What it does
Three small field calculators for snow, on one page, all working without internet once the page is open:
- Snow water equivalent (SWE): how much water the snowpack holds, in millimetres (1 mm is 1 kg on each square metre). Work it out from depth and density, from snow tube weighings (tube with snow, empty tube, core length) or from layers of a snow pit (thickness and density of each). The page also gives the bulk density and the ground snow load.
- Snow load on a roof: the ground load (from the SWE or a value you type) times your own roof factor, in kN/m², kg/m² and lb/ft², and the total on a roof area. It is not a design code: building codes set their own loads and factors, and roofs need an engineer.
- Slope angle: from map contours (interval, number of intervals, map distance and scale), from your phone’s tilt sensor laid on the slope, from a typed clinometer reading, or from two GPS points with elevations. The angle is shown on a 0 to 90° bar with the general band where most slab avalanches start (about 30 to 45°).
This is not an avalanche or safety forecast. Angle is only one part of avalanche terrain; the snowpack, the weather, the terrain above and the runout below all matter. Read your local avalanche forecast and take an avalanche course.
How to use it
- SWE: pick a method. For a snow tube, type the inner diameter of the cutter and one line per sample: the tube’s weight with snow (g), empty (g) and the length of the snow core (cm). For a pit, type one layer per line, thickness then density. You can also open a CSV file of samples or layers.
- Roof: keep “the SWE above”, or switch to typing a ground load. Type a roof factor (roof load ÷ ground load) and, if you like, the roof’s plan area.
- Slope: pick map, phone or GPS. On a phone, press Start the tilt sensor (iPhones ask for permission), lay the phone screen up on the snow or on a ski pole laid down the fall line, and press Hold this reading. For GPS, type both points or use Use my location at each one; heights from a map or altimeter are better than phone GPS heights.
- Download the results as CSV, or a PNG, PDF or Word report.
Worked example (made-up numbers)
- Depth and density: 85 cm of snow at 250 kg/m³ gives SWE = 212.5 mm, a ground load of 2.084 kN/m².
- Snow tube: a 4.6 cm tube (16.62 cm²) with three samples, 480, 505 and 460 g of snow over 78, 82 and 74 cm, gives SWE 288.8, 303.9 and 276.8 mm, so SWE = 289.8 mm (standard deviation 13.6 mm) and a bulk density of 372 kg/m³.
- Layers: 12 cm at 90, 25 cm at 180, 30 cm at 260 and 15 cm at 320 kg/m³ make 82 cm of snow with SWE 181.8 mm and a bulk density of 222 kg/m³.
- Roof: with the first example’s 2.084 kN/m² and a factor of 0.8, the roof load is 1.67 kN/m² (170 kg/m²); on 120 m² that is 200 kN, about 20.4 tonnes of snow.
- Map: five 10 m contour intervals across 3 mm on a 1:25 000 map: 50 m of rise over 75 m, 33.7°, in the 30 to 45° band.
- GPS: two made-up points 146.8 m apart horizontally and 95 m apart in height give 32.9°.
Tips
- Weigh the tube on the same scale with and without snow, and measure the core length, not the hole depth, if some snow fell out.
- Density above 917 kg/m³ is impossible (that is solid ice), so the page flags it: check grams, centimetres and the diameter.
- Contours hide small steep steps: a short convex roll can be much steeper than the map shows.
- A phone measures the surface right under it; measure in a few places and on the steepest part.
FAQ
Is a slope under 30° safe? No. Avalanches can start on lower slopes in some conditions, and gentle slopes are often in the path or runout of steeper ones. The band is a general fact about angles, not advice.
Why does my phone show no reading on a computer? Most computers have no tilt sensor. Type an angle from a clinometer instead.
Does anything leave my device? No. The tilt sensor, your location and your numbers stay in this page.
Where the numbers come from
- Formulas (general physics and snow science, no data copied): SWE = depth × snow density ÷ water density; snow tube SWE = snow mass ÷ tube cross-section; load = mass × standard gravity; slope = atan(rise ÷ run).
- Vincenty (1975), direct and inverse solutions of geodesics on the ellipsoid, with the WGS84 ellipsoid; W3C DeviceOrientation Event specification for the phone's tilt angles.
- General avalanche terrain fact that most slab avalanches start on slopes of about 30 to 45°, as taught in avalanche awareness courses; not a forecast.
- Example numbers are made up by fibub.
Standard scientific values, such as constants, atomic weights and melting points, are facts found in every textbook; we name where ours were checked. If you are an author or publisher and want a value, a credit or a table changed or removed, tell us and we will act quickly.
Last updated 2026-11-09.