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For certain \(r\) intervals, or windows, the Lorenz equations exhibit a period- doubling property similar to that of the logistic difference equation discussed in Section \(2.9 .\) Careful calculations may reveal this phenomenon. Now consider values of \(r\) slightly larger than those in Problem 9. (a) Plot trajectories of the Lorenz equations for values of \(r\) between 100 and \(100.78 .\) You should observe a steady periodic solution for this range of \(r\) values. (b) Plot trajectories for values of \(r\) between 100.78 and \(100.8 .\) Determine as best you can how and when the periodic trajectory breaks up.

Short Answer

Expert verified
**Question:** Analyze the Lorenz equations for different ranges of r values and determine how and when the periodic trajectory breaks up. **Short Answer:** For r values between 100 and 100.78, you will observe a steady periodic solution. However, as you increase r values between 100.78 and 100.8, analyze the plotted trajectories to see how and when the periodic trajectory breaks up. This may require experimenting with different numerical methods, step sizes, and initial conditions to fully observe the changes in periodicity and stability of the trajectories.

Step by step solution

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01

(Understanding the Lorenz equations)

The Lorenz equations are a set of three differential equations that describe the motion of a fluid with respect to temperature variations. They are given by: $ \begin{aligned} \frac{dx}{dt} &= \sigma(y-x) \\ \frac{dy}{dt} &= x(r-z) - y \\ \frac{dz}{dt} &= xy - bz \\ \end{aligned} $ where x, y, and z are dependent variables, t is independent variable, and σ, r, and b are positive constants.
02

(Step 1: Setting up the Lorenz equations for different r values)

We will consider two sets of r values as described in the exercise: 1. r between 100 and 100.78 2. r between 100.78 and 100.8 We will use the Lorenz equations as shown earlier and plug in the r values to set up the necessary equations.
03

(Step 2: Plotting trajectories for r values between 100 and 100.78)

To plot trajectories for different r values, we can use numerical methods like Euler's method or a specialized method like the fourth-order Runge-Kutta method. Use a computer software or a programming language like Python to implement these methods and plot trajectories for the given range of r values. It's important to understand that providing specific details on how to use these numerical methods and computer software is out of the scope of this exercise. You need to experiment with the chosen method and software to attain the desired results. When you plot the trajectories for r values between 100 and 100.78, you should observe a steady periodic solution.
04

(Step 3: Plotting trajectories for r values between 100.78 and 100.8)

Next, we need to plot trajectories for r values between 100.78 and 100.8. Follow the same process and use a numerical method along with a computer software or programming language to plot these trajectories.
05

(Step 4: Analyzing the trajectories for r values between 100.78 and 100.8)

After plotting the trajectories for r values between 100.78 and 100.8, you should carefully analyze the plotted trajectories. You need to investigate how and when the periodic trajectory breaks up. Keep in mind that this exercise might require some trial and error, and you would need to experiment with different numerical methods, step sizes, and initial conditions in order to observe the effects of different r-values on the periodicity and stability of the trajectories.

Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Differential Equations
At the heart of many scientific and engineering problems lie differential equations. These are mathematical equations that relate some function with its derivatives. In the context of the Lorenz equations, we see a system of three differential equations that describe the dynamic behavior of a system, such as the convection rolls of fluids in the atmosphere. These equations are integral in studying how the system evolves over time, depending on various factors like temperature and pressure represented by the variables and parameters in the equations. Understanding how to solve these equations, analytically when possible or numerically often, is crucial for predicting system behaviors in real-world scenarios.
Dynamical Systems
Dynamical systems theory is a broad area that deals with systems that change over time. These systems can be as diverse as planetary orbits, population models, or, in our case, weather patterns described by the Lorenz equations. Crucial in studying dynamical systems is the concept of states and how these states evolve as time progresses. In the exercise, plotting trajectories is a method of visualizing state evolution, with each state characterized by a set of values for the variables x, y, and z. These plots reveal the nature of the system's temporal behavior and any patterns or irregularities that may occur.
Period-Doubling Bifurcation
Bifurcation refers to a qualitative change in a system's behavior as a parameter, such as r in the Lorenz equations, is varied. Period-doubling is a type of bifurcation where a system that has been oscillating with a certain period starts oscillating with twice that period. It's a route to chaos where a system can go through several period-doublings as parameters are varied. In the Lorenz system, as r increases, the attractor changes, leading to period-doubling bifurcations, which are hints of the onset of chaos. Identifying these bifurcations in plotted trajectories from the exercise can help students recognize early signs of complex behavior emerging in dynamical systems.
Numerical Methods
Often, differential equations cannot be solved with pen and paper, and numerical methods come to the rescue. These are techniques that give approximate solutions to mathematical problems that might be too complex to solve analytically. In the exercise, methods like Euler's method or the fourth-order Runge-Kutta method enable the plotting of trajectories by iteratively calculating the states of the system at each timestep. By learning and applying these computational tools, students are empowered to explore and understand systems that are described by complex differential equations, like the Lorenz equations, and appreciate the role of computation in modern scientific analysis.
Chaotic Systems
Chaos theory deals with systems that can show a significant sensitivity to initial conditions, meaning that small differences in the starting point can lead to vastly different outcomes. This phenomenon is sometimes referred to as the 'butterfly effect.' The Lorenz equations, in particular, are famous for being one of the first contexts in which chaos was discovered. In our exercise, when the parameter r is varied, we see the system's trajectory transitioning from periodic to chaotic behavior. Understanding chaotic systems is a fascinating aspect of mathematics and physics because it shows how even deterministic systems (like the Lorenz equations under certain conditions) can behave in unpredictable ways.

