The loss of Arctic sea ice can disrupt the ocean currents and climate near the Western European coast by potentially weakening the North Atlantic Drift, an extension of the Gulf Stream, and leading to colder temperatures and altered weather patterns in the region.
The loss of Arctic sea ice can lead to changes in ocean currents, specifically the weakening of the North Atlantic Current, which can disrupt the flow of warm water towards the Western European coast and potentially result in colder temperatures and altered climate patterns in the region.
