Equus
Member
Most modeling has surface flow somewhat veered, and only veering further through the day as the front nears with the surface low weakening, so it feels like we will need backing from outflow boundaries or other surface features to get really robust low level mesocyclones in any supercells that try to form; SW/SSW surface winds support quick upscale growth but really elongate and straighten the hodographs to a degree that it feels like hail might be a threat even in mixed mode clusters