A Sub-Grid Precipitation Generator Based on NICAM for Simulating Cloud Radar Signals With GCMs

IF 3.4 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Tempei Hashino, Masaki Satoh, Takuji Kubota, Tsuyoshi Koshiro, Kozo Okamoto, Yuichiro Hagihara, Hajime Okamoto, Tatsuya Seiki
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引用次数: 0

Abstract

The forward simulation of radar reflectivity requires details of clouds and precipitation from general circulation models (GCMs). But such details are represented as sub-grid processes that involve parameterizations and assumptions about the spatial coverage and thus depend on the GCM. In this research, we propose the use of a statistical method to generate sub-grid precipitation for generic use. The sub-grid variability is obtained from simulation with a global storm-resolving model called NICAM (non-hydrostatic icosahedral atmospheric model). The proposed method first generates sub-grid precipitation masks based on probabilistic scenarios and then sub-grid precipitation rates are generated from the generalized gamma distribution for the given cloud fraction and grid-scale precipitation rates. Compared to the standard method (which neglects the probabilities) that overestimates the precipitation fraction, our method well reproduces the NICAM data set profiles of both the precipitation fraction and the radar-based cloud fraction. The in-cloud signal frequencies are also reproduced, although less accurately over a tropical region. Inclusion of sub-grid variability in precipitation rates was particularly important for the tropical region to obtain agreement of the precipitation fraction. Application of the two methods to a GCM shows it to have a robust bias for low-level liquid clouds. Furthermore, the sub-grid variability of precipitation led to more occurrences of the small signals, particularly for a range of high precipitation rates. The proposed method was designed to produce geographically dependent sub-grid variability in precipitation, indicating an effective way to use a global storm-resolving model to evaluate conventional GCMs.

Abstract Image

基于NICAM的亚网格降水发生器用于gcm模拟云雷达信号
雷达反射率的正演模拟需要来自一般环流模式(GCMs)的云和降水细节。但是,这些细节被表示为涉及参数化和空间覆盖假设的子网格过程,因此依赖于GCM。在这项研究中,我们建议使用统计方法来生成一般用途的子网格降水。亚网格变率是用全球风暴分辨模式NICAM(非流体静力二十面体大气模式)模拟得到的。该方法首先基于概率情景生成子网格降水掩模,然后根据给定云分数和网格尺度降水率的广义伽玛分布生成子网格降水率。与高估降水分量的标准方法(忽略概率)相比,我们的方法很好地再现了降水分量和基于雷达的云分量的NICAM数据集剖面。云内信号频率也可以重现,尽管在热带地区不太准确。在降水率中包含亚网格变率对于热带地区获得降水比例的一致性尤为重要。两种方法在GCM上的应用表明,GCM对低层液体云有较强的偏置。此外,降水的亚格变率导致了小信号的更多出现,特别是在高降水率范围内。该方法旨在产生地理相关的降水亚网格变率,表明使用全球风暴分辨模式评估常规gcm的有效方法。
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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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