Here is the big picture: there are two current storm tracks across North America. The first, which is well to our north, is the storm track that would normally be across our region. So far this winter, it has been displaced to our north – one of the reasons we have been dry. The second storm track is well to the south across the southern U.S. This places us under a rather slack flow as we oscillate between pushes of warm and cool air with each passage of low-pressure to our north.
