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During the Atlantic Meridional Overturning Circulation (AMOC) period of change (1870-2016), the Arctic has lost most of its sea ice, with an acceleration during the last decade. The loss of sea ice affects the water masses in the Arctic Ocean (AO), and this could impact the AMOC. Here, we suggest the build-up and potential impact of sea ice loss on the salinity, oxygen and stratification of the AO. The AO is an important boundary between the Atlantic Ocean and the Northern Hemisphere Ocean, and also a barrier between the Northern Hemisphere North Atlantic Current and North Atlantic Deep Water. The AO has a northward-flowing middle layer that transports heat and nutrients from the Atlantic Ocean to the Arctic Ocean. The composition of the middle layer changes with increasing salinity from the Atlantic Ocean to the Arctic Ocean, and temperature-driven salinity changes within the middle layer of the AO can affect the density and transport of water masses through it. The loss of sea ice in the Arctic Ocean will be larger on the Atlantic side than the Pacific side, and the density and salinity of the AO middle layer will change in opposite ways to the loss of sea ice on the Atlantic side of the AO. Based on changes in AO water masses during the last century, the change in the Atlantic side of the AO in the last decade (with an accelerating trend) implies that the Arctic Ocean stratification could