One of the contributing factors to our up-and-down winter season has been the ongoing La Nina in the tropical region of the Pacific Ocean.
La Nina disrupts the jet stream pattern by causing a large region of persistent thunderstorms over the western tropical Pacific Ocean. It is one of many weather features that can influence the jet stream.
This winter's pattern has been particularly "blocky," meaning the jet stream has had a tendency to displace warm air very far northward in some places while sending Arctic air way south in other places, and then locking these anomalies in for days or weeks at a time.
The retreat of the cold, dry air for the moment opens up the possibilities of snowstorms coming our way from the southwestern U.S. It is also possible that Arctic air will return before the winter is over.