An ML-Based P3-Like Multimodal Two-Moment Ice Microphysics in the ICON Model

IF 4.4 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Axel Seifert, Christoph Siewert
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引用次数: 0

Abstract

Machine learning (ML) is used to build a bulk microphysical parameterization including ice processes. Simulations of the Lagrangian super-particle model McSnow are used as training data. The ML performs a coarse-graining of the particle-resolved microphysics to multi-category two-moment bulk equations. Besides mass and number, prognostic particle properties (P3) like melt water, rime mass, and rime volume are predicted by the ML-based bulk model. The ML-based scheme is tested with simulations of increasing complexity. As a box model, the ML-based bulk scheme can reproduce the simulations of McSnow quite accurately. In 3d idealized squall line simulations, the ML-based P3-like scheme provides a more realistic extended stratiform region when compared to the standard two-moment bulk scheme in ICON. In a realistic case study, the ML-based scheme runs stably, but can not significantly improve the results. This shows that ML can be used to coarse-grain super-particle simulations to a bulk scheme of arbitrary complexity.

Abstract Image

ICON 模型中基于 ML 的类似 P3 的多模态双瞬冰微物理学
机器学习(ML)用于建立包括冰过程在内的体微观物理参数化。拉格朗日超粒子模型 McSnow 的模拟结果被用作训练数据。ML 对粒子分辨微观物理进行粗粒化处理,并将其转换为多类两时刻体方程。除质量和数量外,基于 ML 的体积模型还能预测颗粒的预报属性 (P3),如熔融水、熔屑质量和熔屑体积。基于 ML 的方案通过复杂程度不断增加的模拟进行了测试。作为一个箱体模型,基于 ML 的体模型方案可以相当准确地再现 McSnow 的模拟结果。在 3d 理想化斜线模拟中,与 ICON 中的标准两时刻体型方案相比,基于 ML 的类 P3 方案提供了更真实的扩展层状区域。在实际案例研究中,基于 ML 的方案运行稳定,但不能显著改善结果。这表明 ML 可用来将超粒子模拟粗粒度化为任意复杂度的体方案。
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来源期刊
Journal of Advances in Modeling Earth Systems
Journal of Advances in Modeling Earth Systems METEOROLOGY & ATMOSPHERIC SCIENCES-
CiteScore
11.40
自引率
11.80%
发文量
241
审稿时长
>12 weeks
期刊介绍: The Journal of Advances in Modeling Earth Systems (JAMES) is committed to advancing the science of Earth systems modeling by offering high-quality scientific research through online availability and open access licensing. JAMES invites authors and readers from the international Earth systems modeling community. Open access. Articles are available free of charge for everyone with Internet access to view and download. Formal peer review. Supplemental material, such as code samples, images, and visualizations, is published at no additional charge. No additional charge for color figures. Modest page charges to cover production costs. Articles published in high-quality full text PDF, HTML, and XML. Internal and external reference linking, DOI registration, and forward linking via CrossRef.
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