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KATABATIC FLOW AND TURBULENCE AS SEEN FROM AIRBORNE IN-SITU MEASUREMENTS AND GROUND-BASED PROFILER MEASUREMENTS DURING VTMX

机译:VTMX期间航空机内原位测量和基于地面的轮廓测量所显示的湍流和湍流

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These data suggest an oscillating drainage flow. The airplane sampled the event centered on 0600 MDT. The east flight leg passed first above the drainage flow, then through the turbulent entrainment layer at its top, and finally within the drainage itself, characterized by northeast wind. The west flight leg, farther into the valley shows only south winds, though there was drainage beneath, revealed in the now southeast flow reported by the tower, sodar, and radar. Having a longer record, these instruments reveal the oscillatory nature of the drainage. More surface and upper air data from the whole Salt Lake Valley will be needed to verify these hypotheses.
机译:这些数据表明排水流量振荡。飞机以0600 MDT为中心对事件进行了采样。东航支路首先经过排水流上方,然后经过其顶部的湍流夹带层,最后经过排水系统本身,以东北风为特征。塔底,声雷达和雷达报告的现在向东南方向的流向中显示,更深的山谷向西的飞行航迹仅显示南风,尽管下方有排水。这些仪器具有更长的记录,显示了排水的振荡特性。需要更多来自整个盐湖谷的地面和高空数据来验证这些假设。

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