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reflectivity and vertical movement of the precipitation directly above and below the aircraft ( Wang et al. 2012 ). The Wyoming Cloud Lidar (WCL) also collected data that were analyzed with the University of Wyoming software. Analysis of in situ observations was conducted using MATLAB, version 9.0.0.341360 (number R2016a), and Microsoft, Inc., Excel (version 2016). All in situ and remote sensing observations were corrected for known errors by the University of Wyoming and the National Center for
reflectivity and vertical movement of the precipitation directly above and below the aircraft ( Wang et al. 2012 ). The Wyoming Cloud Lidar (WCL) also collected data that were analyzed with the University of Wyoming software. Analysis of in situ observations was conducted using MATLAB, version 9.0.0.341360 (number R2016a), and Microsoft, Inc., Excel (version 2016). All in situ and remote sensing observations were corrected for known errors by the University of Wyoming and the National Center for
these flashes were of negative polarity and ceased to occur once the storm moved over Lake Michigan even though the lake enhanced the precipitation. Warner et al. (2014) provide evidence that these flashes were mostly SIUL flashes associated with a variety of anthropogenic structures. The purpose of this paper is to characterize the mesoscale and microphysical aspects of lake-effect thundersnow events using the high-resolution OWLeS observations. Lightning was reported (by humans and/or automated
these flashes were of negative polarity and ceased to occur once the storm moved over Lake Michigan even though the lake enhanced the precipitation. Warner et al. (2014) provide evidence that these flashes were mostly SIUL flashes associated with a variety of anthropogenic structures. The purpose of this paper is to characterize the mesoscale and microphysical aspects of lake-effect thundersnow events using the high-resolution OWLeS observations. Lightning was reported (by humans and/or automated
