Ice thickness

In addition to point-like observations, the ice situation map shows the estimates calculated by the forecast model. You shouldn't go to the ice based on the map estimates alone, because the local variation can be big! Especially immediately after freezing, the ice can be much weaker in currents and backwaters than, for example, in coastal areas. In spring, when the snow has melted, the sun can make even the thickest ice brittle in just a couple of hours.

Ice situation 15.5.2026

Ice thickness is currently only measured in Northern Lapland

On 10 May, ice thickness could only be safely measured in Lake Kilpisjärvi, Lake Kevojärvi in Utsjoki and Lake Ounasjärvi in Enontekiö. on the observation day, the total ice thickness was 89 cm in Lake Kilpisjärvi, 49 cm in Lake Kevojärvi and 33 cm in Lake Ounasjärvi. In Lake Ounasjärvi, the total ice thickness was 20 cm below the seasonal average, and bubbles were visible in the black ice, i.e., it was already brittle.

Syke warms people of thin ice and points out that in the spring, as snow melts and sunlight increases, the thickness of the ice no longer indicates its load-bearing capacity, and the ice becomes brittle. This may cause even seemingly thick ice to be deceptively weak. The ice cover may be surprisingly fragile even in familiar waters, especially in streams and narrow channels, at ditch mouths, as well as close to water structures and vegetation. Persons travelling on ice must carefully verify the load-bearing capacity of the ice along the entire route. It should also be remembered that the ice may be more load bearing in the morning after a frosty night, but it may already have deteriorated significantly in the afternoon due to sunshine.

The Finnish Environment Institute updates the estimate of the ice situation on this page three times a month. The estimate is based on ice thickness measurements at 46 observation sites in different parts of Finland. The ice thickness is measured approximately on the 10th, 20th and 30th day of every month.

You can view the latest observations on the ice situation map (available in Finnish and Swedish). Anyone can record their own ice observations, in which case they will be shown on the map, but the Finnish Environment Institute does not verify these observations. You should not go on the ice solely based on the estimates and observations on the map because ice quality and thickness vary greatly between different water bodies and even within the same lake.

You can observe the general development of the ice situation by a computational estimate of ice thickness, i.e., the colours on the map. The estimate is made by modelling, and it utilises ice thickness observations as well as weather data and forecasts, for instance. It is not possible to determine the actual ice thickness of any waterbody based on the ice situation map. The ice thickness observations are only representative of the specific site on the date of the measurement and are therefore indicative and cannot be extrapolated to large areas.

Further information

Ihmiset ulkoilevat kevätjäällä Siilinkarin majakan edustalla Tampereen Pyhäjärvellä

Stay safe on ice from autumn till spring

If you intend to go out on ice, you should always make sure that it is strong enough on the route you intend to take. Get to know the properties of ice in different seasons and pay attention to possible hazards.

Autumn ice

The water starts freezing in autumn when its surface temperature drops below zero. Shores and bays are the first to freeze over, while any deep areas and places with a current get their ice cover last. It is typical for ice thickness to vary in different areas of a lake or the sea in autumn. Measure the thickness of the ice on your route to be sure that it will carry you. Transparent clear ice must be at least five to ten centimetres thick before it carries a person walking on it.

Spring ice

As the air grows warmer and the sun’s radiation becomes stronger in spring, the snow and ice cover starts to melt. Once the snow is gone and solar radiation starts melting the ice, its structure becomes more fragile and cavities appear in the ice layer, and you can no longer conclude the bearing strength of the ice by measuring its thickness. Even if it were 20 to 30 centimetres thick, the ice can be too fragile to carry the weight of a person.

Hazardous areas

Particularly hazardous areas are straights, deep areas and places with a current, including at river mouths and near springs, sewers and stormwater drains, where the ice may remain thin throughout the winter. You should also monitor the ice thickness near large stones, docks and other structures as well as aquatic plants. Shipping lanes, and cracks and holes cut in the ice, are dangerous even in mid-winter. Snow cover makes it more difficult to spot areas of weak ice.

2.12.2019

Is the ice strong enough?

Talvinen jokimaisema, hyydetulva muodostumassa jokeen.

3.2.2020

Frazil ice causes winter floods

Fun facts about ice

Clear ice and slush ice

The ice cover on the sea or a lake may consist of clear ice, slush ice and water layers inside the ice, and the quality of the ice may vary in different areas. On still waters, clear ice is formed, which is transparent and looks dark when a hole is drilled through it. When water rises on top of the ice, the snow becomes slushy and then freezes into slush ice. Slush ice is opaque and often milky in colour, and it only has around one half of the bearing strength of clear ice.

Ice measurements at monitoring stations

Ice thickness is measured regularly around Finland at 47 monitoring stations, which usually are located at least 50 metres away from the shore. The stations are visited three times a month, and each time the total thickness of not only clear ice but also slush ice and any water layers are measured. Other measurements include the water level from the lower surface of the ice and thickness of the snow layer on ice. The bearing strength of ice is always expressed for clear ice.

Freezing and melting

When surface water temperature drops below zero, the water starts to freeze. The ice cover may grow by one or two millimetres a day per degree of subzero temperature. When the average air temperature is –10 degrees centigrade, several centimetres of ice may form in 24 hours. Once the snow has melted in spring, solar radiation may penetrate the ice layer and also melt it from below. Cavities with rod-like crystals appear in the ice cover, and even if it is thick, it will no longer carry a person.

Ice cover and climate change

Data collected over the years on ice thickness and the length of the ice-covered period show how Finnish winters have changed. These datasets indicate that the ice cover forms a few weeks later and melts a few weeks earlier than hundred years ago. Consequently, the period of ice cover is now around one month shorter. The trend in ice thickness is less clear as it has decreased in Southern Finland but increased in Northern Finland as a result of higher precipitation and a larger share of slush ice.

Recreation on ice

Ice may be difficult to walk on, but strong ice also offers great possibilities for outdoor exercise and recreation. Many people enjoy tour skating, skiing on lake ice, winter swimming and fishing through ice. Ice-free winters and the shortening period of ice cover reduce these recreational opportunities. If you go out on ice, you should learn to check that it will carry you and observe your surroundings and potential hazardous places.

Water situation snapshots

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