Sorteberg A, N. G. Kvamstø and Ø. Byrkjedal (2005) Wintertime Nordic Seas Cyclone Variability and its Impact on Oceanic Volume Transports Into the Nordic Seas.

There were three water masses from (Rudels et al., 2012) I could not identify in neither the data or in the climatologies: Canadian Basin Deep Water (CBDW), Eurasian Basin Deep

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

• In contrast, models with a positive correlation be- tween the heat transport into the Nordic Seas and the Subpolar Gyre Index have a weaker heat trans- port than expected from

a) assess the potential impact of the radioactive contamination of the Nordic Seas arising from possible sources off northern Norway and Russia. b) assess progress

In this section, we assess to what extent the observed variability on seasonal to interannual time scales of the North Atlantic–Nordic seas exchanges (Fig. 2) can be related to local

Comparing the historical period with the two future scenario periods, there is a statistically significant reduction of polar low fre- quency in the Nordic Seas in October–January,

Paper two presents a new benthic foraminifera Mg/Ca record for the Faroe-Shetland Channel, spanning a key interval of Dansgaard-Oeschger cycles (40-30 ka b2k) (Figure 13 h).

An extensive collection of hydrographic measurements from the Nordic Seas 32 confirms the persistent presence of anomalously dense water on the upper slope north of Iceland and