The loss of Arctic sea ice may cause the ocean currents to slow down, which could lead to warmer waters near the Western European Coast. This could cause an increase in air temperatures and more extreme weather events in the region.
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The loss of Arctic sea ice decreases the temperature gradient between the Arctic and lower latitudes, which can weaken the ocean currents such as the Gulf Stream, potentially leading to alterations in the climate near the Western European Coast, including a decrease in mild winters and an increase in severe weather events.
