Nicholls Stephen D, Decker Steven G, Tao Wei-Kuo, Lang Stephen E, Shi Jainn J, Mohr Karen I
NASA-Goddard Space Flight Center, Greenbelt, 20716, United States of America.
Joint Center for Earth Systems Technology, University of Maryland, Baltimore, 21250, United States of America.
Geosci Model Dev. 2017;10(2):1033-1049. doi: 10.5194/gmd-10-1033-2017. Epub 2017 Mar 3.
This study evaluated the impact of five, single- or double- moment bulk microphysics schemes (BMPSs) on Weather Research and Forecasting model (WRF) simulations of seven, intense winter time cyclones impacting the Mid-Atlantic United States. Five-day long WRF simulations were initialized roughly 24 hours prior to the onset of coastal cyclogenesis off the North Carolina coastline. In all, 35 model simulations (5 BMPSs and seven cases) were run and their associated microphysics-related storm properties (hydrometer mixing ratios, precipitation, and radar reflectivity) were evaluated against model analysis and available gridded radar and ground-based precipitation products. Inter-BMPS comparisons of column-integrated mixing ratios and mixing ratio profiles reveal little variability in non-frozen hydrometeor species due to their shared programming heritage, yet their assumptions concerning snow and graupel intercepts, ice supersaturation, snow and graupel density maps, and terminal velocities lead to considerable variability in both simulated frozen hydrometeor species and radar reflectivity. WRF-simulated precipitation fields exhibit minor spatio-temporal variability amongst BMPSs, yet their spatial extent is largely conserved. Compared to ground-based precipitation data, WRF-simulations demonstrate low-to-moderate (0.217-0.414) threat scores and a rainfall distribution shifted toward higher values. Finally, an analysis of WRF and gridded radar reflectivity data via contoured frequency with altitude (CFAD) diagrams reveals notable variability amongst BMPSs, where better performing schemes favored lower graupel mixing ratios and better underlying aggregation assumptions.
本研究评估了五种单矩或双矩体微物理方案(BMPS)对天气研究与预报模型(WRF)模拟的影响,该模拟针对影响美国中大西洋地区的七次强烈冬季气旋。在北卡罗来纳州海岸线外沿海气旋生成开始前约24小时,进行了为期五天的WRF模拟初始化。总共运行了35次模型模拟(5种BMPS和7个案例),并根据模型分析以及可用的网格化雷达和地面降水产品,对其与微物理相关的风暴属性(水汽混合比、降水量和雷达反射率)进行了评估。柱积分混合比和混合比廓线的BMPS间比较显示,由于非冻结水凝物种类具有共同的编程传统,其变化很小,但它们关于雪和霰的截留、冰过饱和度、雪和霰的密度图以及末速度的假设,导致模拟的冻结水凝物种类和雷达反射率存在相当大的变化。WRF模拟的降水场在BMPS之间表现出较小的时空变化,但其空间范围在很大程度上是守恒的。与地面降水数据相比,WRF模拟显示出低到中等(0.217 - 0.414)的威胁评分,且降雨分布向更高值偏移。最后,通过等高线频率与高度(CFAD)图对WRF和网格化雷达反射率数据进行分析,结果显示BMPS之间存在显著变化,其中表现较好的方案倾向于较低的霰混合比和更好的底层聚集假设。