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WUGuoxiong WANGHuijun Da-LinZHANG 《大气科学进展》2004,21(3):382-382
On 16 March 2004, we received an appeal from Dr. Qing WANG of the United States‘ Naval Postgraduate School questioning the legitimacy of the paper entitled, Modeling Marine Stratocumulus with a Detailed Microphysical Scheme, that was published by ZHAO Chunsheng and Yutaka Ishizaka in the January 2004 issue of the Advances in Atmospheric Sciences (AAS). She pointed out that the model described in the paper was developed by her group in which the first author, Dr. Zhao, worked as a visiting scholar during February 1997-February 1998. 相似文献
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This study explores the microphysical responses to a cloud seeding operation in the Sanjiangyuan region, China. The cloud seeding was performed using a zigzag flight pattern, while the detection phase was accomplished using a back-and-forth flight pattern through the top of a stratocumulus layer. Global Position System（GPS） and Particle Measuring System（PMS） data obtained during the operation are used to determine the efective cloud area before and after the operation, diferentiate the phase states of cloud particles, and analyze changes in the concentrations of liquid cloud particles and ice crystals, the evolution of the cloud particle spectrum, and the content of supercooled water. The median diameter of liquid cloud particles in the area of the cloud-seeding operation was 3.5–18.5 μm, most cloud particles observed in the 21.5–45.5-μm size regime were ice crystals, while all particles of size 50 μm and above were in the ice phase. Changes in the concentration and typical diameter of cloud particles within 36 km downwind of the cloudseeding operation did not exceed natural fluctuations in the cloud area before the operation; however, the concentration of liquid cloud particles decreased substantially in areas with high concentrations of supercooled water（concentrations of supercooled water exceeding 0.01 g m 3）. The concentration of ice crystals within the measuring range of the Forward Scattering Spectrometer Probe（FSSP） increased substantially, the water content of ice-phase particles increased, and the average supercooled water content in the cloud decreased from（68.3± 23.1）% before the operation to（34.2± 12.4）%. The efects of cloud seeding were more pronounced in parts of the cloud where the content of supercooled water was higher. Little to no efects were observed in parts of the cloud with low concentrations of supercooled water. 相似文献
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利用CloudSat 卫星资料,选取冰粒子的等效半径（IER）、数浓度（INC）、含水量（IWC）,统计分析了层云、层积云微物理量的垂直分布和季节变化。层云/层积云小粒子（0～50 μm）、中等粒子（50～80 μm）、大粒子（≥80 μm）出现频率分别为18.7%/16.3%、77.6%/62.6%、3.7%/21.2%。在IER 垂直分布上,层云小、中等粒子在云层中部出现较多,层积云小粒子在云层上部出现较多,中等、大粒子在云层中部出现较多。层云/层积云INC低值段（0～50 L-1）、中值段（50～100 L-1）、高值段（≥100 L-1）出现频率分别为90.1%/76.5%、9.6%/19.5%、0.3%/4.1%。在INC垂直分布上,层云低、中值段在云层中部出现较多,层积云低、中值段分别在云层中部、上部出现较多。层云/层积云IWC低值段（0～50 mg·m-3）、中值段（50～100 mg·m-3）、高值段（≥100 mg·m-3）出现频率分别为96.7%/82.8%、3.2%/13.4%、0.1%/3.7%。在IWC垂直分布上,层云低值段在云层中部出现较多,层积云低、中值段分别在云层中部、上部出现较多。 相似文献
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1密卷云和透光层积云的基本特点1.1密卷云密卷云为高云簇,云高一般在6000m以上。云块分散孤立,排列无规则。云体由冰晶组成,中间厚四周薄,其边缘部分丝缕结构明显,遇日、月可以看不到完整的晕圈。因云底较高,日出日落前后云底呈淡黄色或微红色。偶有零星降雪。 相似文献
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基于2007—2010年的CloudSat卫星观测数据,以云层液态水路径为指标将层积云的发展过程划分为五个阶段,对比研究了中国东部降水与非降水层积云发展过程中云微物理特征和云微物理机制的演变,并分析了其海陆差异.研究表明:非降水层积云中,云滴增长主要通过凝结过程完成,但云滴的凝结增长有限,难以形成降水,在非降水层积云发展的旺盛阶段,云层中上部云滴发生较弱的碰并过程.降水层积云中云滴碰并增长活跃,当云层液态水路径小于500 g·m~(-2)时,云滴在从云顶下落至云底的过程中持续碰并,并在云底附近出现云水向雨水的转化;当降水层积云液态水路径超过500 g·m~(-2)时,云滴碰并增长主要发生在云层上部,在云层中部,云液态水含量、液态粒子数浓度和液态粒子有效半径达到最大,云水向雨水的转化最为活跃.层积云微物理特征的海陆差异主要是由海陆上空气溶胶浓度和云中上升气流强度不同导致的.在非降水层积云中下部,陆地丰富的气溶胶为云滴凝结增长提供了充足的云凝结核,因而云微物理量的量值在陆地上空更大,而在云层中上部,云滴凝结增长达到极限,海洋充足的水汽输送使云微物理量的量值在海洋上空更大.当降水层积云液态水路径大于500 g·m~(-2)时,陆地层积云中更强的上升气流使大量云滴在云层中上部累积滞留,云滴碰并增长活跃,云层中上部云微物理量的量值在陆地上空更大. 相似文献
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堡状层积云（高积云）与雷雨天气 总被引：1，自引：0，他引：1
堡状层积云（高积云）与雷雨天气韩东喜（滨州地区气象局．２５６６１２）堡状层积（高积）云（以下简称堡状云），是“个体呈条状的，垂直发展的积云形的云块，它们并列在一线上，有一共同的底边，顶部凸起明显，远处看去很像城堡”。堡状云是由于对流运动占主导地位，突... 相似文献
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利用Droplet Measureinent TeehnologY（DMT）资料,分析了山西2008年7月17日降水性层积云的云微物理结构,通过对云中粒子浓度、直径、二维图像以及谱型分布变化,并结合宏观记录特征,详细分析了飞机上升和下降阶段云系的垂直结构特征。结果表明：飞机上升阶段云系为高积云,飞机下降阶段云系为高积云一层积云结构,Cloud Droplet Probe（CDP）和Cloud Imaging Probe（CIP）测得粒子浓度偏大,最大浓度分别为236em。和9．74cm^-3。层积云云中微物理量水平分布特征具有明显的不均匀性。上升阶段降水的雨滴主要是冰粒子融化形成的,冷云过程占主导地位,在0℃层附近存在明显的融化层亮带。下降阶段降水机制为高积云冷云过程和层积云暖云过程相结合。 相似文献
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