Winter arrives in Scandinavia: snow and rain on the radar
On 10 October 2026, RADAR + NowCast shows snow, sleet and rain across Scandinavia, while southern Spain still reaches 29 degrees.
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While Spain is enjoying mostly quiet autumn weather with pleasant temperatures on the second October weekend, the weather in northern Europe is already showing its wintry side. On Saturday morning, 10 October 2026, RADAR + NowCast from meteo365.es is registering extensive areas of precipitation with snow, sleet and rain in parts of Scandinavia. The current situation shows how differently autumn can unfold across Europe.
meteo365.es news desk | 10 October 2026
Particularly striking is a larger area of wintry precipitation over eastern Finland and the neighbouring region of Karelia. There the radar shows extensive snow signals, while further south areas of rain occur as well.
Another interesting weather zone extends over parts of southern Norway and southern Sweden. Around Oslo and towards the Swedish Baltic coast, different types of precipitation can be made out on the radar map.
While rain is falling in some areas, other regions already show sleet or snow.
The distribution shows that wintry conditions are not spreading evenly across Scandinavia. Instead, the types of precipitation change from region to region and depend on the respective temperature conditions.
What matters is not only the temperature at the ground, but the temperature profile of the entire atmosphere.
Snowflakes form in sufficiently cold parts of the cloud. On their way to the surface they pass through different layers of air.
If the air is cold enough all the way to the ground, the snowflakes can survive. If they meet warmer air, they begin to melt. Depending on the temperature profile, rain or mixed forms of precipitation result.
Altitude also plays an important role. While rain falls in lower-lying regions, it can already be snowing in nearby higher areas.
In autumn it is therefore important not only to see where precipitation is occurring, but also in which form it could reach the ground.
A conventional precipitation image is perceived by many users as a rain map. In reality, different types of precipitation can hide behind the signals shown.
In its display, RADAR + NowCast from meteo365.es distinguishes between four important forms:
The different types of precipitation are marked on the interactive map with their own symbols and display characteristics.
The classification is based on the available meteorological data and is to be understood as a current assessment. Especially in transition areas between rain and snow, actual conditions at the ground can differ locally.
The term nowcasting describes the meteorological short-range forecast for the time immediately ahead.
While classic weather models calculate atmospheric development over hours or several days, nowcasting concentrates on the short-term movement and development of weather features that already exist.
On the interactive map you can follow how areas of precipitation have moved recently and where they are likely to move in the next few minutes.
In changeable autumn weather in particular, this information can be helpful, for example when planning drives, walks or other outdoor activities.
With wintry precipitation, the distinction between rain, sleet and snow matters as well. Type and intensity can change at short notice, however, which is why NowCast forecasts also carry uncertainties.
While wintry precipitation is already occurring in parts of northern Europe, much of Spain is expecting a calm and pleasantly warm autumn day this Saturday.
In Andalusia, for example, highs of around 29°C are forecast in Seville, 27°C in Huelva and 26°C in Córdoba. On the Costa del Sol around 23°C can be expected.
The difference between conditions in southern Spain and the wintry areas of precipitation in Scandinavia is therefore considerable.
Such contrasts are not unusual in October. While the land masses of northern Europe cool down increasingly and outbreaks of cold air make wintry conditions possible, comparatively warm air masses can still hold on in the Mediterranean.
Autumn in Europe is thus showing its late-summer and its already wintry side at the same time.
In northern Scandinavia and at higher altitudes in particular, snowfall during autumn is a normal part of the seasonal transition.
Whether a closed snow cover forms and lasts for a longer time depends on temperatures at the ground, the amount of precipitation and how the weather develops further.
Even after the first wintry precipitation, milder air masses can reach Scandinavia again.
The current radar picture therefore documents a wintry spell first of all, not necessarily the start of a lasting snow cover.
RADAR + NowCast shows areas of precipitation across large parts of Europe and makes it possible to distinguish between rain, sleet, snow and hail.
Using the time bar, users can follow the development so far and look at the short-term forecast movement of the precipitation.
This makes visible not only where precipitation is occurring, but also how dynamically the weather is developing within Europe.Editorial note: this article is based on the radar display from Saturday morning, 10 October 2026. Radar-based precipitation classifications can differ from actual ground observations, especially in transition zones between rain and snow.
meteo365.es news desk | 10 October 2026
Wintry precipitation reaches parts of Scandinavia
Autumn is progressing in northern Europe. On the current European radar map from meteo365.es, clear differences between the types of precipitation can be seen on Saturday morning.Particularly striking is a larger area of wintry precipitation over eastern Finland and the neighbouring region of Karelia. There the radar shows extensive snow signals, while further south areas of rain occur as well.
