Our results suggest that the use of focused biological network models combined with large scale systems biology data sets can identify the salient biology underlying complex stressors like CS.
In order to use micro-scale model to deal with large scale practical engineering interfaces, a cantilever structure connected by bolted joint is taken as a macro scale example, and its dynamic model is established with the pressure distribution on the interface and real contact area obtained by simulations and experiments.
This work studies reduced order modeling (ROM) approaches to speed up the solution of variational data assimilation problems with large scale nonlinear dynamical models.
At the organ level, a full scale simulation model of the heart was used to assess the ability of the proposed method to cope with the additional complexities associated with large scale cardiac electrophysiology models.
Stiff fiber-bundle models can then be viewed as systems with large scale heterogeneities along the interface (i.e., large a and small L) for which the damage zone is notably extended.
However, we should mention that a recent novel (yet more complex) algorithm outperformed DE in multiple optimization tasks with large scale systems biology models due to extensive local search capability [ 9] that is lacking in the simplest form of DE.
The traction-separation relation was then fitted to a cohesive zone model to demonstrate the possibility of bridging atomistic modeling with large-scale numerical simulations.
The northern gradient approach provides an efficient means to detect coseismic signals and potentially constrain fault slip models with large-scale gravitational changes using limited time span of monthly GRACE solutions.
So far, GRACE observations have been applied to constrain fault slip models with large-scale gravity changes, but mostly from the direct use of level 1B (range and range-rate) data (e.g., Han et al. 2010, 2011, 2013).
This gradient approach particularly applies for the detection of coseismic signals with limited time span (e.g., a few months after the earthquake) of monthly GRACE solutions and potentially provides a means to constrain fault slip models with large-scale gravitational changes from GRACE observations.
