Lagrangian and Eulerian supersaturation statistics in turbulent cloudy Rayleigh–Bénard convection: applications for LES subgrid modeling

IF 3 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
K. K. Chandrakar, H. Morrison, R. Shaw
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引用次数: 0

Abstract

Turbulent fluctuations of scalar and velocity fields are critical for cloud microphysical processes, e.g., droplet activation and size distribution evolution, and can therefore influence cloud radiative forcing and precipitation formation. Lagrangian and Eulerian water vapor, temperature, and supersaturation statistics are investigated in direct-numerical simulations (DNS) of turbulent Rayleigh–Bénard convection in the Pi Convection Cloud Chamber to provide a foundation for parameterizing subgrid-scale fluctuations in atmospheric models. A subgrid model for water vapor and temperature variances and covariance and supersaturation variance is proposed, valid for both clear and cloudy conditions. Evaluation of phase change contributions through an a priori test using DNS data shows good performance of the model. Supersaturation is a nonlinear function of temperature and water vapor, and relative external fluxes of water vapor and heat (e.g., during entrainment-mixing and phase change) influence turbulent supersaturation fluctuations. Although supersaturation has autocorrelation and structure functions similar to the independent scalars (temperature and water vapor), the autocorrelation timescale of supersaturation differs. Relative scalar fluxes in DNS without cloud make supersaturation PDFs less skewed than the adiabatic case, where they are highly negatively skewed. However, droplet condensation changes the PDF shape response: it becomes positively skewed for the adiabatic case and negatively skewed when the sidewall relative fluxes are large. Condensation also increases correlations between water vapor and temperature in the presence of relative scalar fluxes but decreases correlations for the adiabatic case. These changes in correlation suppress supersaturation variability for the non-adiabatic cases and increase it for the adiabatic case. Implications of this work for subgrid microphysics modeling using a Lagrangian stochastic scheme are also discussed.
湍流多云Rayleigh–Bénard对流中的拉格朗日和欧拉过饱和统计:在LES子网格建模中的应用
标量场和速度场的湍流波动对云的微观物理过程(如液滴活化和尺寸分布演变)至关重要,因此可以影响云的辐射强迫和降水形成。在Pi对流云室中湍流Rayleigh–Bénard对流的直接数值模拟(DNS)中,研究了拉格朗日和欧拉水蒸气、温度和过饱和统计,为大气模型中亚网格尺度波动的参数化提供了基础。提出了一个水蒸气和温度方差以及协方差和过饱和方差的子网格模型,该模型对晴朗和多云条件都有效。通过使用DNS数据的先验测试来评估相变贡献显示了该模型的良好性能。过饱和度是温度和水蒸气的非线性函数,水蒸气和热量的相对外部通量(例如,在夹带混合和相变过程中)影响湍流过饱和度波动。尽管过饱和具有类似于独立标量(温度和水蒸气)的自相关和结构函数,但过饱和的自相关时间尺度不同。没有云的DNS中的相对标量通量使过饱和PDF比绝热情况下的偏态更小,绝热情况下它们是高度负偏态的。然而,液滴凝结改变了PDF形状响应:在绝热情况下,它变得正偏斜,而在侧壁相对通量较大时,它变得负偏斜。在存在相对标量通量的情况下,冷凝也增加了水蒸气和温度之间的相关性,但在绝热情况下降低了相关性。这些相关性的变化抑制了非绝热情况下的过饱和可变性,并增加了绝热情况下过饱和可变性。还讨论了这项工作对使用拉格朗日随机格式进行亚网格微物理建模的影响。
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来源期刊
Journal of the Atmospheric Sciences
Journal of the Atmospheric Sciences 地学-气象与大气科学
CiteScore
0.20
自引率
22.60%
发文量
196
审稿时长
3-6 weeks
期刊介绍: The Journal of the Atmospheric Sciences (JAS) publishes basic research related to the physics, dynamics, and chemistry of the atmosphere of Earth and other planets, with emphasis on the quantitative and deductive aspects of the subject. The links provide detailed information for readers, authors, reviewers, and those who wish to submit a manuscript for consideration.
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