This study documents the dynamics behind the first occurrence of a multi-year negative Indian Ocean Dipole since the 1960s, which lasted for an unprecedented 19 months, and co-occurred with the triple-dip La Niña event of 2020–2022. The co-occurrence of such extremes is rare and can exacerbate the associated climate risk. We find that Indian Ocean conditions limited the impact of La Niña on the Indian Summer Monsoon, preventing excessive monsoonal rainfall.

Atmospheric deserts are air masses from the boundary layer of desert regions. This study tracked them from North Africa to Europe during a two-year period (May 2022–April 2024). They can occur up to 60 % of the time, and can span large parts of Europe. They typically last about a day, and can alter the atmosphere throughout the free troposphere. On its way from Africa the air either rises and may become even warmer and drier, or it stays at mid-altitudes and cools, or retains its properties.

Hurricane Ophelia of October 2017 is a rare example of a strong post-tropical cyclone impacting Europe, an event that is expected to occur more frequently as our climate warms. This study examines the changes in structure, behaviour, and extratropical transition of Hurricane Ophelia under alternate climate forcing using a regional model. We find that in warmer climates the storm becomes stronger, larger, and maintains the characteristics of a tropical cyclone for longer than in cooler climates.