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*Winter forecast 2021/2022* First look at Winter reveals a shift in the jet stream due to the new La Nina, felt in North America and in Europe

The Winter season 2021/2022 will be under the influence of a new La Nina phase, emerging in the tropical Pacific ocean. It will modify the jet stream pattern over North America and the Pacific Ocean, extending its reach to the rest of the world. The Winter forecast from major weather models captures this jet stream altering by the La Nina and shows its possible weather outcomes.

To try and understand the Winter season and its forecast, we must realize that there is no “magic bullet” when it comes to weather. Global weather is a very complex system, with many large-scale and small-scale climate drivers. We will look at what this La Nina is and how it can/will influence the Winter weather season of 2021/2022.

Below we have an example of a pressure pattern for a “perfect” winter scenario for both the United States and Europe. A blocking ridge over Greenland and North Pacific, with low pressure and colder air for the United States and Europe. This is what winter “fans” in Europe and the United States hope for every winter. But we will see if we can find anything similar in the early forecasts for Winter 2021/2022.



The development of a cold La Nina phase is the key feature in weather development for at least the next 6 months. This La Nina is actually just a different name for cold ocean temperatures in the tropical Pacific ocean. The actual ocean-atmosphere system is called ENSO.

To keep it simple, ENSO is short for “El Niño Southern Oscillation”. This is a region of ocean in the tropical Pacific, which alternates between cold and warm phases. The tropical trade winds (the easterly winds that circle the Earth near the equator) usually initiate or stop a certain phase, as they mix the ocean surface and alter the ocean currents.

The image below from NOAA Climate shows the typical circulation during a negative ENSO event. Air is descending in the eastern Pacific, creating stable and dry weather conditions, while rising air in the western Pacific causes frequent thunderstorms and a lot of rainfall.


ENSO has a major impact on the tropical convection patterns and thus on the ocean-atmosphere system, through which its influence is distributed globally. We usually observe a global scale shift in pressure patterns during the emergence of the ENSO phases, each having a unique impact on the weather globally.

Below we have an image that shows all the ENSO regions. The main regions are 3 and 4 and cover a large part of the tropical Pacific. Most calculations and diagnosis is based on a combination of both the 3 and 4 areas, which is why the main region is marked as 3.4.


Each ENSO phase has a different influence on the tropical weather and circulation and thus impacting the weather worldwide differently. A specific phase (warm/cold) usually develops around late summer and autumn and can last until next summer, or even up to two years in some cases.

The cold phase is called La Nina and the warm phase is called El Nino. Each ENSO phase is determined by the temperature anomalies (warmer/colder) in the ENSO 3.4 region in the tropical Pacific, as seen on the image above.

Looking at the 3.4 region, you can see on the image below how the ocean temperatures dropped in summer and autumn 2020. That was the development of the La Nina last year. We are now seeing a new cooling emerging, which is the start of a new cold phase.


On the image below you can see the global ocean temperature anomaly in mid-September. It reveals colder than normal surface waters in the tropical Pacific regions. This is a growing anomaly, where a new La Nina began emerging in July and is expected to continue to grow towards Winter 2021/2022.


Looking back at last September, the cold anomalies were actually stronger at this time of year, covering a wider area over the tropical Pacific Ocean. We had especially stronger negative anomalies in the eastern parts (region 3).


The best way to depict an emergence of a new cold ocean phase is with a high-resolution animation over time. The video below shows the cold ocean anomalies of the first La Nina from last year weakening over Spring. You can see new cooling starting in July. Notice the “waveforms” across the region, as the surface water is being pushed west by the trade winds.

The image below is an analysis and forecast image from multiple North American long-range models. It shows the La Nina from last year and the forecast for this winter season. It is clear from the forecast that the new cold phase is expected to peak just before the winter season, with its influence reaching into early spring 2022.


Below we have the ocean temperature forecast for late Fall and early Winter from multiple global seasonal models. it shows a developed La Nina across the equatorial Pacific Ocean. It is not as strong as last year, but has a strong presence in the ocean and also in the atmosphere, as we will see in the forecast part of the article below.



Usually, we can first see the influence of these ocean anomalies on the jet stream. The jet stream is a large and powerful stream of air (wind) at around 8-11km (5-7mi) altitude. It flows west-to-east around the entire Northern Hemisphere, affecting pressure systems, and their strength, shaping our weather at the surface.

