How my work benefits society
Atlantic Meridional Overturning Circulation (AMOC) is an important component of the Earth’s climate system that is characterized by a northward flow of warm, salty water in the upper Atlantic, and a southward flow of cold water in the deeper layers of the Atlantic ocean. AMOC is responsible for distributing heat from the lower latitudes to the higher latitudes. Scientific evidence shows that AMOC is likely to “slow-down” in the next 50-100 years. My research focuses on studying the atmospheric response to the slowing down of AMOC, particularly over Europe.