研究海洋大陆地区风暴解决尺度上的热带对流特征

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Xingying Huang, Andrew Gettelman, Brian Medeiros, William C. Skamarock
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引用次数: 0

摘要

全球风暴解析模式(GSRMs)提供了一种了解跨尺度天气和气候事件的方法,以便更好地了解气候影响。在这项工作中,我们应用最近开发和验证的基于开源社区地球系统模式(CESM2)的CAM(社区大气模式)-MPAS(跨尺度预测模式)建模框架,以3千米的水平间距研究海上大陆地区风暴解析尺度的热带对流特征。我们以 2018 年冬季的两次全球数值实验为目标,与该地区的观测结果进行比较。我们重点研究了对流系统、降水统计和热带气旋行为的表征。我们发现,区域精细化实验显示了更准确的降水分布、昼夜周期,以及在强度和强度统计方面与观测结果更一致的热带气旋特征。我们期待这项工作的探索将进一步推动风暴解析模式在跨尺度降水预测中的发展和应用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Examining Tropical Convection Features at Storm-Resolving Scales Over the Maritime Continent Region

Global Storm Resolving Models (GSRMs) provide a way to understand weather and climate events across scales for better-informed climate impacts. In this work, we apply the recently developed and validated CAM (Community Atmosphere Model)—MPAS (Model for Prediction Across Scales) modeling framework, based on the open-source Community Earth System Model (CESM2), to examine the tropical convection features at the storm resolving scale over the Maritime Continent region at 3 km horizontal spacing. We target two global numerical experiments during the winter season of 2018 for comparison with observation in the region. We focus on the investigation of the representations of the convective systems, precipitation statistics, and tropical cyclone behaviors. We found that regional-refined experiments show more accurate precipitation distributions, diurnal cycles, and better agreement with observations for tropical cyclone features in terms of intensity and strength statistics. We expect the exploration of this work will further advance the development and use of the storm-resolving model in precipitation predictions across scales.

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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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