In summer, we often hear about the so-called Azores High, which has now become almost proverbial: it is a high-pressure atmospheric area, where the weather remains substantially stable. It ensured summers such as those recorded in Italy up to about the 1980s, i.e. with a relative temperature range between day and night, not too maximum highs and temporary reductions in temperature due to thunderstorms that developed at the same local level.
As the name suggests, Azores High forms in the vicinity of the Azores islands, in the North Atlantic Ocean, where it has the maximum point of high pressure. Its position is determined by the atmospheric circulation, i.e. - simplifying - by how the exchanges of currents in the atmosphere are organised according to the winds.