Euler method

From any point on a curve, you can find an approximation of a nearby point on the curve by moving a short distance along a line tangent to the curve.

Starting with the differential equation (1), we replace the derivative y′ by the finite difference approximation

${\displaystyle y'(t)\approx {\frac {y(t+h)-y(t)}{h}},}$

(2)

which when re-arranged yields the following formula

${\displaystyle y(t+h)\approx y(t)+hy'(t)}$

and using (1) gives:

${\displaystyle y(t+h)\approx y(t)+hf(t,y(t)).}$

(3)

This formula is usually applied in the following way. We choose a step size h, and we construct the sequence ${\displaystyle t_{0},t_{1}=t_{0}+h,t_{2}=t_{0}+2h,...}$ We denote by ${\displaystyle y_{n}}$ a numerical estimate of the exact solution ${\displaystyle y(t_{n})}$. Motivated by (3), we compute these estimates by the following recursive scheme

${\displaystyle y_{n+1}=y_{n}+hf(t_{n},y_{n}).}$

(4)

This is the Euler method (or forward Euler method, in contrast with the backward Euler method, to be described below). The method is named after Leonhard Euler who described it in 1768.

The Euler method is an example of an explicit method. This means that the new value y_n+1 is defined in terms of things that are already known, like y_n.

Backward Euler method

If, instead of (2), we use the approximation

${\displaystyle y'(t)\approx {\frac {y(t)-y(t-h)}{h}},}$

(5)

we get the backward Euler method:

${\displaystyle y_{n+1}=y_{n}+hf(t_{n+1},y_{n+1}).}$

(6)

The backward Euler method is an implicit method, meaning that we have to solve an equation to find y_n+1. One often uses fixed-point iteration or (some modification of) the Newton–Raphson method to achieve this.

It costs more time to solve this equation than explicit methods; this cost must be taken into consideration when one selects the method to use. The advantage of implicit methods such as (6) is that they are usually more stable for solving a stiff equation, meaning that a larger step size h can be used.

First-order exponential integrator method

Exponential integrators describe a large class of integrators that have recently seen a lot of development.^[13] They date back to at least the 1960s.

In place of (1), we assume the differential equation is either of the form

${\displaystyle y'(t)=-A\,y+{\mathcal {N}}(y),}$

(7)

or it has been locally linearized about a background state to produce a linear term ${\displaystyle -Ay}$ and a nonlinear term ${\displaystyle {\mathcal {N}}(y)}$.

Exponential integrators are constructed by multiplying (7) by ${\textstyle e^{At}}$, and exactly integrating the result over a time interval ${\displaystyle [t_{n},t_{n+1}=t_{n}+h]}$:

${\displaystyle y_{n+1}=e^{-Ah}y_{n}+\int _{0}^{h}e^{-(h-\tau )A}{\mathcal {N}}\left(y\left(t_{n}+\tau \right)\right)\,d\tau .}$

This integral equation is exact, but it doesn't define the integral.

The first-order exponential integrator can be realized by holding ${\displaystyle {\mathcal {N}}(y(t_{n}+\tau ))}$ constant over the full interval:

${\displaystyle y_{n+1}=e^{-Ah}y_{n}+A^{-1}(1-e^{-Ah}){\mathcal {N}}(y(t_{n}))\ .}$

(8)

Generalizations

The Euler method is often not accurate enough. In more precise terms, it only has order one (the concept of order is explained below). This caused mathematicians to look for higher-order methods.

One possibility is to use not only the previously computed value y_n to determine y_n+1, but to make the solution depend on more past values. This yields a so-called multistep method. Perhaps the simplest is the leapfrog method which is second order and (roughly speaking) relies on two time values.

Almost all practical multistep methods fall within the family of linear multistep methods, which have the form

$${\displaystyle {\begin{aligned}&{}\alpha _{k}y_{n+k}+\alpha _{k-1}y_{n+k-1}+\cdots +\alpha _{0}y_{n}\\&{}\quad =h\left[\beta _{k}f(t_{n+k},y_{n+k})+\beta _{k-1}f(t_{n+k-1},y_{n+k-1})+\cdots +\beta _{0}f(t_{n},y_{n})\right].\end{aligned}}}$$

Another possibility is to use more points in the interval ${\displaystyle [t_{n},t_{n+1}]}$. This leads to the family of Runge–Kutta methods, named after Carl Runge and Martin Kutta. One of their fourth-order methods is especially popular.

Advanced features

A good implementation of one of these methods for solving an ODE entails more than the time-stepping formula.

It is often inefficient to use the same step size all the time, so variable step-size methods have been developed. Usually, the step size is chosen such that the (local) error per step is below some tolerance level. This means that the methods must also compute an error indicator, an estimate of the local error.

An extension of this idea is to choose dynamically between different methods of different orders (this is called a variable order method). Methods based on Richardson extrapolation,^[14] such as the Bulirsch–Stoer algorithm,^[15][16] are often used to construct various methods of different orders.

