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The mountain atlas

Montenegro’s mountains, park by park and summit by summit

16 subjects: 5 national parks, the summits worth the walk, and the ski areas. Every one carries the answer nobody else publishes for this country — how often the snow actually lies, winter by winter, for eleven years. The highest ground is Prokletije, at 2,535 m.

Subjects
16
Protected
1,037 km²
Winters of record
10
Daily readings
64,288

Start here

The five national parks and the summits people actually climb, in the order we would send someone.

Where the snow lies, and for how long

The share of days carrying a base of 30 cm or more, from 10 winters of daily reanalysis. January is the test and April is the one that ruins trips — a third of April days on the high massifs still carry a base.

Snow reliability by subject
SubjectSummitJanAprBare ground
Zla Kolata2,535 m74%41%May–Nov
Savin Kuk2,313 m72%38%May–Nov
Prokletije2,535 m71%33%May–Nov
Bobotov Kuk2,523 m69%32%May–Nov
Durmitor2,523 m69%32%May–Nov
Hajla2,403 m67%28%May–Nov
Kom Kučki2,487 m65%25%May–Nov
Kolašin 16002,035 m62%23%May–Nov
Kolašin 14501,750 m62%23%May–Nov
Biogradska Gora2,139 m57%21%May–Nov

5 subjects are missing from this table on purpose. Their grid cell does not resolve snow and we publish no depth for them rather than a number we do not believe — the method section says why.

Skiing

Two lift-served areas on the same Bjelasica flank above Kolašin, plus the chairlifts on Savin Kuk above Žabljak. What follows is eleven winters of record, not a snow report — check the resort on the day.

By massif

Durmitor

Bjelasica and the Komovi

Prokletije

Orjen and Lovćen

Rumija

Lake Skadar

How this is put together

Elevations and coordinates come from OpenStreetMap peak nodes, and every subject names the node it used. Park areas are measured from each park’s own boundary relation rather than copied — which is why Durmitor reads 323 km² here against the 390 km² usually quoted, a figure that takes in the Tara canyon buffer outside the boundary.

Temperatures are eleven years of daily reanalysis from Open-Meteo’s ERA5-Land archive, downscaled to each subject’s own elevation. Durmitor’s plateau at 1,970 m and Bobotov Kuk at 2,463 m came back 3.2 °C apart on the same January day, which is the standard lapse rate doing its work. A summit’s temperature record is that summit’s.

Snow depth is not downscaled. It is the value for a grid cell about nine kilometres across, so it describes the massif rather than the summit, and where two subjects fall in one cell the depth record is literally the same record — the page says so when it happens. On the coastal ridges that cell is mostly low ground beside a warm sea, and it reports almost no snow at altitudes its own temperatures put below freezing. For 5 subjects we therefore publish no depths at all. Eighteen centimetres in eleven winters on Orjen, which sits behind the wettest station in Europe, is not a measurement.

Today’s figures are different in kind: real measurements from the national hydrometeorological institute’s official station network, 22 stations reporting precipitation, minimum and maximum temperature and snow depth. They are shown separately from the record because a reading and a model are not the same claim. An empty snow field means not reported, never zero.

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