Definite competing factors today. As noted above, the instability, deep layer shear, and low-level lapse rates are really good. On the downside, low-level westerly flow here (which occurs when the surface low is well to our northeast) tends to dry out the lower levels and limit convergence along the cold front. The threat is certainly better the further east and northeast one goes, but the overall trend in the CAMs for the local area is positive, especially with the HRRR seeming to come on board this morning.