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

机译:活动期间观察到的热带铁砧卷云的微物理性质: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).rnA 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℃ to -30.0℃, are considered) shows that the typical value of ice water contentrn(IWC) is 10~(-2) g m~(-3), and the number concentrations of ice particles measured by CIP (>100μm) and CPI (>5μm), 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:卷云对辐射传递的影响取决于其微物理性质。分析了在活动(热带对流中的气溶胶和化学物质运输)野外活动(2005年11月至2006年2月,澳大利亚达尔文地区)期间测得的热带砧卷云中的水含量和冰粒中的数量浓度。此活动中使用了一些先进的粒子探测器,包括“云成像探测器”(CIP)和“云粒子成像器”(CPI)。rn对15例病例的统计分析(仅是高度为9.7至14.9 km的砧卷的慢速阶段,在-70.4℃至-30.0℃的温度范围内)显示冰水含量的典型值(IWC)为10〜(-2)gm〜(-3),并用CIP法测定了冰粒的浓度。 (>100μm)和CPI(>5μm)分别为10〜1和10〜2 L〜(-1)。在澳大利亚季风的不同阶段之间,研究并比较了砧木中IWC中值的中位数随温度(或高度)的变化。

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