This week is seeing very mild and settled conditions over most of the continent due to a strong high pressure set over central Europe.
If we look at the daily maximum temperatures (Figure1), we can see that mostly everywhere (except few areas in N Scandinavia and Russia) positive values are observed, with temperatures above 10 °C from the UK to the Balkans. Peaks above 15 °C are observed in France, Spain, Italy and SE Europe, with 20 °C reached in Spain.
Looking at the satellite image (Figure2) the weather patterns over Europe are still the same of last week: clear sky (except some local fog) due to the strong high pressure over central-southern Europe, fronts moving quickly along the edge of the ridge between the UK and the N Atlantic and a low between Scandinavia and Russia causing snow in some places.
Unfortunately the synoptic condition won’t change later this week, with the ridge on W Europe moving north towards Scandinavia and pushing mild air from N Africa and the mid-Atlantic.
Only from the weekend, cold air from Russia will move SE towards the E Mediterranean leading to a drop in temperatures and snow at sea level between E Europe and the Balkans, but elsewhere it will be still mild and sunny.
It’s likely that February will end with dry and mild conditions in many areas, and it will be interesting to see the temperatures anomalies observed overall in this month over the continent.
Regardless of the ‘significance’ of the anomaly, February 2019 won’t certainly be remembered as a cold month in many areas.
This week a strong high pressure system has set over central western Europe, causing sunny days and mild temperatures. Today, maximum values are far above the average mostly everywhere in Europe, with temperatures reaching 20 °C in the Iberian peninsula (Figure1).
Temperatures between 10/15 °C are observed in all the Mediterranean region, France, the UK and Germany. Moving eastward values are lower but still above the average of February. Only in Russia and north Scandinavia temperatures are below 0 °C.
The weather today (Figure2) has seen bright skies over all W Europe and central Mediterranean region, with only some local fog at the lowest levels (mainly in the morning). At the edges of the high-pressure ridge, clouds and band of rain are observed in the north Atlantic and E Mediterranean, instead over N Russia and Finland snowfall is occurring.
This weather condition won’t change during the next weekend, with still dry and mild conditions in central/southern Europe. Colder air will reach tomorrow the E Mediterranean, though without ‘freezing’ temperatures. From Sunday, colder and moister air from the N Atlantic will try to push the anticyclone eastward, causing unsettled and ‘colder’ weather over the UK, France and Spain. We will see next week if there is going to be a change in the weather patterns, though it seems likely that the high pressure will be still steady for the next few days.
In this article I am going to analyse the temperatures observed in some cities in Europe during January 2019. A former analysis made two weeks ago had shown that the first two weeks of the year have been cold (and snowy) in Southern and Eastern Europe, with observed temperatures lower than in NW Europe.
Now that January has passed, we can see if the trend observed at the beginning of the month has occurred also throughout the last two weeks or if it has changed.
In Figure1 I have plotted the average daily temperatures observed in 17 cities in Europe.
We can see that E Europe and N Europe have observed the lowest average temperatures (Moscow is the coldest: -7 °C). Moving westward and southward temperatures rise, with positive values mostly everywhere (except in the Balkans: Bucharest -1 °C). The warmest cities have been Lisbon, Athens and Instanbul.
Regarding the anomalies of the average temperatures compared with the long-term average (1981-2010), in Figure2 I have plotted the results, in order to determine where it has been colder than the average and where it hasn’t.
We can see how the most significant anomalies (in absolute values) have been observed in Scandinavia (colder temperatures) and E Mediterranean (warmer temperatures). Warmer than the average also in Germany, Iceland and Ireland (though the anomalies are mostly between +0.2/+1 °C). In southern Europe little negative anomalies are observed.
This ‘picture’ is different than what seen two weeks ago, when significant negative anomalies were observed in SE Europe and ‘warm’ conditions were observed in the north (especially in Iceland, UK and Germany).
In conclusion, January has been ‘mild’ in some places (i.e. in central/western Europe, Iceland and SE Europe) and cold (compared with the average) in Scandinavia and Mediterranean region, though in both cases, the anomalies have’t been too significant.
During the last two weeks wintry conditions have occurred in numerous countries, both in W Europe and E Europe. Very cold temperatures were observed in Scandinavia and Russia and snow has fallen in many areas between central Europe, the UK and the Mediterranean region.
