I don't really buy that logic from snowgoose69 on american given that there's enough separation here between the two (nearly a full wavelength of the planetary-scale waves they're embedded in) that if the system on the 27th is in fact stronger, that'll act to amplify the 50-50 low just offshore of Newfoundland and Labrador and amplify the ridge downstream of our primary shortwave which will still be over the plains as this is occurring, slowing our storm down and giving it an opportunity to dig. If however, they were located within half a wavelength of one another and/or in the same ridge axes or trough base, it would be a different story. As we recently observed in February 2014, the weak overrunning event on the February 11 2014 apparently did little, if anything to slow the progress of our primary storm on the 12th-13th. While the overrunning event on the 27th was more impressive on this Euro run, the parent shortwave was generally weaker which actually may have contributed to a weaker, drier solution later on the 28th-29th
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