-AO. It fundamentally increases the chances that cold air masses can (frequently) move from the high latitude source regions and migrate into the midlatitudes. That is how it increases snow chances- we need the cold. A -EPO can also bring cold, but can also tend to be on the dry side and absent a -AO/NAO, the pattern is more progressive with lots of variability in storm tracks. We have to then consider the other indices, such as ENSO state and PNA phase, along with climo, to determine how much our snow chances are increased.