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[ 1 ] A new climate simulation for the middle Pliocene (ca. 3 Ma BP) is performed by a global grid-point atmospheric general circulation model developed at the Institute of

Situated near the seasonal sea-ice margin and the interface of Arctic (East Greenland Current; EGC) and Atlantic (Irminger Current; IC) waters (Fig. 1), observations

[ 1 ] A new climate simulation for the middle Pliocene (ca. 3 Ma BP) is performed by a global grid-point atmospheric general circulation model developed at the Institute of