Below is an example of the jet stream at 300mb (9km/5.6mi altitude). In this example, the jet stream is quite curved down over the central United States, which brings colder air down from the north. It is curved upwards over northern Europe. Such formation brings warmer weather to Scandinavia and stormy conditions to Iceland and the British Isles.


Historically, the most typical effect of a cold ENSO phase is a strong blocking high-pressure system in the North Pacific. The image below shows the average pattern during the last few cold ENSO winters. We can see the strong high-pressure system in the North Pacific and a low-pressure area over Canada and southwestern Europe.


The circulation of the strong high-pressure system promotes the development of a low-pressure region over Alaska and Canada. It curves the jet stream downwards in-between the two pressure systems.

You can see that in the image below. It shows the average position of the jet stream during La Nina winters and the corresponding weather patterns over North America. The curved jet stream brings colder air and storms down from the north into northern and the northwestern United States, and warmer and drier weather to the southern parts.


This way, the changing jet stream over the United States can actually divide the country into 2 weather poles. The images below show the temperature and precipitation analysis during the past La Nina winters over the United States.

In the northern part of the country, we see that the colder and wetter events are more frequent, as the jet stream directions the storm systems that way. But that can somewhat lockout the southern United States, creating warmer and quite drier conditions with less frequent storms and cold fronts.



Shifting the jet stream also means changing the snowfall potential. The colder air is more easily accessible to the northern United States, which also shows to have an increased snowfall potential. Especially areas like Alaska, Canada, and the northwest and the northern United States benefit from the jet stream to produce more snowfall. The graphic is by NOAA-Climate.


After passing Canada and the United States, the jet stream moves out into the Atlantic. There are different paths it can take. A lot depends on the overall circulation pattern and the existing pressure systems in the Atlantic. This is where La Nina perhaps loses its direct influence for Europe, as regional systems in the Atlantic take over.

But it usually still has an influence, as it changes the position of the entering jet stream from the west. The incoming jet stream can merge with the systems in the Atlantic, thus helping to create a whole new weather pattern for Europe. The problem is that the final outcome is far more unpredictable in the Euro-Atlantic zone than over North America, which feels a more direct influence.


We now know what La Nina is, and how it can change the jet stream and the weather. Now we will take a look at the global long-range models, and how they see the developing Winter 2021/2022.

We decided to focus on the 3 main (or most used) seasonal models. The ECMWF and UKMO from Europe, and the CFSv2 from the United States. Graphics are from the Copernicus Climate EU project and the CPC/NCEP.

All these forecasts are an average picture over the course of 3 meteorological winter months (December-January-February) and show the general prevailing weather patterns. Even if the models would be completely accurate, it does not mean that such weather conditions would last for 3 months straight. It only suggests how the weather patterns might look 40-60% of the time.


The ECMWF model is most often referred to as the most reliable model, at least in the long-range category. In reality, a lot depends on the individual situation and individual seasons. But generally, the ECMWF model is at the top of the chart as far as reliability goes. But no long-range/seasonal forecast can ever be deemed “reliable. We are only looking at trends and how the weather patterns might evolve over the entire continents or the planet.

In the pressure pattern forecast from ECMWF below, we can see the strong high-pressure system in the North Pacific, typical for a La Nina. The low-pressure system is developed over eastern Canada and the jet stream is bending in between the two pressure systems, just like we have seen in the previous segment.

We also see the North Atlantic in a positive NAO mode, which means an amplified jet stream over the British Isles and into Scandinavia. But this is not a typical positive NAO setup, as it is more west-oriented. It allows for winter situations over Europe. Most likely if the high-pressure system in the central Atlantic can crawl further up north, blocking the jet stream and creating a more northerly flow into Europe.


The airmass temperature forecast below shows North America divided into two parts. Western and central Canada is forecast to be colder than normal, with a high chance of the colder air extending towards the parts of the northern United States and over the Midwest and into the northeast. The Southern United States is forecast to be warmer than normal.

Europe also features higher than normal temperatures, but not to a high degree. Tho a more westerly flow dominant scenario is suggested, the pressure pattern does allow for a break in the flow. Occasional cold flow from northwest Europe is possible down into the mainland.


Looking closer at Europe, we see the surface temperatures are mostly above normal. Higher temperature anomalies and milder conditions are more likely towards the eastern regions. Central and western regions are likely to see occasional cold fronts from the northwest, hence the lower magnitude anomaly.


