By Julia · weer-meteo.be editorial team
Where and when snow falls in the Ardennes
The Belgian Ardennes form the highest relief in the country, with high points such as the Hautes Fagnes plateau and the Signal de Botrange, which reaches 694 metres, Belgium's officially highest point. Around this massif, towns such as Saint-Hubert and Bastogne sit on plateaus high enough for snow to be noticeably more frequent and longer-lasting there than elsewhere in the country, particularly from December to February, though early spells from November or late ones in March are not unusual.
Snow in the Ardennes most often results from a sufficient cooling of the air mass combined with altitude: the higher one climbs towards the Hautes Fagnes, the lower the temperatures drop and the greater the likelihood that precipitation falls as snow rather than rain. This relief, modest on an Alpine scale but decisive for Belgium, explains why some Ardennes municipalities build up a snow cover while the surrounding lowlands simply stay wet and grey.
The 0°C isotherm, key to understanding the rain-snow boundary
The 0°C isotherm marks the altitude at which air temperature reaches zero degrees. When this line sits above the Ardennes relief, precipitation falls as rain even on the heights; when it drops below the altitude of the plateau, snow can settle, sometimes only on the summits around Botrange, sometimes across the whole massif if the cold air sinks low enough. This line shifts from one day to the next, sometimes even from one hour to the next, which explains why it is hard to predict precisely where snow will start during a borderline episode.
It is precisely this sensitivity to altitude that explains why it can snow in Saint-Hubert or on the Hautes Fagnes while it is simply raining in Brussels, barely a hundred kilometres further north but at a much lower altitude. Following the 0°C isotherm in the forecast, rather than relying solely on the lowland temperature, remains the most useful habit for anticipating a snow episode in the Ardennes.
Typical snow episodes: easterly returns and polar air
Two patterns recur often when snow settles in for a longer spell in the Ardennes. The first is the "easterly return", when a cold air flow from central Europe or Russia skirts a high-pressure area and reaches Belgium from the east: this dry, cold air, meeting residual moisture, can produce snowfall over the Ardennes relief for several days in a row, often accompanied by a persistently grey sky and biting cold.
The second typical pattern is the arrival of maritime polar air, a moister flow from the north or north-west that brings showers which can turn to snow over the Ardennes once the air cools enough at altitude. This type of episode tends to be more unsettled, with snow showers interspersed with sunny spells, rather than continuous snow cover. In both cases, the combination of relief and the air mass's origin explains why the Ardennes remains the region most regularly affected by snow in Belgium.
Roads, ice and winter caution
The altitude and the temperature swings typical of the Ardennes make the roads across the massif particularly prone to ice, often earlier and for longer than in the rest of the country. A common winter phenomenon is black ice, which forms when rain or drizzle falls on a road surface that is already below zero, creating a thin, almost invisible layer of ice that is especially dangerous to drive on, notably on secondary roads and Ardennes passes around Bastogne, Saint-Hubert or the Vielsalm area.
Caution is also needed on exposed roads at altitude, where snow can linger for days after it has disappeared from the lowlands, and where freezing fog further hampers visibility. Before any trip to the Ardennes in winter, it remains essential to check road conditions and recommended equipment, and to follow the bulletins and warnings issued by the IRM/KMI during a snow episode or a significant risk of ice.
Cross-country skiing, sledging and following an Ardennes municipality
When snow holds for long enough, the Ardennes offer winter activities enjoyed by families and sports enthusiasts alike, particularly cross-country skiing and sledging. The Baraque de Fraiture site, a well-known high point for Nordic ski enthusiasts, and the Ovifat area near the Hautes Fagnes, are among the places traditionally mentioned for these activities when snow cover allows it. These sites remain dependent on sufficient, lasting snow cover, however, which is never guaranteed from one season to the next, or even from one week to the next.
Before heading to one of these sites, it is therefore advisable to check the recent trend in temperature and precipitation for the relevant Ardennes municipality, using that municipality's dedicated page on weer-meteo.be: it allows one to follow the trend of the 0°C isotherm, the precipitation forecast and the ice risk over the coming days, before confirming a cross-country ski outing, a sledging trip or simply a walk through a snow-covered forest. Local piste operators generally communicate on whether a site is actually open, a useful piece of additional information before setting off.
Coldest and mildest winters: the normals
80 of the 556 places we cover with 1991–2020 normals have at least one month whose average low is below 0 °C. The average winter low ranges from -1.7 °C in Butgenbach to 3.5 °C in Ostend.
Coldest winter lows
- Butgenbach (Liège): -1.7 °C
- Bullange (Liège): -1.7 °C
- Waimes (Liège): -1.4 °C
- Bastogne (Luxembourg): -1.4 °C
- Libramont-Chevigny (Luxembourg): -1.3 °C
Mildest winter lows
- Ostend (West Flanders): 3.5 °C
- Zuienkerke (West Flanders): 3.5 °C
- Bredene (West Flanders): 3.3 °C (the same normals as 1 other place)
- De Panne (West Flanders): 3.1 °C
- Jabbeke (West Flanders): 3.0 °C
| Region | Places | Average winter low (°C) |
|---|---|---|
| West Flanders | 57 | 2.3 |
| East Flanders | 55 | 1.9 |
| Flemish Brabant | 63 | 1.8 |
| Brussels-Capital Region | 19 | 1.7 |
| Antwerp | 67 | 1.7 |
| Walloon Brabant | 26 | 1.5 |
| Hainaut | 69 | 1.5 |
| Limburg | 38 | 1.2 |
| Namur | 38 | 0.7 |
| Liège | 84 | 0.5 |
| Luxembourg | 40 | -0.5 |
Computed from the 1991–2020 normals published on each town page (nearest weather station corrected for altitude, or ERA5 reanalysis): see the methodology page.