Ice Dams: What Causes Them and What Actually Fixes Them

If you live in Western New York you have seen them: a ridge of ice along the eave, icicles hanging off the gutter, and sometimes a stain appearing on the ceiling inside. Most homeowners treat this as a roof problem or a gutter problem. It is neither.

The mechanism

An ice dam forms when the upper part of your roof is warm enough to melt snow and the lower part is not. Meltwater runs down the roof under the snow, reaches the eave, which overhangs unheated space, and refreezes there. The ice builds up into a ridge. More meltwater arrives, and now it is pooling behind a dam, sitting on shingles that were designed to shed water, not hold it. Eventually it finds a way underneath and into the roof deck, the wall, or the ceiling.

The key point is the temperature difference across your roof. It exists because heat is escaping from your living space into the attic and warming the roof deck from below. The roof is doing its job. The attic is the problem.

Why the usual fixes do not fix it

Heated cables melt a channel through the dam. They do not stop the dam forming, they cost money to run all winter, and they are managing the symptom in perpetuity.

Raking snow off the roof works while you do it, which is not most of the winter, and it puts you on a ladder in the exact conditions where you should not be on a ladder.

New gutters change nothing. Gutters are where the ice is visible, not where it comes from.

Adding attic insulation alone helps, but usually less than people expect, because the dominant heat path in most homes is air leakage rather than conduction. Piling material on an unsealed attic floor leaves the air path open.

What actually stops them

Three things, in this order.

Air sealing the attic floor. Top plates, plumbing and electrical penetrations, flue and chimney chases with correct fire-rated material, duct boots, dropped soffits, recessed light housings, and the hatch. This is where the warm air is getting into the attic, and closing those paths is the single highest-impact thing you can do.

Bringing the insulation to target. Once the air path is closed, depth does what it is supposed to do. In Western New York the target is R-49 to R-60.

Keeping the ventilation clear. A cold attic is a dry attic, and soffit-to-ridge airflow is what keeps it cold. Insulation pushed into the eaves blocks the soffit vents, so baffles go in at the same time. Skipping them trades an ice dam for a moisture problem in the roof deck.

The one to take seriously

If you see a stain spreading on an upstairs ceiling or on the inside of an exterior wall during a thaw, water is already getting in. That is a call to make now rather than in spring, because the damage compounds and because the drying-out season is a long way off.

What we would ask you not to do is climb up and chip at the ice. People do it every winter, and they damage shingles, they damage gutters, and a meaningful number of them fall. It also does not address the cause, so the dam comes back with the next snowfall.