Over Noth America, the ECMWF forecast shows neutral/normal temperatures over much of Alaska, Canada, and most of the northern half of the United States. Warmer than normal temperatures are forecast for the southern regions. This is an early forecast, so the neutral temperatures will likely shift to colder, as the forecast consolidates.


Precipitation anomaly forecast shows a more normal La Nina type pattern over Canada and the United States. We see the mainland United States with wetter conditions in the northern parts under the jet stream and drier conditions in the south-central regions.

Europe is shown to have more precipitation over the northern regions, where most of the storms would follow. We still see wetter conditions in the Mediterranean. That would mean occasional breaks in the westerly flow and a low-pressure system over southern regions as a result.


We produced a special snowfall forecast from the ECMWF data, provided by the Copernicus-EU project. Over Europe, we see mostly less than normal snowfall. The exceptions are the northern United Kingdom and central Scandinavia. This shows an obvious storm track, due to the positive NAO pressure pattern. Increased snowfall is also suggested on the south Alpine slopes.


Over North America, we see a very interesting snowfall forecast. ECMWF suggests more snowfall than usual in most of the northern United States, especially in the northwest part. The increased snowfall potential continues over the Midwest and into the northeastern United States. We can also see a small extension of more snowfall down into the south-central regions.



Our second model of choice is the UKMO model, from the official United Kingdom Met-Office. This has also been a good performer in the past winters, so we tend to include it in our standard “suite” of model forecasts.

UKMO only has a slightly different pattern than the ECMWF, and quite honestly it seems just as likely at the current point in time. It shows the strong La Nina blocking high-pressure in the Pacific. But the main low-pressure area is centered further west over central Canada.


This causes a jet stream extension from North America upwards into Greenland. This means a more northwesterly flow is likely into Europe, as high pressure in the North Atlantic is bending the jet stream upwards into Greenland.

The temperature forecast also looks similar to the ECMWF. Over North America we have the cold pool over western Canada and Alaska, reaching down into the northern United States. The south-central and the eastern United States are forecast to be warmer than normal.

Europe now features a warmer winter, but not as much as the ECMWF. The UKMO also keeps the storm track over northern Europe.


Looking closer at Europe, we see the stronger warm anomalies focused over central and eastern Europe, similar to the ECMWF. The western half has more neutral to warm anomalies, indicating an increased potential for northerly flow and cold fronts into the region from the northwest.


Over North America, we see the double weather pole. Cold up north in Canada, and warmer down in the United States. The exception is the Midwest, which shows an extension of near-normal temperatures. That is likely the pathway for cold air spills down from Canada.


The precipitation forecast also nicely shows the “dipole” pattern over the United States, with drier in the south and wetter in the northern parts. Northern parts of the United States also have a higher chance of more snowfall, under the jet stream. Europe is again precipitation neutral, with hints of higher precipitation over northern parts, due to the higher frequency of storms moving over this area.



As a counterbalance to European models, we usually use the main North American long-range model, the CFS version 2 from the NOAA/NCEP in the United States.

The CFS model is closer to the ECMWF, with the strong high-pressure system in the Pacific and the Low-pressure system over eastern Canada and Greenland. This is the more typical La Nina situation we have mentioned before. The jet stream in the North Atlantic bends northeastward, over the British Isles and into Scandinavia. This is a common theme in all three models.


Airmass temperatures are most interesting over North America, with a strong cold air anomaly in Canada and warmer air in the southern United States. Europe is seen warm, as would be expected with storms moving far out in northern Europe.


Looking closer at Europe, the surface temperatures are really warmer than normal over much of the continent. The main exception is again the western half, as with the other two models. This happens because, despite the more northerly track of storm systems, we usually get some break-away storms and cold front when the jet stream pattern re-adjusts. Western Europe is the most likely region to be influenced by the colder from the north as storms go on a more southerly track.


The North American forecast is really a strong dipole pattern. Much colder than normal temperatures over Alaska and much of Canada, and warmth over the southern parts of the United States. The cold extends down into the northern United States, especially the Midwest.


We have to keep in mind that most of the weather dynamics happen between the cold and warm anomalies, including snowfall. CFS has no snow depth forecast graphic, but this pattern would likely look similar to the ECMWF snowfall forecast seen earlier above

The precipitation anomaly forecast below shows the main weather dynamics (with increased precipitation) over the northern United States and western Canada. This also includes likely more snowfall, as the cold source is readily available from the cold anomalies in Canada.

Europe is generally neutral when it comes to precipitation, with a hint for more precipitation over northern Europe, where the jet stream takes storm systems.



