‘Heat blob’ contributing to sea ice loss in Arctic

The video discusses the warming of the Arctic Ocean and the rapid disappearance of sea ice, attributed to increased heat transport by ocean currents since 2001. The Atlantic Meridional Overturning Circulation (AMOC) plays a key role in this process, carrying warm, salty water from the tropics to northern latitudes. This heat transport affects sea ice formation, with warm Atlantic water forming a heat blob in the Arctic. The phenomenon of Atlantification, where parts of the Arctic resemble the Atlantic, is also explored, highlighting the escape of warm water to the ocean surface, leading to reduced winter sea ice.

How does the increased transmission of heat to northern latitudes affect sea ice formation?

What phenomenon do scientists refer to when discussing the impact of warm, salty Atlantic water on the Arctic?