In a system such as the climate, we can never include enough variables to describe the actual system on all relevant length scales (e.g. the butterfly effect — MICROSCOPIC perturbations grow exponentially in time to drive the system to completely different states over macroscopic time) so the best that we can often do is model it as a complex nonlinear set
of ordinary differential equations with stochastic noise terms — a generalized Langevin equation or generalized Master equation, as it were — and average behaviors over what one hopes is a spanning set of butterfly - wing perturbations to assess whether or not the resulting system trajectories fill the available phase space uniformly or perhaps are restricted or constrained in some way.
We develop systems
of ordinary differential equations to address the generic features of the initial phase of spheroid formation and an agent - based three - dimensional computational model to focus on spatial differences in the process.
Not exact matches
Ordinary differential equations typically apply when several variables are a function
of time, while partial
differential equations get used when a variable is dependent on both time and space, says Michael Reed, a professor
of mathematics at Duke University who applies mathematics to physiology and medicine.
With respect to solvers, in 1993, he developed the world's fastest
ordinary differential equation solver in a three - dimensional model for a given level
of accuracy and applied it to atmospheric chemistry.
The framework is based on solving nonlinear coupled
ordinary and partial
differential equations that model the kinetics
of the following phenomena: (1) mass transport in the electrolyte and electrode using the Nernst - Planck
equation; (2) electrical potential distribution using the Poisson
equation; (3) interfacial reactions that determine the boundary conditions or source terms (using the Butler - Volmer
equation or constant - flux conditions); and (4) evolution
of the electrode / electrolyte interface using the Allen - Cahn
equation within the phase - field modeling (PFM) approach.
They implemented
ordinary differential equations — a process for describing how things change over time — to improve their ability to infer what these gene relationships might look like and to allow more dynamic simulation
of these biological processes over time.
We have built a linear
ordinary differential equation (ODE) based model for the kinetics
of β - selection in the presence or absence
of Itpkb.
Complex nonlinear multivariate systems often exhibit «strange attractors» — local fixed points in a set
of coupled nonlinear
ordinary differential equations — that function as foci for Poincare cycles in the multivariate phase space.
Such systems occur in numerous domains
of physics and can be described by both
ordinary and partial
differential equations.