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A new tethered balloon-borne payload for fine-scale observations in the cloudy boundary layer

机译:一种新的系留在气球上的系留有效载荷,用于在阴天边界层进行精细观测

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摘要

A new scientific payload is introduced for fine-scale measurements of meteorological (wind vector, static air temperature, humidity, and air pressure) and microphysical (aerosol particles and cloud droplets) properties, suspended below a tethered balloon. The high resolution sensors and the tethered balloon are described. Measurements in a lifted fog layer from a first field campaign are presented. The detailed investigation of the fog/haze and the temperature inversion layer demonstrates the damping influence of the fog on temperature fluctuations, while the wind fluctuations are significantly decreased by the evolving temperature inversion, which was about 30 m above the fog layer. From spectral analysis the noise floors of the high-resolution sensors are determined to 10~(-6) kg m~(-3) for the L WC (liquid water content) and 4 mK for the fast temperature sensor (UFT-B). The correlation between temperature and LWC structures in shallow haze layers is investigated. The release of latent heat andthe corresponding warming in the haze of about 0.1 K could be quantified.
机译:引入了一种新的科学有效载荷,用于对系留在气球下方的气象(风向,静态空气温度,湿度和气压)和微物理(气溶胶颗粒和云滴)特性进行精细测量。描述了高分辨率传感器和系留气球。展示了第一次野战中升起的雾层中的测量结果。对雾/霾和温度反演层的详细研究表明,雾对温度波动的阻尼影响,而随着温度反演的发展,风的波动显着减小,温度反演在雾层上方约30 m。通过频谱分析,将高分辨率传感器的本底噪声确定为L WC(液态水含量)为10〜(-6)kg m〜(-3),而快速温度传感器(UFT-B)的噪声本底确定为4 mK 。研究了浅雾层中温度与轻质水结构之间的相关性。潜热的释放以及在约0.1 K的雾度中相应的变暖可以被量化。

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