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Dynamic Ensemble Analysis of Frontal Placement Impacts in the Presence of Elevated Thunderstorms during PRECIP Events

机译:PRECIP活动期间在高雷暴天气下正面位置影响的动态整体分析

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The Program for Research on Elevated Convection with Intense Precipitation (PRECIP) field campaign sampled 10 cases of elevated convection during 2014 and 2015. These intense observing periods (IOP) mostly featured well-defined stationary or warm frontal zones, over whose inversion elevated convection would form. However, not all frontal zones translated as expected, with some poleward motions being arrested and even returning equatorward. Prior analyses of the observed data highlighted the downdrafts in these events, especially diagnostics for their behavior: the downdraft convective available potential energy (DCAPE) and the downdraft convective inhibition (DCIN). With the current study, the DCAPE and DCIN are examined for four cases: two where frontal motion proceeded poleward, as expected, and two where the frontal motions were slowed significantly or stalled altogether. Using the Weather Research and Forecasting (WRF) model, a multi-model ensemble was created for each of the four cases, and the best performing members were selected for additional deterministic examination. Analyses of frontal motions and surface cold pools are explored in the context of DCAPE and DCIN. These analyses further establish the DCAPE and DCIN, not only as a means to classify elevated convection, but also to aid in explaining frontal motions in the presence of elevated convection.
机译:高降水对流研究计划(PRECIP)野外运动在2014年和2015年期间对10例高对流进行了采样。这些强观测期(IOP)主要表现为界限分明的静止或暖锋区,在这些区域上,对流会导致高对流形成。但是,并非所有的额叶区域都能按预期的方向平移,一些极向运动被阻止,甚至返回赤道。先前对观测数据的分析强调了这些事件中的下降气流,特别是其行为的诊断:下降气流对流可用势能(DCAPE)和下降气流对流抑制(DCIN)。在当前的研究中,检查了DCAPE和DCIN的四种情况:两种情况下,额叶运动如预期的那样极向进行,另外两种情况下,额叶运动明显减慢或完全停止。使用天气研究和预报(WRF)模型,为这四个案例中的每一个创建了一个多模型集合,并选择了表现最佳的成员进行其他确定性检查。在DCAPE和DCIN的背景下探索了对锋面运动和地表冷池的分析。这些分析进一步建立了DCAPE和DCIN,不仅作为对流对流的一种手段,而且还有助于解释对流存在时的额叶运动。

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