Frostline.info

How we estimate frost depth

1. The freezing index

The air freezing index (AFI) adds up how far, and for how long, daily average air temperature stays below 32°F over a winter. A winter that averages 10°F below freezing for 30 days scores 300 °F-days. NOAA's National Climatic Data Center computed AFI return periods for 3,110 US weather stations from 1951–80 records. We use the 100-year return period: a winter that cold happens about once a century. The same dataset is behind the air-freezing-index map in the International Residential Code, which is used to design frost-protected shallow foundations.

2. From station to ZIP code

For each ZIP code we take the three nearest stations and average their AFI, weighted by the inverse square of distance. County figures average the county's ZIP codes. Stations sit at specific elevations, so mountain ZIP codes far from a station can be colder or milder than shown.

3. From freezing index to inches

We use the modified Stefan equation from frost engineering:

depth = λ · √(48 · k · n · AFI ÷ L)

SoilkMoistureDry densityλ
Sand / gravel1.310%120 pcf0.65
Silt / loam0.920%100 pcf0.80
Clay0.830%90 pcf0.85

4. Typical code footing depth

Building codes do not use our estimate. Each jurisdiction adopts a fixed frost-line depth, usually rounded up for safety. To show what codes in a similar climate commonly require, we fit a curve (depth ≈ 1.35 × AFI0.465) to the adopted frost depths of about 20 US cities and show a range of ±20%, rounded to 6 inches, with a 12-inch floor. Local requirements can fall outside this range.

Limitations

Sources