Traditionally I have focused more on teleconnections for cold; and I am pretty ignorant about storm dynamics. I know that Miller A/B are ideal models and most noreasters are hybrids. Is it correct to say that the recent storm was pretty firmly in the Miller B category: a LP coming from the midwest transferring to a coastal low?
I understand the general idea of the dry slot coming from the gap between the winding down of the primary and the winding up of the secondary. Is a dry slot an absolute in these types of storms? Are there conditions which lead to smaller or larger dry slots? What factors determine the location of the slot? If the coastal low had formed closer to the coast would the dry slot have been more towards the west, or would it have merged with the precip from the primary low leading to a smaller dry slot (or no dry slot)?
I appreciate anyone who feels like taking time to share some knowledge.