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102<br />
References<br />
Abiodun, B.J., J.M. Prusa and W.J. Gutowski,<br />
Implementation of a Non-hydrostatic, Adaptive-Grid<br />
Dynamics Core in CAM3. Part I: Comparison of<br />
Dynamics Cores in Aqua-Planet Simulations. Clim.<br />
Dynamics, 31, 795-810 [DOI: 10.1007/s00382-008-0381-<br />
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Abiodun, B.J., W.J. Gutowski and J.M. Prusa,<br />
Implementation of a Non-hydrostatic, Adaptive-Grid<br />
Dynamics Core in CAM3. Part II: Dynamical Influences<br />
on ITCZ Behavior and Tropical Precipitation. Clim.<br />
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Figure 2. Energy spectra of CAM-EULAG in aquaplanet<br />
simulation compared with spectra from CAM<br />
simulations using either Eulerian spectral or finite<br />
volume dynamics cores.<br />
Lipps, F.B., and R.S. Hemler, A scale analysis of deep<br />
moist convection and some related numerical<br />
calculations. J Atmos Sci, 39, 2192–2210, 1982.<br />
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Figure 3. Time and zonal average precipitation vs.<br />
latitude for a uniform low-resolution case [LU -<br />
4˚(lat)], a case with high resolution for (20S-20N)<br />
[H20 – 2˚(lat)] and a case with very high resolution<br />
for (20S-20N) [V20 – 1˚(lat)]. Resolution outside the<br />
tropics is 4˚(lat) in all cases.<br />
Smolarkiewicz P.K., Temperton, C., Thomas, S.J. and<br />
Wyszogrodzki,A.A., Spectral Preconditioners for<br />
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ocean modelling, 6-10 September 2004, Reading, UK,<br />
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