Localized, steady to heavy snow bands affected portions of north-central Montana between the evening of February 15th and early morning of February 16th. As an eastward-moving shortwave trough traversed the region, a low pressure center aloft developed within this shortwave. The low's cyclonic circulation drew relatively-warm air northward and then around the backside of the low pressure center. This warm air encountered colder air, resulting in frontogenesis in the low- to mid-level atmosphere. The combination of lift induced by this frontogenesis and abundant low- to mid-level moisture contributed to the development of steady to heavy snow bands, generally north through west of the low pressure center aloft. The greatest snow totals were focused in Cascade County, where reports of about 6 to 12-inches of snow were received.