Elsewhere, an occluded front will slowly drift southwards from southern Scotland into Northern Ireland, northern England and East Anglia. The front is expected to become increasingly convective in nature, aided by low-level convergence and some diurnal heating. While CAPE is rather meagre, the environment is well-sheared which may be enough to compensate for an isolated lightning strike. That said, profiles remain capped at around 700mb, therefore limiting convective depth. Nonetheless, there could be a few funnel clouds associated with this convection.