Key points are not available for this paper at this time.
Recently, Hilmer and Jung have shown that the wintertime link between the North Atlantic oscillation (NAO) and the sea ice export through Fram Strait changed from zero correlation (1958-77) to about 0.7 (1978-97) during the last four decades. In the current study, the authors focus on the question of how the two phenomena are linked in a long-term context during wintertime (December-March). This is done on a statistical basis using data from a century-scale control integration of the coupled general circulation model ECHAM4-OPYC3 along with historical sea level pressure data for the period 1908-97.
Jung et al. (Mon,) studied this question.