A possible mechanism for the strong weakening of the North Atlantic subpolar gyre in the mid‐1990s
A possible mechanism for the strong weakening of the North Atlantic subpolar gyre in the mid‐1990s
复制标题
20世纪90年代中期北大西洋副极地环流强烈减弱的可能机制
DOI:
10.1029/2009gl039166
复制
发表时间:
2009
影响因子:
5.2
通讯作者:
M. Bentsen
中科院分区:
文献类型:
--
作者:
K. Lohmann;H. Drange;M. Bentsen
The extent and strength of the North Atlantic subpolar gyre (SPG) changed rapidly in the mid‐1990s, going from large and strong in 1995 to substantially weakened in the following years. The abrupt change in the intensity of the SPG is commonly linked to the reversal of the North Atlantic Oscillation (NAO) index, changing from strong positive to negative values, in the winter 1995/96. In this study we investigate the impact of the initial SPG state on the subsequent behavior of the SPG by means of an ocean general circulation model driven by NCEP‐NCAR reanalysis fields. Our sensitivity integrations suggest that the weakening of the SPG cannot be explained by the change in the atmospheric forcing alone. Rather, for the time period around 1995, the SPG was about to weaken, irrespective of the actual atmospheric forcing, due to the ocean state governed by the persistently strong positive NAO during the preceding seven years (1989–1995). Our analysis indicates that it was this preconditioning of the ocean, in combination with the sudden drop in the NAO in 1995/96, that lead to the strong and rapid weakening of the SPG in the second half of the 1990s. This hypothesis explains the diverging evolution of the strength of the SPG and the atmospheric forcing (winter NAO) after 1995, as has been suggested recently.