Re: effect on Beaufort, I don’t think it was heat under the ice, looking at the pack the sudden disintegration of floes happens at the periphery where waves can reach the pack.
I posted a forecast of the storm six days before, because the isobars, despite its compact size and because of being surrounded by walls of high SLP, were impressing. And it travelled open ocean hundreds of miles before reaching the Beaufort, to lift those 4 m waves.
Below the forecast I cropped and posted Jul 28 and the analysis on August 3rd, which shows slightly weaker storm in appearance. What feeds a low like this to not dissolve in the middle of this high pressure background?