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Most popular questions from this chapter

Consider the ellipsoid $$ V(x, y, z)=r x^{2}+\sigma y^{2}+\sigma(z-2 r)^{2}=c>0 $$ (a) Calculate \(d V / d t\) along trajectories of the Lorenz equations \((1) .\) (b) Determine a sufficient condition on \(c\) so that every trajectory crossing \(V(x, y, z)=c\) is directed inward. (c) Evaluate the condition found in part (b) for the case \(\sigma=10, b=8 / 3, r=28\)

(a) Find all the critical points (equilibrium solutions). (b) Use a computer to draw a direction field and portrait for the system. (c) From the plot(s) in part (b) determine whether each critical point is asymptotically stable, stable, or unstable, and classify it as to type. $$ \text { The van der Pol equation: } \quad d x / d t=y, \quad d y / d t=\left(1-x^{2}\right) y-x $$

The equation of motion of an undamped pendulum is \(d^{2} \theta / d t^{2}+\omega^{2} \sin \theta=0,\) where \(\omega^{2}=g / L .\) Let \(x=\theta, y=d \theta / d t\) to obtain the system of equations $$ d x / d t=y, \quad d y / d t=-\omega^{2} \sin x $$ (a) Show that the critical points are \((\pm n \pi, 0), n=0,1,2, \ldots,\) and that the system is almost lincar in the neighborhood of cach critical point. (b) Show that the critical point \((0,0)\) is a (stable) center of the corresponding linear system. Using Theorem 9.3.2 what can be said about the nonlinear system? The situation is similar at the critical points \((\pm 2 n \pi, 0), n=1,2,3, \ldots\) What is the physical interpretation of these critical points? (c) Show that the critical point \((\pi, 0)\) is an (unstable) saddle point of the corresponding linear system. What conclusion can you draw about the nonlinear system? The situation is similar at the critical points \([\pm(2 n-1) \pi, 0], n=1,2,3, \ldots\) What is the physical interpretation of these critical points? (d) Choose a value for \(\omega^{2}\) and plot a few trajectories of the nonlinear system in the neighborhood of the origin. Can you now draw any further conclusion about the nature of the critical point at \((0,0)\) for the nonlinear system? (e) Using the value of \(\omega^{2}\) from part (d) draw a phase portrait for the pendulum. Compare your plot with Figure 9.3 .5 for the damped pendulum.

Consider the eigenvalues given by equation ( 39 ). Show that $$\left(\sigma_{1} X+\sigma_{2} Y\right)^{2}-4\left(\sigma_{1} \sigma_{2}-\alpha_{1} \alpha_{2}\right) X Y=\left(\sigma_{1} X-\sigma_{2} Y\right)^{2}+4 \alpha_{1} \alpha_{2} X Y$$ Hence conclude that the eigenvalues can never be complex-valued.

(a) Find all the critical points (equilibrium solutions). (b) Use a computer to draw a direction field and portrait for the system. (c) From the plot(s) in part (b) determine whether each critical point is asymptotically stable, stable, or unstable, and classify it as to type. $$ d x / d t=y, \quad d y / d t=x-\frac{1}{6} x^{3}-\frac{1}{5} y $$

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