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Broadening of cloud droplet size distributions and warm rain initiation associated with turbulence: an overview 被引量:7
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作者 LU Chun-Song LIU Yan-Gang +1 位作者 NIU Sheng-Jie XUE Yu-Qi 《Atmospheric and Oceanic Science Letters》 CSCD 2018年第2期123-135,共13页
In the study of warm clouds,there are many outstanding questions.Cloud droplet size distributions are much wider,and warm rain is initiated in a shorter time and with a shallower cloud depth than theoretical expectati... In the study of warm clouds,there are many outstanding questions.Cloud droplet size distributions are much wider,and warm rain is initiated in a shorter time and with a shallower cloud depth than theoretical expectations.This review summarizes the studies related to the effects of turbulent fluctuations and turbulent entrainment-mixing on the broadening of droplet size distributions and warm rain initiation,including observational,laboratorial,numerical,and theoretical achievements.Particular attention is paid to studies by Chinese scientists since the 1950s,since most results have been published in Chinese.The review reveals that high-resolution observations and simulations,and laboratory experiments,are needed because knowledge of the detailed physical processes involved in the effects of turbulence and entrainment-mixing on cloud microphysics still remains elusive.The effects of turbulent fluctuations and entrainment-mixing processes have been unrealistically separated in most theoretical studies.They could be unified by further advancement of a systems theory into a predictive theory.Developing parameterizations for the effects of fluctuations and entrainment-mixing processes is still in its infancy,and more studies are warranted. 展开更多
关键词 Cloud droplet sizedistribution warm rain turbulent fluctuation entrainment-mixing systemstheory
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利用线阵估计湍流边界层起伏压力模型参数 被引量:3
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作者 葛辉良 暴雪梅 +2 位作者 王忠康 何祚镛 王育生 《哈尔滨工程大学学报》 EI CAS CSCD 2003年第6期600-603,共4页
湍流边界层起伏压力模型是预报水听器阵流噪声及流激水下结构振动和声辐射的基础,但湍流边界层起伏压力模型(如Corcos模型)都为经验模型,含有多个需要试验确定的待定参数,其中包括点功率谱密度与迁移速度.在此利用一条20元小阵元(6mm... 湍流边界层起伏压力模型是预报水听器阵流噪声及流激水下结构振动和声辐射的基础,但湍流边界层起伏压力模型(如Corcos模型)都为经验模型,含有多个需要试验确定的待定参数,其中包括点功率谱密度与迁移速度.在此利用一条20元小阵元(6mm)密排线阵在水洞中的测量数据估计湍流边界层起伏压力的波数频率谱,通过估计迁移峰谱密度级估计湍流边界层起伏压力的点功率谱密度级,利用高分辨率波数谱估计方法估计迁移波数并计算迁移速度.与利用单个水听器测量点功率谱密度及利用两个水听器相关时延测量迁移速度的方法相比,本文采用的方法在波数域分离了迁移峰和低波数的背景干扰,提高了置信度.数据分析结果表明,水洞中湍流边界层起伏压力的归一化迁移速度为0 75±0 05,点功率谱密度随流速的4~6次方增长. 展开更多
关键词 湍流边界层起伏压力 流噪声 迁移速度 点功率谱密度
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