The term „Arktický vzduch,“ which translates to „Arctic air“ in English, refers to a mass of cold, polar air that originates from high-latitude regions, specifically the Arctic. In the context of meteorology and climatology, Arctic air is characterized by its low temperatures and significant impact on weather patterns in the mid-latitudes when it moves southward.
When Arctic air invades lower latitudes, it can lead to colder temperatures, frost, and even snow, particularly during winter months. The movement of Arctic air is influenced by atmospheric circulation patterns and the jet stream, which can occasionally shift and allow these cold air masses to penetrate into areas that typically have milder climates.
Understanding Arctic air is essential for weather forecasting and climate studies, as it significantly influences weather events, temperature fluctuations, and overall climate conditions across the globe, especially in regions close to the poles.
Bodavý chlad panuje nad Rochesterem v Minnesotě, s mrazivými poryvy větru -10 až -20 stupňů. Severní větry brání během klesání teplotě podstatně se zvýšit, zůstávají v jednociferných hodnotách. Počasí přinese…