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Cloud and rain liquid water statistics in the CHUVA campaign

机译:CHUVA活动中的云雨液态水统计

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The purpose of this study is to present statistics related to the integration of cloud and rain liquid water and the profiles for different cloud types and regimes. From 2010 to 2012, the CHUVA project collected information regarding cloud and rain characteristics in different precipitation regimes in Brazil. CHUVA had four field campaigns between 2010 and 2011, located in the North. Northeast and Southeast regions of Brazil, covering the semi-arid, Amazon, coastal and mountain regions. The synergy of several instruments allowed us to classify rain events and describe the cloud processes regionally. Microwave radiometers, LiDAR, radar, and disdrometers were employed in this study. The rain type classification was made using vertical profiles of reflectivity (VPR) and polarimetric variables from dual polarization radar (XPOL). The integrated liquid water (ILW_C) for non-precipitating clouds was retrieved with a microwave ground-based radiometer using a neural network. For rainy conditions, the profiles from the rain liquid water content (LWC_R) and their integrated (ILW_R) properties were estimated by Micro Rain Radar (MRR) and XPOL VPRs. For non-precipitating clouds, the ILW_C values were larger for the sites in tropical regions, in particular near the coast, than for Southeast Brazil. For rainy cases, distinct LWC_R profiles were observed for different rain classifications and regions. The differences are small for low rain rates and a distinction between different rainfall regimes is more evident for high rain rates. Vale and Belem clouds present the deepest layers and largest convective rain rates. The clouds in the Southeast region of Brazil (Vale do Paraiba) and North region (Belem) showed the largest reflectivity in the mixed and glaciated layers, respectively. In contrast, the Northeast coastal site (e.g. Fortaleza) showed larger values in the warm part of the clouds. Several analyses are presented, describing the cloud processes and the differences among the cloud types, rain rates and regions.
机译:这项研究的目的是提供与云和雨水水的整合有关的统计数据以及不同云类型和状态的概况。从2010年到2012年,CHUVA项目收集了有关巴西不同降水方式下的云和雨特征的信息。 CHUVA在2010年至2011年之间在北部进行了四次野战。巴西的东北和东南地区,涵盖半干旱,亚马逊,沿海和山区。几种仪器的协同作用使我们能够对降雨事件进行分类,并按地区描述云的过程。这项研究采用了微波辐射计,LiDAR,雷达和测距仪。使用垂直反射率(VPR)和双极化雷达(XPOL)的极化变量对降雨类型进行分类。使用神经网络,通过微波地面辐射计检索非降水云的综合液态水(ILW_C)。对于下雨条件,通过微雨雷达(MRR)和XPOL VPR估算了雨水含水量(LWC_R)及其综合(ILW_R)特性的轮廓。对于非降水云,热带地区(尤其是沿海地区)的站点的ILW_C值大于巴西东南部的站点。对于多雨的情况,对于不同的雨水分类和地区观察到了明显的LWC_R剖面。对于低降雨率而言,差异很小,而对于高降雨率而言,不同降雨制度之间的区别更加明显。淡水河谷和贝伦河云层最深,对流降雨率最大。巴西东南部地区(Vale do Paraiba)和北部地区(Belem)的云层分别在混合层和冰川层中显示出最大的反射率。相反,东北沿海站点(例如福塔莱萨)在云层温暖的部分显示出较大的值。提出了几种分析,描述了云的过程以及云类型,降雨率和区域之间的差异。

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