I read it as through now not moving forward...but to your point, yes moving forward that signal does dampen out quite a bit. And also to your point about the decreasing seasonal lag is we don't always need a massive ridge at H5 to get big heat into here. If we get a very strong sfc high across the Southeast or just off the Southeast Coast that can certainly pump in big heat (and humidity) all while maintaining a more northwesterly flow aloft(indicative of a subtle trough or downwind of a ridge crest)...and this is how we get our higher end severe events (ala summer 1995).