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Extra resources for Ord Convective and advective heat transfer in geological science

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U. Christensen and G. A. Glatzmaier, Numerical modeling of the geodynamo: mechanisms of field generation and equili­ bration, J. Geophys. , 104, 10383-10404, 1999. Roberts, P. H. and G. A. Glatzmaier, Geodynamo theory and simu­ lations, Rev. Mod. , 72, 1081-1123, 2000. Roberts, P. H. and G. A. Glatzmaier, The geodynamo, past, present and future, Geophys. Astrophys. , 94, 47-84, 2001. Rogers, T. , G. A. Glatzmaier, and S. E. Woosley, Simulations of two-dimensional turbulent convection in a density-stratified fluid, Phys.

This feature is often called a discontinuity, but the sharpness and lateral con­ tinuity of the increase remains important research topics. Fig­ ure 2b indicates regions where the most compelling observations (from detailed waveform analyses) of the shear velocity increase are found, relative to large scale patterns in LAYANDGARNERO shear velocity (Figure 2a, Plate 1). , 2001]. g. Weber and Davis, 1990; Kendall and Nangini, 1996; Garnero and Lay, 2003]. , 1998]. This requires further investigation and assessment of the reliabil­ ity of isolated detections based on waveform complexity.

Earth Planet. , 98, 163-185, 1996. , A spectral solution of the magneto-convection equa­ tions in spherical geometry, Int. J Numer. Meth. Fluids, 32, 773-797, 2000. Hollerbach, R. and C. A. Jones, Influence of the Earth's inner core on geomagnetic fluctuations and reversals, Nature, 365,541-543,1993. Jones, C. , A. Longbottom, and R. Hollerbach, A self-consistent convection driven geodynamo model, using a mean field approx­ imation, Phys. , 92, 119-141, 1995. , M. Ochi, T. Sato, Flip-flop transitions of the magnetic intensity and polarity reversals in the magnetohydrodynamic dynamo, Phys.

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