Savoie mountain weather: freezing level and rain-snow line
Heading into the mountains: the official bulletins
This page compares model forecasts. For a high-mountain outing, use Météo-France’s mountain weather bulletin and avalanche risk bulletin, with their dates, and the advice of a professional.
Operators’ images, refreshed at their own pace; they are not a continuous video stream. Click to enlarge; check the capture time on the image or at the source.
Sectors and altitudes
Model estimates at the altitude of each row; these are not measurements.
The freezing level is the altitude where the model puts a temperature of 0 °C; the rain-snow line is estimated 200 to 400 m lower. Source: Open-Meteo, updated every hour.
To read mountain weather, look at the altitude, not the village. This table compares eleven sectors of the Northern French Alps: freezing level (0 °C isotherm), rain-snow line, forecast snowfall and wind, with how they are worked out and their limits.
In short. The freezing level (0 °C isotherm) is the altitude at which the Open-Meteo model puts a temperature of 0 °C; the rain-snow line is estimated 200 to 400 m lower. The wind shown is the model wind 10 m above the ground, at each point’s altitude: on the ridges it can be stronger. These are model estimates, not measurements or a mountain bulletin.
Understanding the conditions
The freezing level: what the figure means
The freezing level, or 0 °C isotherm, is the altitude above which the air is below zero, according to the model, at the time shown. It rises in mild spells and drops when a cold air mass arrives. It is a guide for snow, ice on a high road or frost on a hike, not a measurement.
The rain-snow line: a range
To estimate how low the snow will fall, the site subtracts 200 to 400 m from the freezing level. So it gives a range, never an altitude to the nearest metre: the intensity of the precipitation, humidity and terrain can shift it. The rain-snow line does not tell you whether the snow will settle on the ground.
Wind at altitude
The wind in the table is the model wind 10 m above the ground, at the altitude of each row. On a ridge or a pass, actual gusts can be much stronger; no ridge measurement is shown here.
Why massifs rather than a town?
A valley town tells you nothing about the weather at 3,000 m. For each sector, the table gives the village and the resort’s high point: you can read the difference in altitude and temperature at the same moment.
It is the altitude at which the weather model puts a temperature of 0 °C. Above it, the air is below freezing; below it, it is milder.
How is the rain-snow line estimated?
By subtracting 200 to 400 m from the freezing level. The result is an altitude range; it is neither a measurement nor a guarantee that the snow will settle.
Is the wind shown the wind on the summits?
It is the model wind 10 m above the ground, at each point’s altitude. On ridges or passes it can be stronger: no summit measurement is shown.
Does this page replace a mountain weather bulletin?
No. For an outing at altitude, check Météo-France’s mountain weather bulletin and avalanche bulletin, with their dates.
Sources and method
Text of this page last revised on . This date says nothing about how recent the images or data are: the webcams are supplied by the credited operators and their timestamp shows when the image was taken; model forecasts and official reports are separate pieces of information, each with its own time.