Mozambique Channel Eddies in GCMs: A question of resolution and slippage
Quartly, G.D.; de Cuevas, B.A.; Coward, A.C. ORCID: https://orcid.org/0000-0002-9111-7700. 2013 Mozambique Channel Eddies in GCMs: A question of resolution and slippage. Ocean Modelling, 63. 56-67. 10.1016/j.ocemod.2012.12.011
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Abstract/Summary
Hydrographic observations in the 21st century have shown that the flow within the Mozambique Channel is best described by a series of large poleward-propagating anticyclonic eddies, rather than, as previously thought, a continuous intense western boundary current. The portrayal of this region in various runs of the NEMO 75-level model is found to vary between those two descriptions depending upon the resolution used and the implementation of the model's lateral boundary conditions. In a comparison of 1/4 ̊ resolution runs, the change of these conditions from free-slip to no-slip leads to the mean southward flow moving further offshore, with greater variability in the zonal and meridional velocities as the flow organises itself into eddies, and a reduction in total transport. If a realization of a model is unable to get these aspects of the physical flow correct, then this will significantly reduce its ability to show a realistic biological signal or long-term response to climate change. Further south, beyond Durban, the application of no-slip conditions similarly causes the mean Agulhas Current to lie further offshore, making it much more able to simulate Natal Pulses.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | 10.1016/j.ocemod.2012.12.011 |
Programmes: | NOC Programmes |
ISSN: | 14635003 |
Additional Keywords: | Indian Ocean: Mozambique Channel, NEMO, Spatial resolution, Boundary conditions, Stability, Natal Pulse (Current meandering) |
Date made live: | 07 Jan 2013 14:50 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/446712 |
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