Azores High

In boreal summer, the Azores High is strongest. When the Azores High ridges toward the United States during its expanded summer phase, this creates a deep southwest flow of hot and humid tropical air toward the East Coast of the United States, and the central pressure can sometimes be located over Bermuda (hence why it is often referred to as the Bermuda High).

This high-pressure block exhibits anticyclonic behavior, circulating the air clockwise. Due to this direction of movement, African eastern waves are impelled along the southern periphery of the Azores High away from coastal West Africa towards the Caribbean, Central America, or the Bahamas, favoring tropical cyclogenesis, especially during the hurricane season.

The Azores High exhibits a direct influence on the North Atlantic Oscillation (NAO), and the index is commonly measured by comparing the sea level pressures in Ponta Delgada, Azores and near Reykjavík, Iceland.

Variations

Research into global warming suggests that it may be intensifying the Azores High in some years, independently of oscillations such as ENSO, leading to more precipitation extremes across the Southeastern United States as well as drier summers and milder winters across Western Europe. Latitudinal displacement of the ridge is also occurring, and computer models depict more westward expansion of the anticyclone in the future. However, during the winter of 2009–2010, the Azores High was smaller and weaker than usual, allowing sea surface temperatures in the Central Atlantic to increase quickly, as well as resulting in a cold winter across much of Europe.