Other desirable features include:

• dense output: cheap numerical approximations for the whole integration interval, and not only at the points t₀, t₁, t₂, ...
• event location: finding the times where, say, a particular function vanishes. This typically requires the use of a root-finding algorithm.
• support for parallel computing.
• when used for integrating with respect to time, time reversibility

Alternative methods

Many methods do not fall within the framework discussed here. Some classes of alternative methods are:

• multiderivative methods, which use not only the function f but also its derivatives. This class includes Hermite–Obreschkoff methods and Fehlberg methods, as well as methods like the Parker–Sochacki method^[17] or Bychkov–Scherbakov method, which compute the coefficients of the Taylor series of the solution y recursively.
• methods for second order ODEs. We said that all higher-order ODEs can be transformed to first-order ODEs of the form (1). While this is certainly true, it may not be the best way to proceed. In particular, Nyström methods work directly with second-order equations.
• geometric integration methods^[18][19] are especially designed for special classes of ODEs (for example, symplectic integrators for the solution of Hamiltonian equations). They take care that the numerical solution respects the underlying structure or geometry of these classes.
• Quantized state systems methods are a family of ODE integration methods based on the idea of state quantization. They are efficient when simulating sparse systems with frequent discontinuities.

Parallel-in-time methods

Some IVPs require integration at such high temporal resolution and/or over such long time intervals that classical serial time-stepping methods become computationally infeasible to run in real-time (e.g. IVPs in numerical weather prediction, plasma modelling, and molecular dynamics). Parallel-in-time (PinT) methods have been developed in response to these issues in order to reduce simulation runtimes through the use of parallel computing.

Early PinT methods (the earliest being proposed in the 1960s)^[20] were initially overlooked by researchers due to the fact that the parallel computing architectures that they required were not yet widely available. With more computing power available, interest was renewed in the early 2000s with the development of Parareal, a flexible, easy-to-use PinT algorithm that is suitable for solving a wide variety of IVPs. The advent of exascale computing has meant that PinT algorithms are attracting increasing research attention and are being developed in such a way that they can harness the world's most powerful supercomputers. The most popular methods as of 2023 include Parareal, PFASST, ParaDiag, and MGRIT.^[21]

Convergence

A numerical method is said to be convergent if the numerical solution approaches the exact solution as the step size h goes to 0. More precisely, we require that for every ODE (1) with a Lipschitz function f and every t^* > 0,

${\displaystyle \lim _{h\to 0^{+}}\max _{n=0,1,\dots ,\lfloor t^{*}/h\rfloor }\left\|y_{n,h}-y(t_{n})\right\|=0.}$

All the methods mentioned above are convergent.

Consistency and order

Suppose the numerical method is

${\displaystyle y_{n+k}=\Psi (t_{n+k};y_{n},y_{n+1},\dots ,y_{n+k-1};h).\,}$

The local (truncation) error of the method is the error committed by one step of the method. That is, it is the difference between the result given by the method, assuming that no error was made in earlier steps, and the exact solution:

${\displaystyle \delta _{n+k}^{h}=\Psi \left(t_{n+k};y(t_{n}),y(t_{n+1}),\dots ,y(t_{n+k-1});h\right)-y(t_{n+k}).}$

The method is said to be consistent if

${\displaystyle \lim _{h\to 0}{\frac {\delta _{n+k}^{h}}{h}}=0.}$

The method has order ${\displaystyle p}$ if

${\displaystyle \delta _{n+k}^{h}=O(h^{p+1})\quad {\mbox{as }}h\to 0.}$

Hence a method is consistent if it has an order greater than 0. The (forward) Euler method (4) and the backward Euler method (6) introduced above both have order 1, so they are consistent. Most methods being used in practice attain higher order. Consistency is a necessary condition for convergence, but not sufficient; for a method to be convergent, it must be both consistent and zero-stable.

A related concept is the global (truncation) error, the error sustained in all the steps one needs to reach a fixed time ${\displaystyle t}$. Explicitly, the global error at time ${\displaystyle t}$ is ${\displaystyle y_{N}-y(t)}$ where ${\displaystyle N=(t-t_{0})/h}$. The global error of a ${\displaystyle p}$th order one-step method is ${\displaystyle O(h^{p})}$; in particular, such a method is convergent. This statement is not necessarily true for multi-step methods.

Stability and stiffness

For some differential equations, application of standard methods—such as the Euler method, explicit Runge–Kutta methods, or multistep methods (for example, Adams–Bashforth methods)—exhibit instability in the solutions, though other methods may produce stable solutions. This "difficult behaviour" in the equation (which may not necessarily be complex itself) is described as stiffness, and is often caused by the presence of different time scales in the underlying problem.^[23] For example, a collision in a mechanical system like in an impact oscillator typically occurs at much smaller time scale than the time for the motion of objects; this discrepancy makes for very "sharp turns" in the curves of the state parameters.

Stiff problems are ubiquitous in chemical kinetics, control theory, solid mechanics, weather forecasting, biology, plasma physics, and electronics. One way to overcome stiffness is to extend the notion of differential equation to that of differential inclusion, which allows for and models non-smoothness.^[24][25]