2029–30 Azores High Anticyclosis Event

The 2029–30 Azores High Anticyclosis was a weather event that significantly impacted weather patterns in the Northern Atlantic. The high-pressure system over the Azores dramatically lost strength in April 2029. This was due to consistent troughing and low-pressure systems that plagued it. By July that same year, when the weather system is usually at peak strength, it instead had a mean atmospheric pressure of 1019.8 millibars. This drastically changed the outcome for tracks of tropical cyclones that year; the storms that developed in the Main Development Region (MDR) had weaker steering currents and began to recurve out to sea without impacting many land areas. This, however, did not affect the storms out of the common areas of influence, which would include tropical cyclones that would form in the Gulf of Mexico or the Caribbean. Later that year, the weather system regained some strength as the troughing lessened around it. Eventually, by July 2030, it was back to its normal state and had no abnormal impacts on the hurricane season.