Start with how cold the pavement actually gets. Hector's normals count 41.7 nights a year at or below zero, most of them in December, January and February, and the normal January low is 0.1 degrees. On about 88 days a year the high never gets above freezing. Asphalt binder stiffens as it cools, and a mat that cannot stretch as it shrinks relieves the strain by cracking across its width. Those transverse cracks, running straight across a driveway or a parking aisle, are the signature defect of cold-climate pavement. Filled, they keep meltwater out of the base. Left open, they widen a little every spring.
Then there is how deep the cold reaches. The City of Fargo's deck handout gives the local frost line as 52 inches, and across the river Minnesota's building rule puts Clay County in its deeper frost zone, where footings go five feet down. HomeGuide recommends a compacted gravel base of 6 to 8 inches under a home driveway, a small fraction of that depth, so the whole base and a good deal of the soil under it freeze every winter. Where that soil holds water, ice lenses grow and lift the pavement unevenly. Sealer cannot fix heave; drainage and base work can.
The damage season is the thaw. At Hector the pavement crosses the freezing line about 84 days a year, and 31 of those crossings come in March and April. Frost leaves the ground from the top down, so for a few weeks meltwater sits on a still-frozen layer with nowhere to go and the base is at its softest. NDDOT puts it plainly for state highways: the most significant pavement damage happens in the first four weeks after spring thaw begins. The Red River crests in the same weeks. The ten highest crests on record at the Fargo gauge all fell between March 21 and April 18.
Water also has trouble leaving. The Red falls only about a foot per mile through the valley, and the city runs 81 storm sewer lift stations to help move storm water across terrain that flat. Under the lawns lies the Fargo series, a soil named after the city: a poorly drained silty clay with very low to low permeability and a seasonal water table that can reach the surface. A driveway on that ground cannot count on the subgrade to soak up a puddle. Its crown, its edges and where the downspouts empty decide whether meltwater runs off or sits against the asphalt until it refreezes.
The housing stock is young for a northern city. Fargo grew from 74,111 people in 1990 to 125,990 in 2020, the median housing unit was built in 1991, and 36.7 percent of units date from 2000 or later, according to ACS 2019-2023 estimates. New residential growth since the mid-1980s has gone south and southwest, so many drives there are on their first or second coat, while a large part of the north end had to be rebuilt after the 1957 tornado. Most households rent and only about a third of units are detached houses, which puts a large share of the city's asphalt in apartment and commercial parking lots.
Winter rules shape how the pavement is used. From November 1 to April 15, overnight parking in the older core between 19th Avenue North and 13th Avenue South alternates between avenues and streets from 1 to 7 a.m., which pushes more overnight parking onto private driveways. A snow emergency is declared when the National Weather Service forecasts four inches or more, and snow cleared from driveways and sidewalks may not go into the street, so it piles along the edges of the drive and the boulevard. Those banks melt against the asphalt on every warm afternoon, which is where edge cracking and crumbling usually begin.