Another interesting weather zone extends over parts of southern Norway and southern Sweden. Around Oslo and towards the Swedish Baltic coast, different types of precipitation can be made out on the radar map.
While rain is falling in some areas, other regions already show sleet or snow.
The distribution shows that wintry conditions are not spreading evenly across Scandinavia. Instead, the types of precipitation change from region to region and depend on the respective temperature conditions.
Why rain and snow occur so close together
Especially during the transitional months of October and November, weather conditions in northern Europe can differ considerably over relatively short distances.What matters is not only the temperature at the ground, but the temperature profile of the entire atmosphere.
Snowflakes form in sufficiently cold parts of the cloud. On their way to the surface they pass through different layers of air.
If the air is cold enough all the way to the ground, the snowflakes can survive. If they meet warmer air, they begin to melt. Depending on the temperature profile, rain or mixed forms of precipitation result.
Altitude also plays an important role. While rain falls in lower-lying regions, it can already be snowing in nearby higher areas.
In autumn it is therefore important not only to see where precipitation is occurring, but also in which form it could reach the ground.
RADAR + NowCast: not every precipitation is rain
This is exactly where RADAR + NowCast from meteo365.es comes in.A conventional precipitation image is perceived by many users as a rain map. In reality, different types of precipitation can hide behind the signals shown.
In its display, RADAR + NowCast from meteo365.es distinguishes between four important forms:
- Rain: liquid precipitation that reaches the surface as water drops.
- Sleet: mixed precipitation of rain and snow, which often occurs at temperatures around freezing.
- Snow: frozen precipitation in the form of ice crystals and snowflakes.
- Hail: solid grains of ice that form above all in strong convective clouds and thunderstorms.
The different types of precipitation are marked on the interactive map with their own symbols and display characteristics.
The classification is based on the available meteorological data and is to be understood as a current assessment. Especially in transition areas between rain and snow, actual conditions at the ground can differ locally.
What NowCast adds
Besides showing current precipitation, meteo365.es offers a NowCast function.The term nowcasting describes the meteorological short-range forecast for the time immediately ahead.
While classic weather models calculate atmospheric development over hours or several days, nowcasting concentrates on the short-term movement and development of weather features that already exist.
On the interactive map you can follow how areas of precipitation have moved recently and where they are likely to move in the next few minutes.
In changeable autumn weather in particular, this information can be helpful, for example when planning drives, walks or other outdoor activities.
With wintry precipitation, the distinction between rain, sleet and snow matters as well. Type and intensity can change at short notice, however, which is why NowCast forecasts also carry uncertainties.
Clear weather contrasts within Europe
The current situation in Scandinavia stands in striking contrast to conditions on the Iberian Peninsula.While wintry precipitation is already occurring in parts of northern Europe, much of Spain is expecting a calm and pleasantly warm autumn day this Saturday.
In Andalusia, for example, highs of around 29°C are forecast in Seville, 27°C in Huelva and 26°C in Córdoba. On the Costa del Sol around 23°C can be expected.
The difference between conditions in southern Spain and the wintry areas of precipitation in Scandinavia is therefore considerable.
Such contrasts are not unusual in October. While the land masses of northern Europe cool down increasingly and outbreaks of cold air make wintry conditions possible, comparatively warm air masses can still hold on in the Mediterranean.
Autumn in Europe is thus showing its late-summer and its already wintry side at the same time.
Does the first snow mean winter has begun?
Individual snowfalls in October do not automatically mean that lasting wintry conditions have set in.In northern Scandinavia and at higher altitudes in particular, snowfall during autumn is a normal part of the seasonal transition.
Whether a closed snow cover forms and lasts for a longer time depends on temperatures at the ground, the amount of precipitation and how the weather develops further.
Even after the first wintry precipitation, milder air masses can reach Scandinavia again.
The current radar picture therefore documents a wintry spell first of all, not necessarily the start of a lasting snow cover.
Follow European precipitation almost in real time
The current situation can be followed on the interactive weather map from meteo365.es.RADAR + NowCast shows areas of precipitation across large parts of Europe and makes it possible to distinguish between rain, sleet, snow and hail.
Using the time bar, users can follow the development so far and look at the short-term forecast movement of the precipitation.
This makes visible not only where precipitation is occurring, but also how dynamically the weather is developing within Europe.Editorial note: this article is based on the radar display from Saturday morning, 10 October 2026. Radar-based precipitation classifications can differ from actual ground observations, especially in transition zones between rain and snow.
