A Connecticut winter typically delivers 30 to 50 freeze-thaw cycles between November and March. Each cycle does small damage to asphalt that has any water under the surface. Water in the base freezes, expanding ~9% in volume, and lifts the surface above. When it thaws, the base settles back unevenly. Over a winter, that cycle widens existing cracks, opens new ones, and accelerates wear at the edges.
The driveways that age fastest in CT winters are the ones with drainage problems. Water that ponds on the surface or saturates the base before each freeze is multiplied by every cycle of the season.