O_Skagseth-T_Furevik-R_Ingvaldsen-H_Loeng-KA_Mork-KA_Orvik-V_Ozhigin.pdf (1.554Mb)

However, in areas where the Atlantic water submerges the lighter Arctic water, as west and south of the Great Bank, one must expect different current areetion

proc~sses, and equally important is i t to try to understand the mechanisms causing the climatic variations. Climat in the Barents Sea. l) The climatic

North Atlantic marine ecosystems are exposed to the forcing of several climatic phe- nomena, such as the North Atlantic Oscillation (NAO), the Atlantic Multidecadal Os- cillation

Updating large-scale estimates of krill biomass and distribu- tion of krill in the Southwest Atlantic sector has the potential to guide the establishment of a future time

• To first order, the large scale ocean circulation response to an increase in the Arc- tic river runoff – slowdown of the Atlantic Meridional Overturning Circulation and the

The influence of the interannual variability of AASIC decline on the stratosphere–troposphere coupling during different phases of the AMO is analyzed. When the AASIC loss

Further investigation suggests that the enhanced synoptic eddy and low-frequency flow SELF interaction over the North Atlantic in February and March during the AMV1, caused by

During the positive phase of the Atlantic Multidecadal Oscillation (AMO) since the 1990s, the anomalously warm North Atlantic triggers a series of zonally symmetric and