However, these weather conditions are changing, with milder air coming from mid-Atlantic and N Africa. Indeed, already today higher temperatures are observed (Figure1) with values above 10 °C in many areas in S Europe (especially S Spain, Italy and E Mediterranean region) and above 0 °C mostly everywhere, except in the Alpine region, Scandinavia and N Russia.
The satellite imagery (Figure2) shows the main features of the weather conditions over the continent.
A high-pressure is setting on W and Central Europe, with bright conditions in Spain, S France and central/N Italy and fog/low clouds between Germany and Poland. Between France, the UK and the N Sea a (weak) low pressure system is causing showers across England and Benelux.
Moving eastward, warm air from N Africa is causing settled and mild conditions in the E Mediterranean and convection is occurring between S Italy and Greece. This is due to a (weak) low-pressure system positioned close to Sicily which is leading to a temperature contrast between the (relatively) cold air from central Europe and the mild air from N Africa. Thus, convective cells are forming on the sea, causing numerous thunderstorms in the area.
Finally, in E Europe and Scandinavia cold temperatures are still observed, with snowfall between Finland and Russia.
The weather conditions for this week will see an increase in the strenght of the high-pressure in central/southern Europe with settled conditions and relatively mild temperatures (though fog/low clouds are possible in the valleys limiting the increase in temperatures). In fact, from Tuesday possible peaks of 20 °C are expected in S Spain, Portugal, S Turkey and Cyprus. Temperatures between 10/15 °C are expected in S France, Italy and the Balkans and close to 10 °C in the UK and Central Europe. In addition, during the night temperatures will be close or slightly below 0 °C especially in the valleys (and in case of clear sky),causing a strong temperature gradient between day and night.
Only in E Europe and Scandinavia it will be still cold, though with values above the average.
On Thursday, colder air from N Atlantic should cause a slight decrease in temperatures (with frequent showers) in Central Europe, though with no snow or ‘freezing’ conditions. However, only from next week (so in 7 days) a more significant change in the weather conditions should be observed, though it is still too early to talk about its possible effects.
During the weekend and today temperatures have dropped in central Europe and northern Europe, with ‘freezing’ conditions in some areas.
The minimum temperatures observed this morning (Figure1) are well below 0 °C mostly everywhere in central and northern Europe, with values between -5/-10 °C especially in Germany, Alpine region and Czech republic; in some areas (central Germany and in the Alps) values between -10/-15 °C are observed.
Moving north towards Scandinavia, temperatures are well below -20 °C, with peaks of -30/-35 °C especially between Sweden and Finland.
Cold conditions are also occurring in Russia and E Europe, instead moving towards the Mediterranean region and the Atlantic coast temperatures tend to increase, with values above 0 °C mostly everywhere. The warmest conditions are observed in S Greece, Cyprus and S Spain, with minimum temperatures between 10/15 °C in some areas.
The afternoon has seen still very cold temperatures in central/northern Europe, with numerous cities observing maximum temperatures below 0 °C (Figure2), instead moving southward and westward temperatures have been milder, with values above 10 °C especially in Portugal, S Spain and E Mediterranean.
The low temperatures observed in central Europe are due to the combination of the cold air, moved southward last week, with a high-pressure system (Figure3) settled on central Europe since this past weekend. Thus, the cold air is ‘trapped’ at surface causing temperature inversion (temperatures in the free atmosphere around 1500 m a.s.l are ‘warmer’ than at surface) and fog/low clouds.
Looking on the Atlantic, a low pressure system is moving towards the UK, leading Polar maritime air to move south-eastward (notice the scattered clouds).
Scandinavia and Russia are reached by very cold air coming from Siberia, which is moving southward towards central Russia (see the cold front, band of clouds, from Sweden to central Russia).
Finally, in the Mediterranean region settled conditions occur on the Iberian peninsula (positioned on the warmer side of the anticylone); in Italy a weak low-pressure system is causing overcast conditions and rainfall especially along the peninsula and finally, in the E Mediterranean, showers are occurring mainly in Turkey.
The next days will see colder air towards the UK and W Europe, with showers and snow at low levels especially between tomorrow and Thursday, with the high-pressure moving eastward towards Russia.
The cold air will move towards the central Mediterranean region, causing the development of a deep low pressure system between Spain and Italy which will bring rain, strong winds and snow (at low-medium levels) along the Italian peninsula and in N Spain; some snow should fall also in the Po valley and Alpine region.
Later in the week, the low pressure system will move towards Greece and the Balkans causing unsettled weather.
In Central and N Europe instead, the weather will be nice (but still cold), with some snow showers especially mainly between central Sweden and Finland.
