Can North Atlantic Sea Ice Anomalies Account for Dansgaard–Oeschger Climate Signals?*
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The Norwegian Defence Research Establishment (FFI) has for decades been doing hydrographical surveillance in prioritized areas. In connection with this work, FFI has also
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The noise levels decreased with range into the ice cover; the reduction is fitted by a spreading loss model with a frequency-dependent attenuation factor less than for
In summary, observed hydrographic vari- ability in the subpolar North Atlantic and in the Atlantic inflow branches to the Nordic Seas leads cod stock variations in the Barents Sea
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• The sea-ice cover in the Nordic Seas can abruptly disappear for small changes in surface freshwater input or Atlantic water temperature (Paper I), or occur spon- taneously as a
This is one of the climate processes that determine the seasonal ice zone variability and long term change in the Nordic Sea region as the Nordic and Barents Seas are the main