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Microphysical properties of tropical anvil cirrus observed during ACTIVE: A statistical analysis

机译:在活动期间观察到热带砧座卷曲的微观物理特性:统计分析

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The effect of cirrus cloud on radiative transfer depends on its microphysical properties. The water content and number concentrations of ice particles in tropical anvil cirrus measured during the ACTIVE (Aerosol and Chemical Transport in Tropical Convection) field campaign (from November 2005 to February 2006 in Darwin area, Australia) are analyzed. Some advanced particle probes are utilized during this campaign, including Cloud Imaging Probe (CIP) and Cloud Particle Imager (CPI). A statistical analysis of the fifteen cases (only the slow phase of anvil cirrus with the height ranging from 9.7 to 14.9 km and temperature ranging from -70.4 deg C to -30.0 deg C, are considered) shows that the typical value of ice water content (IWC) is 10~(-2) g m~(-3), and the number concentrations of ice particles measured by CIP (>100(mu)m) and CPI (>5(mu)m), are 10~(1) and 10~(2) L~(-1), respectively. The changes in median of IWC in anvil cirri with temperature (or altitude) are examined and compared among different phases of Australian monsoon.
机译:卷云云对辐射转移的影响取决于其微神科性质。分析了在活跃(热带对流中的气溶胶和化学传输)田间运动(2005年11月至2006年11月,澳大利亚达尔文地区2006年11月)中测量的热带砧座中冰颗粒的水含量和数量浓度。在此活动期间使用一些先进的粒子探针,包括云成像探针(CIP)和云粒子成像器(CPI)。十五个病例的统计分析(只有高度为9.7至14.9公里的高度为-70.4℃至-30.0°C至-30.0°C的高度的砧座卷曲的慢阶段)表明冰水含量的典型值(IWC)是10〜( - 2)gm〜(-3),通过CIP(> 100(mU)m)和CPI(> 5(mu)m)测量的冰颗粒的数量浓度为10〜( 1)和10〜(2)L〜(-1)分别。在澳大利亚季风的不同阶段进行了检查,并比较了IWC中IWC中位数的变化,并比较了澳大利亚季风的不同阶段。

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