Articles | Volume 7, issue 6 
            
                
                    
            
            
            
        https://doi.org/10.5194/os-7-821-2011
                    © Author(s) 2011. This work is distributed under the Creative Commons Attribution 3.0 License.
                Wind forcing of salinity anomalies in the Denmark Strait overflow
Related subject area
            Approach: In situ Observations | Depth range: All Depths | Geographical range: Nordic Seas | Phenomena: Temperature, Salinity and Density Fields
            
                    
                        
                            
                            
                            
                        
                    
            
        
        Cited articles
                        
                        Aagaard, K. and Carmack, E.: The Role of Sea Ice and Other Fresh Water in Arctic Circulation, J. Geophys. Res., 94, 14485–14498, 1989.
                    
                
                        
                        Coward, A. and de Cuevas, B.: The OCCAM 66 Level Model: physics, initial conditions and external forcing, SOC Internal Report No. 99, National Oceanography Centre, Southampton, UK, 2005.
                    
                
                        
                        Curry, R., Dickson, B., and Yashayaev, I.: A change in the freshwater balance of the Atlantic Ocean over the past four decades, Nature, 426, 826–829, 2003.
                    
                
                        
                        Dickson, R. R. and Brown, J.: The production of North Atlantic Deep Water: Sources, rates and pathways, J. Geophys. Res., 99, 12319–12341, 1994.
                    
                
                        
                        Dickson R. R., Yashayaev, I., Meincke, J., Turrell, W. R., Dye, S. R., and Holfort, J.: Rapid Freshening of the Deep North Atlantic over the past Four Decades, Nature, 416, 832–837, 2002.
                    
                 
 
             
             
             
            