As you know, we are heading towards an anticyclonic period. Weather conditions will improve and anticyclone will return to our regions. Or at least not far from us.
What is the reason for this change? Quite simply: the amplification of the polar vortex. A polar vortex that, to be fair, has never been weak until now. And then you ask yourself: How is it possible that the Arctic managed to penetrate the high-pressure plexus? Or rather, why did the anticyclone move north?
The answer lies in the complex dynamics that can be detected at different levels of the atmosphere. For example, it is not said that the higher stratosphere can constantly condition the lower troposphere. And that’s what’s been happening lately, that is, despite a freezing polar vortex, tropospheric conditioning has failed. For a whole host of reasons that warrant further investigation.
However, what matters is the result. Result that led to the Arctic slump but is now drifting in a different direction. high pressure indeed. Be careful though, as it was meant to be a temporary twist. On the other hand, we are approaching the latter part of winter, a period in which the polar vortex begins to age and, consequently, is subject to greater attacks from the troposphere.
This means that different winter dynamics could take place in Februarypresumably as a result of a weakening of the vortex itself. However, the dynamics are much coarser than the previous ones, a dynamic that, as we have been writing for some time, could lead to a major freeze wave.
In addition, the cold air will flow over Eastern Europe in the next few days. Cold air that will touch our regions and who knows that there will not be surprises right away.