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Combining In Situ and Satellite Observations to Understand the Vertical Structure of Tropical Anvil Cloud Microphysical Properties During the TC4 Experiment

机译:原位和卫星观察结合了解TC4实验期间热带砧云微神科性质的垂直结构

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Tropical anvil clouds have a profound impact on Earth's weather and climate. Their role in Earth's energy balance and hydrologic cycle is heavily modulated by the vertical structure of the microphysical properties for various hydrometeors in these clouds and their dependence on the ambient environmental conditions. Accurate representations of the variability and covariability of such vertical structures are key to both the satellite remote sensing of cloud and precipitation and numerical modeling of weather and climate, which remain a challenge. This study presents a new method to combine vertically resolved observations from CloudSat radar reflectivity and Cloud‐Aerosol Lidar and Infrared Pathfinder Satellite Observation cloud masks with probability distributions of cloud microphysical properties and the ambient atmospheric conditions from detailed in situ measurements on tropical anvils sampled during the National Aeronautics and Space Administration TC4 (Tropical Composition, Cloud and Climate Coupling) mission. We focus on the microphysical properties of the vertical distribution of ice water content, particle size distributions, and effective sizes for different hydrometeors, including ice particles and supercooled liquid droplets. Results from this method are compared with those from in situ data alone and various CloudSat/Cloud‐Aerosol Lidar and Infrared Pathfinder Satellite Observation cloud retrievals. The sampling limitation of the field experiment and algorithm limitations in the current retrievals is highlighted, especially for the liquid cloud particles, while a generally good agreement with ice cloud microphysical properties is seen from different methods. While the method presented in this study is applied to tropical anvil clouds observed during TC4, it can be readily employed to study a broad range of ice clouds sampled by various field campaigns.
机译:热带砧云对地球的天气和气候产生了深刻的影响。它们在地球的能量平衡和水文周期中的作用受这些云中各种水流器的微神科性质的垂直结构的严重调节,以及它们对环境环境条件的依赖性。准确表示这种垂直结构的可变性和可协助性的是卫星遥感云和降水和天气和气候的数值模拟的关键,这仍然是一个挑战。本研究提出了一种新的方法,将垂直解决的观测结合在Cloudsat雷达反射率和云气溶胶激光葡萄球菌和红外探测器卫星观察云面罩中,具有云微微物理特性和环境大气条件的概率分布,从详细地对热带砧座进行了采样的原位测量国家航空航天局TC4(热带成分,云和气候耦合)任务。我们专注于冰水含量,粒度分布和不同水流仪的有效尺寸的垂直分布的微神科性质,包括冰颗粒和过冷液滴。这种方法的结果与单独的原位数据和各种Cloudsat /云气溶胶激光雷达和红外探测器卫星观察云检索的结果进行比较。突出显示电流检索的现场实验和算法限制的采样限制,特别是对于液体云颗粒,而是从不同的方法看出与冰云微动物性质的一般良好的一致性。虽然本研究中呈现的方法应用于TC4期间观察到的热带砧云,但是可以容易地使用各种场地运动采样的广泛冰云。

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