ehh I don't think it is as bad as what is being advertised...assuming you're referencing the UD Helicity swaths?
In this case, I think the UP helicity swaths (which we see 2-5km on the models) are heavily favored towards the higher portion of the llvls and lower portion of the mlvls. With that in mind the hodographs are largest when viewing the 0-3km layer as opposed to 0-1km layer given the shear in this level is pretty weak...IDK strong enough to yield TOR potential. Regardless, LCL's are very high and in fact keep rising.
Another thing (at least for most of CT) is we may not generate much in the way of sfc instability...it's all elevated. Of course we can get elevated supercells but that would probably yield a risk for some hail and strong wind gusts.
I'm not very impressed with the svr potential in CT outside of the shoreline.