Improving supercooled liquid water representation in the microphysical scheme ICE3

IF 3 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Rémi Dupont, Claire Taymans, Benoît Vié
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引用次数: 0

Abstract

Most numerical weather prediction (NWP) models have a significant bias in predicting supercooled liquid water (SLW). For this reason, icing risk diagnostic tools do not use supercooled liquid water forecast by the models as an input parameter, but rather temperature and humidity, which are forecast better than SLW. The main objective of this study is to improve the SLW representation in the microphysical scheme ICE3 (Three Ice categories) used in the operational Applications de la Recherche à l'Opérationnel à Méso‐Echelle (AROME) model. For this purpose, several parametrizations of the microphysical processes were evaluated to find a better representation of SLW in the Mesoscale Non‐Hydrostatic model (MESO‐NH), which also uses ICE3. Elements of the microphysical scheme of the HARMONIE‐AROME model and work carried out by the Centre National de Recherches Météorologiques (CNRM) have been tested and compared with the current scheme. After a preliminary study, three parametrizations of the microphysical scheme were selected, in which the processes of ice initiation, snow and graupel collection of cloud droplets, condensation, Bergeron–Findeisen, and saturation adjustment were modified. Then, MESO‐NH simulations were performed and compared with observations from the In‐Cloud ICing and Large‐drop Experiment (ICICLE) airborne campaign. Three case studies were used with different icing weather conditions such as freezing rain, freezing drizzle, lake effect, etc. The results show a better representation of SLW with a greater presence of cloud droplets for colder temperatures up to 30 C. However, the liquid water content remains underestimated and the ice mass is overestimated. The ice initiation and cloud droplet collection by snow and graupel play a major role in the SLW representation. Parametrizations with restrictive ice initiation criteria reduce cloud droplet consumption and provide better agreement with observations. The results are promising and need to be investigated further with more cases and in the operational model AROME.
改进微观物理方案 ICE3 中的过冷液态水表示法
大多数数值天气预报(NWP)模式在预测过冷液态水(SLW)时存在明显偏差。因此,结冰风险诊断工具不使用模型预测的过冷液态水作为输入参数,而是使用温度和湿度作为输入参数,而温度和湿度的预测效果要好于过冷液态水。本研究的主要目的是改进运行中的 "AROME"(Applications de la Recherche à l'Opérationnel à Méso-Echelle)模式所使用的微物理方案 ICE3(三冰类别)中的过冷液态水表示。为此,对微观物理过程的几种参数化进行了评估,以便在同样使用 ICE3 的中尺度非静水模型(MESO-NH)中更好地表示 SLW。对 HARMONIE-AROME 模式的微观物理方案和国家气象研究中心(CNRM)的工作进行了测试,并与当前方案进行了比较。经过初步研究,选择了微物理方案的三个参数,其中对冰的形成过程、云滴的雪和岩浆收集过程、凝结过程、Bergeron-Findeisen 过程和饱和度调整过程进行了修改。然后,进行了 MESO-NH 模拟,并与云内结冰和大滴实验(ICICLE)机载活动的观测结果进行了比较。三个案例研究使用了不同的结冰天气条件,如冻雨、冻细雨、湖泊效应等。结果表明,在温度高达 30 C 的低温条件下,SLW 的代表性更好,云滴的存在更多。冰的形成以及雪和冰砾的云滴收集在 SLW 表征中起着重要作用。采用限制性起冰标准进行参数化可以减少云滴消耗,并与观测结果更加吻合。这些结果很有希望,需要在更多的案例和 AROME 运行模式中进一步研究。
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来源期刊
CiteScore
16.80
自引率
4.50%
发文量
163
审稿时长
3-8 weeks
期刊介绍: The Quarterly Journal of the Royal Meteorological Society is a journal published by the Royal Meteorological Society. It aims to communicate and document new research in the atmospheric sciences and related fields. The journal is considered one of the leading publications in meteorology worldwide. It accepts articles, comprehensive review articles, and comments on published papers. It is published eight times a year, with additional special issues. The Quarterly Journal has a wide readership of scientists in the atmospheric and related fields. It is indexed and abstracted in various databases, including Advanced Polymers Abstracts, Agricultural Engineering Abstracts, CAB Abstracts, CABDirect, COMPENDEX, CSA Civil Engineering Abstracts, Earthquake Engineering Abstracts, Engineered Materials Abstracts, Science Citation Index, SCOPUS, Web of Science, and more.
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