and in interacting social and biological systems. Such systems are nonlinear, with responses strongly non-proportional to perturbations, and show an associated extreme variability across scales.
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