Yesterday, while I was analyzing data for snow chances in England next week, I spent extra time doing an in-depth analysis by incorporating BUFKIT's lake-effect snow algorithms. In order to do the analysis, I had to look up sea surface temperatures in the North Sea between Norway and England, which are in the +4 to +8C range. Once I had that information, I ran through the BUFKIT forecast soundings to see what the "lake-induced" CAPEs are forecast to be, and I found values up to nearly 500 J/Kg by 9 p.m. Tuesday. The main uncertainty at this point is where the strongest and most persistent snow bands set up, which will lead to higher than typical snow accumulations across England.
On Friday, March 16, 2018, I provided an updated forecast to a client stating that on Tuesday, March 20, there was a threat for 3" or more snow in northern parts of their area of concern, a threat for minor to moderate icing (thin glaze to as much as 0.10-0.20" possible) due to freezing rain in northwestern parts of their area, and a threat for 1" or more rainfall in southeastern parts of their area. All three of these concerns ended up happening in the areas I highlighted. At the time, looking five days out, there remained considerable uncertainty about which precipitation type would be most dominant. In addition, factor in the late March timing, meaning lighter snow rates would be slower to accumulate (if at all). The heavier snow rates, 1-2"/hr, would be sufficient. However the occurrence of such rates would be within localized bands, which are difficult to pinpoint where they would set up even 24 hours ahead of time, but nearly impossible five days ahead. From...

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