The loss of Arctic sea ice may cause a decrease in the strength of the Atlantic Meridional Overturning Circulation, which is a major ocean current that brings warm water to the western European coast. This could lead to a decrease in the amount of warm water reaching the coast, resulting in a cooler climate in the region.
The loss of Arctic sea ice can disrupt ocean currents and climate near the western European coast by weakening the North Atlantic Drift, a warm current that brings heat from the tropics to the region, potentially leading to colder temperatures and altered weather patterns.
The loss of Arctic sea ice can disrupt the normal circulation patterns of the Atlantic Ocean, leading to a weakening of the North Atlantic Current and the potential for colder climate in Western Europe due to a reduced supply of warm waters from the Gulf Stream.