Reading images and descriptions can be somewhat confusing. So to summarize, here is what the Winter season 2021/2022 early forecast has to offer:

Europe is expected to have warmer than average temperatures over most of the continent, getting stronger towards the east. This, however, does not mean that there will be no cold fronts and colder days. It just implies that cold fronts and colder air mass intrusions will be less frequent over the region. Western Europe is likely to see more frequent colder air intrusions than eastern Europe.

But the models are not 100% in agreement with the pattern over the North Atlantic. It can be tricky at this stage before we have a clearly defined pattern over North America. The main change is the positioning of the low-pressure over Canada. Changing the low-pressure system position from east Canda to central or west can have a big impact on the Europe Winter weather

Normal to wetter conditions are expected over northern Europe. The British Isles and Scandinavia could have a more unsettled winter, as the jet stream positions over these regions, bringing behind more stormy weather. Mainland Europe is expected to have average precipitation, with above-average precipitation likely in southwestern Europe and the Mediterranean.

North America winter forecast looks fairly solid to be a classical La Nina type winter. Most of western and Central Canada is to expect colder and snowier conditions, along with Alaska.

The United States can expect to see a “two-faced” pattern or a “two-faced” winter. The Northern United States is expected to be normal-to-colder with wetter than normal winter. This increases the chance of more snowfall, but more likely towards the western half and in the Midwest, and less likely in the eastern parts.

The Southern United States has a high chance for warmer and mostly drier than normal winter weather. This however does not imply that no cold front can reach the southern states. It just implies that in a La Nina pattern, it is much less likely to get frequent cold fronts down to the very south.

Below we have the official temperature forecast for the United States by NOAA. It shows the temperature probability, with colder to equal chances in the northern United States. Most of the southern half of the country has a higher probability of warmer than normal weather, which we saw in the models above.


The official precipitation forecast is also quite similar to the models above. We see an equal-to-higher probability for more precipitation (and snowfall) in the northwestern and the northeastern United States. The Southern United States is mostly drier than normal.


The problem with a La Nina winter is usually the continuation of drought conditions in the south and southwest. Below we have a graphic from NOAA, which shows the current drought conditions in the United States. We see exceptional drought conditions over the western United States.


The northwestern United States is likely to recover to some degree during the winter, as we have seen on the precipitation forecasts. But the drought conditions in the southwest will continue, and likely even getting worse in a La Nina. The entire southwest and especially southern California is expected to have continued severe drought conditions through winter. Drought conditions are likely to be declared in the southern states as well over the winter, as La Nina is notorious for less precipitation in the southern states during the winter.



One of the more important sources of winter weather dynamics is of course the north polar stratosphere and the Polar Vortex. At the bottom of the page, you can find a link to our latest Polar Vortex and Stratosphere guide article. It contains info on what the stratospheric Polar Vortex is and how it can influence the weather and even override the La Nina influence.

Long-range forecasts are generally not as good at forecasting stratospheric dynamics in detail. This means they tend to underestimate any potential Sudden Stratospheric Warming events (SSW) since the final forecast is made out of many individual calculations, which have different ideas about the stratospheric development.

A stratospheric warming event can have a major impact on the circulation and can cause major pattern changes in the Northern Hemisphere. So a potential SSW event is an important factor that can change the course of winter in either way across the Northern Hemisphere.

We actually had a stratospheric warming event last winter, which changed the pressure patterns and helped to produce the strong cold outbreak in the southern United States in February 2021.

Below you can see strong positive values in the stratosphere in early January, associated with the higher pressure buildup during a stratospheric warming event. The event and/or its influence was slowly descending over time, reaching the surface levels by mid and late January. This persisted well into February, influencing the weather circulation and releasing colder air out of the Arctic (negative AO index on the bottom).


Below is an image that shows an average temperature pattern 0-30 days after a stratospheric warming event. High pressure over the Arctic helps to unlock the cold air out of the Arctic regions, sending it down into the mid-latitudes of the United States and Europe. Not every stratospheric warming event produces this pattern, but this is an average image of many events in the past 40 years.


You can read more about the developing polar vortex and the stratosphere for the upcoming winter, in our specialized article linked below:

Polar Vortex and Winter 2021/2022

We will release monthly updates, as fresh winter forecasts are produced by the models, so make sure to bookmark our page. Also, if you have seen this article in the Google App (Discover) feed, click the like button (♥) there to see more of our forecasts and our latest articles on weather and nature in general.
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