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North zone

Problem

Slopes

Size

Overload

Trend

Centre zone

Probleme

Slopes

Size

Overload

Trend

South zone

Problem

Slopes

Size

Overload

Trend

Off-piste snow cover thicknesses

North zone		Snow thickness
Snowpack		1500m	2000m	2500m
N	1600 m	0 cm	150 cm	200 cm
S	1900 m	0 cm	100 cm	150 cm

Center area		Snow thickness
Snowpack		1500m	2000m	2500m
N	1600 m	0 cm	150 cm	200 cm
S	1900 m	0 cm	100 cm	150 cm

South zone		Snow thickness
Snowpack		1500m	2000m	2500m
N	1600 m	0 cm	120 cm	150 cm
S	1900 m	0 cm	60 cm	100 cm

Snowpack stability

In particular on sunny slopes individual small and medium-sized moist avalanches are possible as a consequence of warming during the day and solar radiation. Explanation: these may only stand for these avalanches can be released naturally. Gliding avalanches can also occur at any time. High altitudes and shady slopes :. The near-surface layers of the snowpack can be released in isolated cases and mostly by large additional loads. The avalanche danger will persist.

Snow quality

Low altitudes :. The surface of the snowpack will freeze to form a strong crust will already soften in the late morning. Areas with glide cracks are to be avoided. shady slopes and intermediate and high altitudes :. The upper section of the snowpack is dry and has a loosely bonded surface. Snow depths vary greatly above approximately 2400 m, depending on the infuence of the wind. The conditions are spring-like. Until Friday the weather will be sunny at times. Above approximately 1200 m snow will fall from the afternoon in particular in the north.

Detailed information for protected areas

Sorteny

At altitude, the wind has transported the little available snow and formed small irregular accumulations and, especially on the northern slopes, there is very pleasant snow for skiing. In the lower parts and on sunny slopes, the snow is hard in the morning, it is recommended to be equipped with spiked material to circulate, but it will soften throughout the day.

Comapedrosa

There is less and less continuous snow at the lower elevations of the Park. In the early hours we will have to be careful not to slip due to the ice crust on the southern slopes or at low altitudes. In the upper parts of the Park, numerous excursions can be made, always maintaining a careful choice of the itinerary.

Madriu-Perafita-Claror

The mantle is generally thin and irregular, with better snow continuity on the northern and obscure slopes. It has been the sector most affected by the precipitation, with new snow that is abundant above the forest line, although in some high places the wind has left the old snow, exposed.

Thick snow in recent days (last 24 hours measured at 06:00 UTC)

	07/03/2026	08/03/2026	09/03/2026
FEDA (Central)	0 cm	0 cm	0 cm
Engolasters - FEDA	0 cm	0 cm	0 cm
Ransol - FEDA	0 cm	0 cm	0 cm
Fontverd	0 cm	1 cm	0 cm
Bony de les Neres	0 cm	0 cm	0 cm
Grau Roig - FEDA	0 cm	4 cm	1 cm
Caborreu	0 cm	0 cm	0 cm
Sorteny	2 cm	6 cm	4 cm
Coll Pa	0 cm	0 cm	0 cm
Perafita	0 cm	3 cm	0 cm
Tossa Espiolets	0 cm	2 cm	0 cm
La Solana	1 cm	5 cm	0 cm
Vall del Riu FEDA	3 cm	3 cm	0 cm
Envalira Antenes	0 cm	9 cm	3 cm
Les Fonts d'Arinsal	0 cm	4 cm	0 cm

Breu guia nivometeorològica

This bulletin has been prepared in collaboration with Météo France and prepared following the rules and recommendations of the European Avalanche Warning Services, of which the National Meteorological Service is a member.

Hazard Index	Snow Cover Stability	Trigger probability	Off-piste skiing directions and recommendations
5 Very strong	The mantle is poorly consolidated and very unstable in general.	Numerous very large and even extremely very large avalanches are expected to fall spontaneously, even on slightly sloping terrain *.	Excursions and presence in the mountains must be abandoned. < / td>
4 Strong	The snow cover is weakly stabilized on most sloping slopes *. < / td>	Avalanche triggering is likely even due to weak overload ** on numerous sloping slopes *. Sometimes spontaneous falls from numerous large and often very large avalanches can be expected.	Excursions limited to areas with a moderate slope and without being exposed to avalanches that are triggered from upper parts.
3 Marcat	The snow cover is between moderately to weakly stabilized on numerous sloping slopes *.	Avalanche triggering is possible even due to weak overload ** especially in the terrain * indicated in the bulletin . In some situations it is possible to fall spontaneously from some large avalanches and in isolation from very large ones.	Sloping slopes at altitudes and orientations indicated in the BPA should be avoided. It requires a lot of experience and a good ability to appreciate the danger of avalanches. It is essential to choose the terrain according to the conditions.
2 Moderate	The snow cover is moderately stabilized on some sloping slopes *; in the rest it is well stabilized.	The triggering of avalanches mainly by strong overload ** on sloping terrain *, usually described in the bulletin. Spontaneous avalanches of very large size are not expected.	Careful planning of excursions is required. Caution is advised in the selection of the route, especially it is necessary to avoid inclined slopes with the indicated orientation and altitude.
1 Weak	The snow cover is generally well stabilized.	In general, triggers are only possible in isolation due to strong overload ** on very sloping terrain *. Only small and medium avalanches are possible spontaneously.	Excursions and downhill skiing are possible almost without restrictions, although BPA recommendations must be followed.

Avalanche danger bulletin of Principat d'Andorra

Off-piste snow cover thicknesses

Snowpack stability

Snow quality

Detailed information for protected areas

Sorteny

Comapedrosa

Madriu-Perafita-Claror

Thick snow in recent days (last 24 hours measured at 06:00 UTC)