This article was originally posted on the University of Minnesota Extension website and was authored by Timothy Larson, Lewis Hendricks, Patrick Huelman, and Richard Stone. It can be viewed in its full, original format here.
An ice dam is a ridge of ice that forms at the edge of a roof and prevents melting snow (water) from draining off the roof. The water that backs up behind the dam can leak into a home and cause damage to walls, ceilings, insulation, and other areas. Figure 1 shows a cross section of a home with an ice dam.
There is a complex interaction among the amount of heat loss from a house, snow cover, and outside temperatures that leads to ice dam formation. For ice dams to form there must be snow on the roof, and, at the same time, higher portions of the roof’s outside surface must be above 32°F while lower surfaces are below 32°F. For a portion of the roof to be below 32°F, outside temperatures must also be below 32°F. When we say temperatures above or below 32°F, we are talking about average temperature over sustained periods of time.
The snow on a roof surface that is above 32°F will melt. As water flows down the roof it reaches the portion of the roof that is below 32°F and freezes. Voila! – an ice dam.
The dam grows as it is fed by the melting snow above it, but it will limit itself to the portions of the roof that are on the average below 32°F. So the water above backs up behind the ice dam and remains a liquid. This water finds cracks and openings in the exterior roof covering and flows into the attic space. From the attic it could flow into exterior walls or through the ceiling insulation and stain the ceiling finish.
Nonuniform roof surface temperatures lead to ice dams.
Since most ice dams form at the edge of the roof, there is obviously a heat source warming the roof elsewhere. This heat is primarily coming from the house. In rare instances solar heat gain may cause these temperature differences.
Heat from the house travels to the roof surface in three ways: conduction, convection, and radiation. Conduction is heat energy traveling through a solid. A good example of this is the heating of a cast iron frying pan. The heat moves from the bottom of the pan to the handle by conduction.
If you put your hand above the frying pan, heat will reach it by the other two methods. The air right above the frying pan is heated and rises. The rising air carries heat/energy to your hand. This is heat transfer by convection. In addition, heat is transferred from the hot pan to your hand by electromagnetic waves and this is called radiation. Another example of radiation is to stand outside on a bright sunny day and feel the heat from the sun. This heat is transferred from the sun to you by radiation.
In a house, heat moves through the ceiling and insulation by conduction through the slanted portion of the ceiling (Figure 1). In many homes, there is little space in regions like this for insulation, so it is important to use insulations with high R-value per inch to reduce heat loss by conduction.
The top surface of the insulation is warmer than the other surroundings in the attic. Therefore, the air just above the insulation is heated and rises, carrying heat by convection to the roof. The higher temperatures in the insulation’s top surface compared to the roof sheathing transfers heat outward by radiation. These two modes of heat transfer can be reduced by adding insulation. This will make the top surface temperature of the insulation closer to surrounding attic temperatures directly affecting convection and radiation from this surface.
There is another type of convection that transfers heat to the attic space and warms the roof. In Figure 1, the winding arrow beginning inside the house and going through the penetration in the ceiling, from the light to the attic space, illustrates heat loss by air leakage. In many homes this is the major mode of heat transfer that leads to the formation of ice dams.
Exhaust systems like those in the kitchen or bathroom that terminate just above the roof may also contribute to snow melting. These exhaust systems may have to be moved or extended in areas of high snow fall.
Other sources of heat in the attic space include chimneys. Frequent use of wood stoves and fireplaces allow heat to be transferred from the chimney into the attic space. Inadequately insulated or leaky duct work in the attic space will also be a source of heat. The same can be said about knee wall spaces.
The photograph below shows a single story house with an ice dam. The points of heat loss can be clearly seen as those areas with no snow. The ceiling below this area needs to be examined for air leakage, missing or inadequate insulation, leaky or poorly insulated ductwork, and the termination of a kitchen.
The photograph below illustrates unusually high heat loss from the roof. There is very little snow left on the roof and at its edge is both an ice dam and a “beautiful” row of icicles.
So it is primarily heat flowing from the house that is causing the nonuniform temperatures of the roof surface leading to ice dams.
In all Minnesota communities it is possible to find homes that do not have ice dams. Ice dams can be prevented by controlling the heat loss from the home.
Both of these actions will increase the snow load that your roof has to carry because it will no longer melt. Can your roof carry the additional load? If it is built to current codes, there should not be a structural problem. Roofs, like the rest of the home, should have been designed to withstand expected snow loads. In Minnesota, plans showing design details to meet expected snow loads are usually required to receive a building permit. The plans for your home may be on file at your local building inspection office. To help you understand the plans, or if you cannot find plans for your home, you may want to contact an architectural engineering firm. A professional engineer should be able to evaluate the structure of your home and answer your questions about the strength of your roof.
