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The article by Kuang et al. is a noteworthy first attempt to use a geodynamo simulation (constrained by the assimila¬tion of geomagnetic field models) to predict future secular variation.
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Now the Earth Simulator, one of the fastest computers in the world, has been used to run a geodynamo simulation that is the nearest yet to the real thing.
The latter team for the first time in the history of IGRF used assimilation of a retrospective field models including (CHAOS-2s) into a geodynamo simulation based on an approximation of core dynamics in order to obtain a SV forecast for the upcoming 5 years.
To go further, we could reduce the importance of SV model errors by co-estimating the unresolved field at degrees n>14 (and its associated uncertainties) together with the field at large length-scales, following Aubert (2014) who performed such a co-estimation using the cross-covariances between Gauss coefficients obtained from the forward integration of a geodynamo simulation.
Here we present a geodynamo simulation with an Ekman number of the order of 10-7 the highest-resolution simulation yet achieved, making use of 4,096 processors of the Earth Simulator.
Use a simulation model.
IGI uses a flight simulation game engine designed to create areas that go on for miles and miles.
The researchers used a computer simulation of a network to test reliability.
In 2016, he essentially copied Bonde's procedure, using a Labster simulation of enzyme kinetics.
We used a gravity simulation to have them bounce.
Fothergill created the footage with Maya animation software using a crowd simulation plugin called Miarmy.
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