The global retreat of glaciers and rising sea levels are well-established consequences of climate change. However, recent observations suggest a deceleration in glacier re- treat in regions such as Iceland and Scandinavia, amidst escalating levels of forcing and greenhouse gas emissions. The North Atlantic Basin, with its unique character- istics, plays a crucial role in redistributing heat content and influencing local climatic dynamics. While studies have investigated the significance of North Atlantic surface features like the North Atlantic Oscillation and Atlantic Multidecadal Oscillation on the cryosphere, the role of oceanic circulations remains relatively underexplored. This study focuses on the Atlantic Meridional Overturning Circulation (AMOC ), linking it to the formation of a region of reduced oceanic warming (as respect to the rest of the world) to the south of Greenland, which influences atmospheric circulation and local climate dynamics. We explore the impact of AMOC trends on regional glacier dynamics using an ensemble of Coupled Model Intercomparison Project Phase 6 (CMIP6 ) models. Our findings reveal significant correlations be- tween AMOC and air temperature as well as precipitation over regions including Iceland, Scandinavia, and southern Greenland, suggesting a crucial role of AMOC in regulating regional climate and glacier mass balance. This is confirmed by OGGM runs forced by the CMIP6 ensemble demonstrating significant negative correlations between AMOC decline and glacier volume, particularly in Iceland and Scandinavia. Southern Greenland also exhibits a response to AMOC decline, albeit not as spa- tially extensive despite its proximity to the warming hole. In contrast, Svalbard does not demonstrate significant correlation, with studies suggesting that it is more strongly influenced by the NAO and by the Arctic Amplification. Our study high- lights the importance of understanding AMOC evolution to improve predictions of future glacier change in the North Atlantic region.