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Figure 6: The approximate numerical errors at one snapshot of a. Kuroshio model run. The region in red indicates that large numerical errors are commited in this region.

 

5 Conclusion

 

We have introduced three possible applications of wavelet analysis to the field of oceanography, and we believe that these applications are more than trivial but will be an important contribution to the field.

 

References

 

[1] Arakawa, A. and Lamb, V. R., Computational design of the basic dynamical processes of the UCLA general circulation model. Methods of Computational Physics, Vol 17, Academic Press, New York, 173-265, 1977.

[2] Batteen, M. L. and Y.-J. Han, On the computational noise of finite-difference schemes used in ocean models, Tellus, 33, 387-396, 1981.

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[4] Blumberg, A. F., and G. L. Mellor, A description of a three-dimensional coastal ocean circulation model, Three dimensional Coastal Ocean Models. Vol 4, edited by N. Heaps, pp 208, American Geophvsical Union. Washington, D.C.1987.

 

 

 

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