Propagation of Meridional Circulation Anomalies along Western and Eastern Boundaries
Propagation of Meridional Circulation Anomalies along Western and Eastern Boundaries
复制标题
经向环流异常沿西部和东部边界的传播
DOI:
10.1175/jpo-d-13-0134.1
复制
发表时间:
2013
影响因子:
3.5
通讯作者:
Marshall D
中科院分区:
文献类型:
--
作者:
Marshall D
Motivated by the adjustment of the meridional overturning circulation to localized forcing, solutions are presented from a reduced-gravity model for the propagation of waves along western and eastern boundaries. For wave periods exceeding a few months, Kelvin waves play no role. Instead, propagation occurs through short and long Rossby waves at the western and eastern boundaries, respectively: these Rossby waves propagate zonally, as predicted by classical theory, and cyclonically along the basin boundaries to satisfy the no-normal flow boundary condition. The along-boundary propagation speed iscLd/δ, wherecis the internal gravity/Kelvin wave speed,Ldis the Rossby deformation radius, andδis the appropriate frictional boundary layer width. This result holds across a wide range of parameter regimes, with either linear friction or lateral viscosity and a no-slip boundary condition. For parameters typical of contemporary ocean climate models, the propagation speed is coincidentally close to the Kelvin wave speed. In the limit of weak dissipation, the western boundary wave dissipates virtually all of its energy as it propagates toward the equator, independent of the dissipation coefficient. In contrast, virtually no energy is dissipated in the eastern boundary wave. The importance of background mean flows is also discussed.
影响因子:
5.2
作者:
D. Marshall;B. Vogel;Xiaoming Zhai
通讯作者:
D. Marshall;B. Vogel;Xiaoming Zhai