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In the following simulations we use this simulated 2-D signal (y sim ) with the same modes and amplitudes, we only change the SNR value.
In simulations, we use the NS-2 simulator of version 2.34.
For our forward simulations, we use the 3-D global chemical transport model MATCH driven by NCEP meteorology.
In our hybrid simulations we use Chamberlain profiles for the atmospheric components.
For the simulations we use a crystal plasticity finite element and different polycrystal homogenization models.
In our simulations we use, however, fixed atmospheric greenhouse concentrations (except for water vapour) and, therefore, the transition to a Snowball state may occur at different TSI for different atmospheric levels of greenhouse gases.
In the 3D simulations we use an adaptive mesh refinement technique in order to guarantee a sufficient interface resolution while keeping the computational costs low.
To reduce the computational costs of the numerical simulations, we use mixed lattice Boltzmann models, constructed using different quadrature methods on each Cartesian axis.
For our simulations, we use synthetic graphs ranging from 100K to 16M vertices to show the scalability and quality performance of our algorithm.
In addition to simulations, we use a large set of SNMP data from an operational IP network on the order of 1000 nodes to test our methods.
In our simulations, we use ν=1.
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