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In recent weeks, the UK and much of Western Europe have been experiencing a prolonged spell of rainy and overcast weather due to stagnant low-pressure systems. These systems have been unable to move eastward as usual because a large high-pressure area has become entrenched over Scandinavia. This high-pressure zone acts as a barrier, effectively blocking the typical progression of weather fronts across the region.
This meteorological setup is known as a “blocked” pattern, a phenomenon that, while not uncommon, has had significant effects on the UK’s weather this year. The impact of such blocking situations varies depending on the exact location of the high-pressure system. Its position can dramatically influence the local weather conditions experienced across different parts of Europe.
For instance, when the area of high pressure is established directly over the UK, it prevents moist, rain-bearing weather systems from reaching the region. This scenario often results in extended dry periods. During summer months, this can contribute to heatwaves and potentially bring about drought conditions. In contrast, during the winter, the same pattern typically leads to dry, sunny, and chilly weather.
Even minor shifts in the location of the blocking high-pressure system can cause markedly different outcomes. If positioned just north of the UK during winter, it can funnel frigid air from northeastern Europe into the country. Such conditions may resemble those seen during the “Beast from the East” event in 2018, characterized by bitterly cold weather across large parts of the UK
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