2000  years of North Atlantic-Arctic climate – Quaternary Science Review – Auger, Mayewski, Maasch, Schuenemann, Carleton, Birkel, Saros

Abstract The North Atlantic-Arctic boundary is highly variable due to the transports of heat and moisture through the Gulf Stream and polar jet stream. The North Atlantic storm track generally follows the Gulf Stream and terminates near southeast Greenland and Iceland as the Icelandic Low. The Icelandic Low is the main driver of the North read more 2000  years of North Atlantic-Arctic climate – Quaternary Science Review – Auger, Mayewski, Maasch, Schuenemann, Carleton, Birkel, Saros