Mechanical attic ventilation IS NOT a recommended solution to ice dams in Minnesota. It can create other attic moisture problems and may cause undesirable negative pressure in the home.
Interior damage should not be repaired until ceilings and walls are dry. In addition, interior repair should be done together with correcting the heat loss problem that created the ice dam(s) or the damage will occur again.
The proper new construction practices to prevent ice dams begin with following or exceeding the state code requirements for ceiling/roof insulation levels.
The second absolutely necessary practice is to construct a continuous, 100% effective air barrier through the ceiling. There should not be any air leakage from the house into the attic space!
Recessed lights, skylights, complicated roof designs, and heating ducts in the attic will all increase the risk of ice dam formation.
Moisture entering the home from ice dams can lead to the growth of mold and mildew. These biologicals can cause respiratory problems. It is important that the growth of mold and mildew be prevented. This can be done by immediately drying out portions of the house that are wet or damp.
University of Minnesota, U.S. Department of Agriculture, and Minnesota Counties cooperating.
Sure, Minnesota has shown up at the top of many lists praising the state for its bike paths, child wellness, charity and much more. But it all comes with a catch: the state’s challenging winter.
According to a recently compiled list on Thrillist, Minnesota winters are not only miserable, but the most miserable in the United States – beating out even Alaska. Really? Ouch.
“Parts of northern Minnesota see up to 170in of snow in a winter,” the list states. “One hundred seventy inches! That’s like two and a half times the height of Kent Hrbek!! It can get down to -60 degrees, a temperature at which frostbite can occur in fewer than five minutes. There are no chinook winds or moderating oceans to temper things outside of a small area by Lake Superior.”
Adding insult to injury, the list even makes a crack at Minnesota’s sports teams.
“Your sports teams never win championships. All of your good high school hockey players end up starring for NHL teams in other cities. Ice fishing can’t be that cool, really.”
Hey now, we have the Minnesota Lynx. They won the WNBA title in 2001, 2013 and 2015!
Michigan ranked No. 2 and coming in last with the least miserable winter on the list: Hawaii.
This depends on the types of windows installed and the relative humidity levels in the home.
This is caused by a combination of high interior air humidity and a large temperature difference between the window and the indoor air. When warm interior air hits the cold window, it decreases in temperature. Cold air cannot hold as much moisture as warm air, which is why the condensation forms. If the condensation forms in large quantities and runs down the glass, the windowsill or underlying wall materials may become moldy or moisture damaged, and could require repairs.
Remedies for reducing the formation of condensation include:
• Lowering the humidity (removing plants, hanging laundry, storing wood outside to dry, installing an exhaust fan, etc.)
• Installing heat sources below windows to reduce the formation of condensation by flowing warm air across the glass.
• Installing storm windows on single-pane windows, and keeping blinds or curtains slightly away from the windows to allow airflow in front of the windows.
The seals between the panes have deteriorated, which allows condensation to form between the panes of glass. Although it cannot be cleaned and is often considered inconvenient to look through, this diminishes the insulating capacity of the window only slightly. However, it is often considered inconvenient to look through. Correction of the problem typically involves having the window replaced.
• Double or triple-glazed glass (i.e. thermopiles). These are two or three panes of glass manufactured as one window with a very thin separation between the panes. This separation width provides less convective heat loss than the typical separation width of 2-4 inches, which is often observed on standard thermopane or singlepane windows equipped with a storm window.
• Low-E coatings. Installing heat sources below windows to reduce the formation of condensation by flowing warm air across the glass.
• Inert gas fills. Another big advancement in window technology has been the introduction of inert gas fills into the space between the glazings. Argon and krypton are the usual choices, with argon being the most common. Filling the space between the glazing with these heavier gases reduces heat loss due to convection and conduction.
• Low-conductivity spacers. The spacer between the glazing at the perimeter of the window has historically been made out of aluminium, which is not only lightweight and durable, but also provides considerable heat loss. Newer non-metallic spacers are now available to reduce heat loss at this location.
The cost for the inclusion of the energy efficiency features described above varies, but can be 10-15 percent more than standard double-glazed units. However, many window manufacturers are converting their production lines to produce only high-performance units. Some super high-performance windows that are using cutting-edge technology for even more energy savings than those described above are available, but at considerably higher costs.
Proper installation is especially important with high-performance windows because poor installation techniques can negate their performance. Installation should be completed in accordance with manufacturer’s recommendations and should reflect current industry standards. Be sure to check out your contractor’s qualifications to ensure proper installation.
Completion of an energy efficiency assessment is recommended prior to upgrading in order to determine the feasibility of upgrading windows.
Contact AmeriSpec Inspection Services to learn more.
This article appeared as a newsletter from AmeriSpec Inspection Services in December of 2015.