The Link between the North Atlantic Oscillation and Arctic Sea Ice Export through Fram Strait
- 1 October 2001
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 14 (19) , 3932-3943
- https://doi.org/10.1175/1520-0442(2001)014<3932:tlbtna>2.0.co;2
Abstract
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. From the results of this study there is less indication that a significant link on interannual and decadal timescales between the NAO and the sea ice export through Fram Strait is a characteristic property of the climate system—at least under present-day climate conditions. This missing link can be explained by a vanishing net impact of the NAO on sea ice thickness as well as sea ice drift near Fram St... Abstract 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. From the results of this study there is less indication that a significant link on interannual and decadal timescales between the NAO and the sea ice export through Fram Strait is a characteristic property of the climate system—at least under present-day climate conditions. This missing link can be explained by a vanishing net impact of the NAO on sea ice thickness as well as sea ice drift near Fram St...Keywords
This publication has 35 references indexed in Scilit:
- The Role of Ocean Dynamics for Low-Frequency Fluctuations of the NAO in a Coupled Ocean–Atmosphere GCMJournal of Climate, 2000
- Simulation of the interannual variability of the wind-driven Arctic sea-ice cover during 1958–1998Climate Dynamics, 2000
- Arctic Sea Ice Variability in the Context of Recent Atmospheric Circulation TrendsJournal of Climate, 2000
- Signature of recent climate change in frequencies of natural atmospheric circulation regimesNature, 1999
- ENSO dynamics and seasonal cycle in the tropical Pacific as simulated by the ECHAM4/OPYC3 coupled general circulation modelClimate Dynamics, 1998
- Contour mapping of Arctic basin ice draft and roughness parametersJournal of Geophysical Research: Oceans, 1992
- Latent and Sensible Heat Flux Anomalies over the Northern Oceans: The Connection to Monthly Atmospheric CirculationJournal of Climate, 1992
- The role of sea ice and other fresh water in the Arctic circulationJournal of Geophysical Research: Oceans, 1989
- An estimate of the mean field of Arctic sea ice motionJournal of Geophysical Research: Oceans, 1984
- Die Schwankungen der atmosphärischen Zirkulation über dem Nordatlantischen Ozean im 25-jährigen Zeitraum 1881-1905Geografiska Annaler, 1924