The first snow of the season rarely causes concern in Millcreek. A few inches cover the roof, the driveway, and the lawn. It starts melting the next day. Then another storm arrives. Homeowners in the valley may not have any snow left from the previous storm. But If you live along the East Bench, and your roof is still covered, you may have reason to worry about how much more snow your roof will get when the next one arrives.
As you move higher into Millcreek’s foothills, colder temperatures can allow snow to remain on a roof longer between storms. When snow does not melt as quickly, it may accumulate, adding weight to your roof for a longer period. Storms that stack on top of one another can make the problem worse.
Snow doesn’t have to look especially deep to add substantial weight to a roof. Wet snow is particularly heavy, and successive layers can build when temperatures remain low enough to prevent significant melting.
While the problem is more common for homes at higher elevations, elevation is only one part of that equation. Roof slope, design, construction and the condition of your residential roofing system all affect how your home handles winter weather.
Why the East Bench Sees More Snow Than the Valley Floor
As you travel higher in elevation, the air gets colder. This colder air lets snow linger longer before it melts, and storm systems moving across the Wasatch Front often drop more precipitation as they climb toward higher ground. A storm that leaves the valley floor with a light dusting can drop several more inches on a foothill street.
Thankfully, Utah’s building code requires that ground snow loads increase incrementally as elevation rises, so a home built at a higher point on a bench is generally engineered for greater snow load than a home built near the valley floor just a mile or two away, even within the same city.
What Higher Elevation Means for Your Roof
While that higher design standard is a starting point, it’s still not a guarantee for the specific roof on your house. Age, past repairs, and how well a roof has been maintained all affect how closely your roof meets the standard it was originally built to. A well-built roof at elevation can still be pushed toward its limit by an unusually heavy storm, and an older roof may have even less margin for error.
In addition, snow on a north-facing roof on the shaded side of the bench may stick around far longer than a south-facing roof that gets direct sun for part of the day. Two houses on the same street can end up with very different snow loads based solely on the direction their rooflines face.
When Roof Snow Removal Makes Sense
Not every snowfall calls for removal. A few inches of light powder rarely puts significant stress on a roof built for this climate, but you are welcome to have it done if it gives you peace of mind. However, removal might be a good idea if the snow depth builds up over multiple storms without a chance to melt in between, or if a north-facing section holds onto snow long after the rest of the neighborhood has cleared.
A few signs to look for when considering professional snow removal:
- Visible sagging along the roofline or near valleys where snow tends to collect
- Sticking doors or windows after a heavy snow
- A snow depth that’s noticeably deeper on your roof than on similar homes nearby
- Ice building up at the eaves
Many roofing companies in Utah know how to clear snow without damaging shingles, and they carry the equipment to reach steep or high sections that are not safe to approach with a rake from the ground. A snow-covered roof can be risky to clear on your own, especially on a bench lot with a steep pitch, but it is usually a routine task for professionals.
If your roof is older or has a shaded, north-facing slope, it may be wise to schedule a professional snow removal team to inspect it after a storm. Both hold onto snow longer than a newer roof or a sunnier exposure, which gives ice more time to build up at the eaves before anything melts off naturally.
When to Schedule Snow Removal
The best time to address a heavy roof load is before a freeze-and-thaw cycle turns standing snow into ice. Snow that sits through a warm afternoon and refreezes overnight becomes far heavier and harder to remove than it would have been a day earlier. On the East Bench, where the angle of some roofs already creates uneven melting across a single roof, that window can close faster on the shaded side of the house than the sunny side.
Getting Ahead of a Foothill Winter
The views may be one of the perks of living higher on Millcreek’s East Bench, but the extra elevation can bring extra snow load, too. Knowing your roof was designed for its location is helpful, but it is not a substitute for regular inspections and maintenance.
If this winter is piling up more snow than usual, do not wait until your roof starts showing signs of stress. Schedule professional roof snow removal early to help keep a manageable winter buildup from becoming a much bigger problem.