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On the Initiation of the 20 June 2015 Great Plains Low-Level Jet

机译:关于2015年6月20日的启动大平原低级喷气机

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Extensive measurements were made of the summertime Great Plains low-level jet (LLJ) in central Kansas during June and July 2015 as a component of the Plains Elevated Convection at Night (PECAN) field study. Here, the authors describe the early phase of the LLJ development on 20 June 2015. Half-hourly soundings were launched to monitor the progress of the jet. An airborne mission was also conducted using the University of Wyoming King Air research aircraft. Vertical sawtooth patterns were flown along a fixed track at 38.7 degrees N between longitudes 98.9 degrees and 100.3 degrees W to document changes in the potential temperature and wind profiles. Ageostrophic winds during the LLJ formation were also assessed. In addition, a high-resolution numerical simulation of the 20 June 2015 LLJ case was conducted using the Weather Research and Forecasting Model. Observations and model results show that the early stage of development consisted of a rapid increase in wind speed in the hours just after sunset with less pronounced directional change. The LLJ evolution is similar to that expected from an inertial oscillation of the ageostrophic wind following the stabilization of the near-surface layer.
机译:2015年6月和7月,作为平原夜间对流(PECAN)现场研究的一部分,对堪萨斯州中部的夏季大平原低空急流(LLJ)进行了广泛测量。在此,作者描述了2015年6月20日LLJ开发的早期阶段。每半小时进行一次探测,以监测飞机的进展情况。一个空中任务也使用怀俄明大学国王航空研究飞机进行。垂直锯齿模式沿着固定轨道在北纬38.7度、经度98.9度和西经100.3度之间飞行,以记录潜在温度和风廓线的变化。还评估了LLJ形成期间的非地转风。此外,利用天气研究和预测模型对2015年6月20日的LLJ案例进行了高分辨率数值模拟。观测和模型结果表明,发展的早期阶段包括日落后几小时内风速迅速增加,方向变化不太明显。LLJ的演变类似于近地表层稳定后非地转风的惯性振荡。

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