In conclusion, it will be a very interesting week, because of the presence of different air masses on the continent and possibility of snow at low levels in numerous areas.
If we look at the satellite imagery of today (Figure1) we can see different weather conditions across the continent.
Between the UK and Scandinavia we can see the cold air coming from the Arctic, visible for the scattered cumulus clouds on the N Sea caused by instability (ocean surface is warmer than the air mass, thus the warm air lifts up in the atmosphere and condenses forming clouds and precipitation); these are causing scattered showers (mainly snow) in Scotland and E England, as well as a decrease in temperatures in the UK, Norway and N France.
On the west (in N Atlantic) a deep low-pressure system (989 hPa) is moving towards Ireland, though it will weaken before reaching the coast (between tomorrow and Saturday), so no severe event is expected.
On the southern part of this cyclone, less clouds and calm conditions are due to a high-pressure west of Spain, which is leading to a warm air advection from mid-Atlantic towards the Iberian peninsula (maximum values of +14/+17 °C today between Portugal and S Spain).
Instead, from E Spain to the Baltic region, a long and narrow tail of clouds stands for a cold front moving southeastward (causing rainfall and snow between France, N Italy and the Alpine region ); this is simply the front of the arctic air mass which is ‘pushing’ towards central-southern Europe.
Moving eastward, we can see how between S Italy, the Balkans and Turkey the weather conditions are ‘calm’, with clear skies (notice the snow at the ground between Greece, Serbia and Romania). Here, a high-pressure is causing settled (and relatively) mild conditions (maximum temperatures between +12/+15 °C in S Greece and Turkish coast).
On the northern side of the anticyclone, we can see another band of clouds (between Ukraine and Russia) which is related to a warm front moving eastward and causing snow at ground level (due to the negative temperatures at surface).
The warm front in E Europe and the cold front in central Europe are related to a deep low-pressure system (976 hPa) positioned between the Baltic sea and S Finland. This is causing intense snowfall in the area and quite strong winds on the Baltic sea, and it is leading to very cold air from NE Russia towards central Scandinavia, where temperatures close or below -30 °C are observed.
Thus, today has been fascinating on a meteorological point of view, and also the next days will be interesting due to the fast change in the weather conditions over Europe.
The first two weeks of January have seen very cold air coming from Russia towards Central-Eastern Europe, with lot of snow especially in S. Germany, Austria (more than 2 metres in the Alpine region) and the Balkans. Also in Greece and S. italy snow has fallen, at sea levels at times.
In northwestern Europe instead, and especially between France, the UK and the N. Atlantic, a strong high-pressure ridge has caused settled conditions for several consecutive days, causing also very warm air towards these areas and Scandinavia.
I have analysed and plotted the daily average temperatures in 17 countries (cities) and compared the results. This analysis is simply focused on considering the main cities, thus it is not a detailed analysis for each country.
The results (Figure1) show that in S. Europe (especially between Italy and the Balkans) the daily average temperatures have been lower than in central-northern Europe.
We can see how Rome and Istanbul observed similar or lower temperatures than London, Paris and Amsterdam (to cite a few). In addition, it is impressive to see that Reykjavik has observed a very similar mean temperature to the cities in southern Europe.
Also the Balkans have observed temperatures lower than in northern Europe, with Bucharest colder than Stockholm and observing temperatures very similar to Helsinki.
However, not all southern Europe has observed low temperatures; the Iberian pensinsula has seen warmer conditions (though with temperatures close to their climatological average), with Lisbon the warmest capital so far. This is due to the frequent flow of warm air coming from the Tropics caused by the high-pressure ridge set (since December) between W Europe and the Atlantic.
In E. Europe (Warsaw, Moscow) the lowest temperatures have been observed (which is also in accordance to their climate); these areas where directly influenced by the polar continental air coming from E/NE Russia throughout the whole period.
If we look at the daily temperature anomaly (Figure2) computed respect to the climatological average (1981-2010), we can see how Reykjavik has observed the highest values (almost +5 °C; the daily mean average temperature in January for the Icelandic city is 0 °C).
Overall, all the area from France to Scandinavia and Iceland has seen warmer temperatures, instead E Europe and S/SE Europe have experienced a colder weather.
In conclusion, we can say that the new year has brought cold weather in the southern and eastern part of the continent (with snow in numerous and unusual areas); instead, the western and nothern areas (especially the countries along the N Atlantic coast) are still experiencing mild conditions (as occurred also in December).