Regardless of how close Ophelia gets and how tropical it is on closest approach or landfall, I am intrigued by the potential for some degree of 'subsidence warming' ahead of the system; tropical cyclones produce upper-level outflow channels of warm air, which then tend to slow down a little way ahead of the system's track (as the upper-level flow is often the steering flow too) and then subside toward the surface, with consequential warming which can then lead to increased surface temperatures compared to what would usually be taking place under a given setup of airflow and airmass temperatures.
This could give Monday's temperatures a little extra kick upward. What I don't know, helpfully enough, is whether this is already being incorporated into the models... 

Originally Posted by: Stormchaser