"ZETANC" A MODEL FOR ALL SEASONS
The ZETANC developed at GFDL is a high resolution, non-hydrostatic, fully compressible model of hemispheric
extent. The model is being used for the simulation of the detailed structure of extra-tropical storms and storm tracks. The studies are aimed in particular at a more definitive understanding of the effects of moist convection on storm structure and evolution. These simulations will be used to evaluate parameterizations
in global climate models. The model will also will be used to study the seasonal cycle and inter-annual variability of the storm tracks and their
sensitivity to climate change, placing particular emphasis on extreme extra-tropical weather.
ZETANC could be used to simulate phenomena at any meteorological scale since it does not
require the standard restricted assumptions. In order to illustrate the versatility of the model, two extreme experiments
are shown: a) Bubble convection in an isentropic environment, and b) the life-cycle of baroclinic eddies.
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Bubble Convection
The initial bubble is circular, 50 meters in diameter and weakly buoyant. As the bubble rises it develops two vortices centered on its sides (Hill vortices). The upward velocity is larger
at the bottom than at the top. This differential velocity causes the bubble to deform with a classical mushroom shape. Since the bubble is not very buoyant individual convective
cells are produced in its periphery. Probably, Kelvin-Helmholtz instability is produced on the sides by
the strong circulation. I selected this experiment because was reported in the literature by Andre Robert "Bubble convection Experiments
with semi-implicit Formulation of the Euler Equations. J.A.S 1993". Click on the figure for animation. -> |
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