This is an excellent description of how Autumn changes the patterns we’ve become so used to over the summer months, and how it manifests itself. As the Northern Hemisphere moves from summer into autumn, the North Atlantic atmosphere begins a seasonal reorganisation. Faster cooling at high latitudes strengthens the temperature contrast between polar and subtropical air, influencing the jet stream and creating a more favourable environment for mid-latitude weather systems. The transition is visible at the surface through shorter days, cooler nights and the first incursions of colder air, but some of the most important changes occur several kilometres above the ground. Across the North Atlantic, the large-scale circulation gradually shifts towards a more energetic cool-season pattern, with the jet stream exerting greater influence on the low-pressure systems, fronts and changing air masses that shape European autumn weather. This does not mean that storms begin on a particular date, nor does every autumn follow the same progression. Strong Atlantic activity can alternate with blocking highs and settled periods, yet the background environment generally becomes more favourable for active mid-latitude weather as the temperature difference between northern and southern latitudes grows. More …