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Observations of ship tracks from ship-based platforms

机译:舰载平台上的航迹观察

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Ship-based measurements in June 1994 provided information about ship-track clouds and associated atmospheric environment observed from below cloud levels that provide a perspective different from satellite and aircraft measurements. Surface measurements of latent and sensible heat fluxes, sea surface temperatures, and meteorological profiles with free and tethered balloons provided necessary input conditions for models of ship- track formation and maintenance. Remote sensing measurements showed a coupling of ship plume dynamics and entrainment into overlaying clouds. Morphological and dynamic effects were observed on clouds unique to the ship tracks. These morphological changes included lower cloud bases early in the ship-track formation, eyidence of raised cloud bases in more mature tracks, sometimes higher cloud tops, thin cloud-free regions paralleling the tracks, and often stronger radar returns. The ship-based lidar aerosol measurements revealed that ship plumes often interacted with the overlying clouds in an intermittent rather than continuous manner. These observations imply that more must be learned about ship-track dynamics before simple relations between cloud condensation nuclei and cloud brightness can be developed.
机译:1994年6月基于船的测量提供了有关从海平面以下观测到的船迹云和相关大气环境的信息,从而提供了与卫星和飞机测量不同的视角。潜热通量和感热通量,海面温度以及带有自由和系留气球的气象剖面的表面测量为船形和维护模型提供了必要的输入条件。遥感测量表明,船羽动力和夹带进入了覆盖的云层。在船舶航迹特有的云层上观察到了形态学和动力效应。这些形态变化包括在舰船航迹形成初期较低的云层基数,更成熟的航迹中升高的云层基数的迹象,有时较高的云层顶部,与航迹平行的无云薄区域以及通常更强的雷达回波。基于舰船的激光雷达气溶胶测量结果显示,舰船羽流经常以断续而非连续的方式与上覆的云层相互作用。这些观察结果表明,在发展云凝结核与云亮度之间的简单关系之前,必须进一步了解船舶航迹动力学。

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