Collaborative Research: Investigations of Non-Classic Lake-Effect Boundary Layer Processes

在研究和业务天气观测系统和数值模拟技术的进步，导致逐步改善的物理过程中涉及的发展和演变的湖泊效应雪暴的理解。 特别是最近的观测期间，湖泊诱导对流实验（湖冰）和中尺度数值模型已被用来更好地了解孤立的“经典”湖效应系统，主要是从湖表面的热量和水分通量在秋季和冬季。 对经典湖泊效应系统中微尺度和中尺度过程之间相互作用的科学理解得到了加强，现在可以应用于更复杂，也许更常见和更强烈的，这个合作研究项目将建立在过去的研究成果，并使用新的观测和数值模式，以发展一个物理上一致的理解天气系统和中尺度湖泊的复杂相互作用，影响系统和因素控制的连贯性，结构沿着，中尺度湖效应对流带。 特别是，主要研究人员将分析从雷达、飞机、卫星和地面仪器获得的数据，并进行详细的中尺度模型模拟，以研究非经典湖泊效应情况下尚未解决的问题。 四个具体的研究目标是：1）确定在有和没有大尺度降水的情况下，云微物理结构和湖泊效应边界层热力学的差异; 2）确定暖湖对移动中尺度降水系统的中尺度动力学和结构的影响（如与天气锋有关的）; 3）确定对流边界层和来自逆风湖的中尺度环流影响顺风湖上湖效应发展的过程;（4）确定导致沿着湖效应雪带中尺度结构发展的动力机制以及垂直风切变对带结构相干性的影响。这项研究的成功完成可能有助于改善对强烈湖泊效应暴风雪的预测。

Advances in research and operational weather observation systems and numerical modeling techniques have led to progressive improvements in understanding of physical processes involved in the development and evolution of lake-effect snow storms. In particular recent observations taken during the Lake-Induced Convection Experiment (Lake-ICE) and mesoscale numerical models have been utilized to better understand isolated "classic" lake-effect systems that develop primarily from lake surface heat and moisture fluxes in fall and winter months. The enhanced scientific understanding of interactions between microscale and mesoscale processes in classic lake-effect systems can now be applied to more complex, and perhaps more common and intense, non-classic lake-effect storms.This collaborative research project will build on past research results and use new observations and numerical models to develop a physically-consistent understanding of complex interactions of synoptic systems and mesoscale lake-effect systems and factors controlling the coherence of, and structure along, mesoscale lake-effect convective bands. In particular the Principal Investigators will analyze data obtained from radars, aircraft, satellites and surface instrumentation and perform detailed mesoscale model simulations to study unresolved issues for non-classic lake-effect situations. Four specific research objectives are to: 1) Determine differences in the cloud microphysical structure and thermodynamics of lake-effect boundary layers that occur with and without large-scale precipitation aloft; 2) Determine the effects of a warm lake on the mesoscale dynamics and structure of moving mesoscale precipitation systems (such as associated with synoptic fronts); 3) Determine the processes by which the convective boundary layer and mesoscale circulations from an upwind lake influence lake-effect development over a downwind lake; 4) Determine the dynamic mechanisms leading to the development of mesoscale structures along lake-effect snow bands and the influence of vertical wind shear on band structural coherence. Successful completion of this research could help improve the forecast of intense lake-effect snowstorms.