Evaluating two numerical advection schemes in HYCOM for eddy-resolving modelling of the Agulhas Current

被引:22
作者
Backeberg, B. C. [1 ]
Bertino, L.
Johannessen, J. A. [2 ]
机构
[1] Univ Cape Town, Dept Oceanog, ZA-7700 Rondebosch, South Africa
[2] Univ Bergen, Inst Geophys, N-5020 Bergen, Norway
基金
新加坡国家研究基金会;
关键词
SEA-SURFACE TEMPERATURE; IN-SITU; OCEAN; VARIABILITY; CIRCULATION; ORDER; FLOW;
D O I
10.5194/os-5-173-2009
中图分类号
P4 [大气科学(气象学)];
学科分类号
070601 [气象学];
摘要
A 4th order advection scheme is applied in a nested eddy-resolving Hybrid Coordinate Ocean Model (HYCOM) of the greater Agulhas Current system for the purpose of testing advanced numerics as a means for improving the model simulation for eventual operational implementation. Model validation techniques comparing sea surface height variations, sea level skewness and variogram analyses to satellite altimetry measurements quantify that generally the 4th order advection scheme improves the realism of the model simulation. The most striking improvement over the standard 2nd order momentum advection scheme, is that the southern Agulhas Current is simulated as a well-defined meandering current, rather than a train of successive eddies. A better vertical structure and stronger poleward transports in the Agulhas Current core contribute toward a better southwestward penetration of the current, and its temperature field, implying a stronger Indo-Atlantic inter-ocean exchange. It is found that the transport, and hence this exchange, is sensitive to the occurrences of mesoscale features originating upstream in the Mozambique Channel and southern East Madagascar Current, and that the improved HYCOM simulation is well suited for further studies of these inter-actions.
引用
收藏
页码:173 / 190
页数:18
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