\documentstyle[11pt]{article} \textheight 22cm \textwidth 16cm \hoffset= -0.6in \voffset= -0.5in \setlength{\parindent}{0cm} \setlength{\parskip}{15pt plus 2pt minus 2pt} \pagenumbering{roman} \setcounter{page}{-9} \newcommand{\dg}{^\circ} \newcommand{\be}{\begin{equation}} \newcommand{\ee}{\end{equation}} \newcommand{\bd}{\begin{displaymath}} \newcommand{\ed}{\end{displaymath}} \newcommand{\comega}{\varpi} \begin{document} \begin{center} {\Large ASTR450 Homework \# 10 -- Perturbations\\ Due Tuesday, May 2} \end{center} 1. {\bf Impulse Approximation to a Drag Force.} Consider a satellite on an inclined elliptical orbit acted on by a drag force of the form ${\bf F} = -k{\bf v}_{rel}$, where ${\bf v}_{rel}$ is the velocity of the satellite relative to the atmosphere, and $k$ is a positive constant. Recall that Earth's atmosphere decays exponentially with height (scale height $\approx 10$km).\\ a) Approximate the range of eccentricities for which the drag force can be approximated by an impulse at pericenter. \\ b) Consider a rotating Earth. Start by making a qualitative estimate of the error made in neglecting rotation. How does the Earth's rotation affect an equatorial orbit ($i=\Omega=0$)? Describe how the orbital elements $a, e, i, \Omega, \comega$ vary in time.\\ c) Now imagine orbits with $i\ne 0, \Omega \ne 0$. Using the perturbation equations and other physical arguments, describe qualitatively how these orbits will evolve (i.e. how $a, e, i, \Omega, \comega$ vary in time). 2. {\bf Radial Perturbation Forces.} Consider a radial perturbation force of the form ${\bf F} = R \hat r$, where $R$ is a function of the distance $r$.\\ a) Apply the perturbation equations to this force and obtain simplified expressions for $da/dt$, $de/dt$, $di/dt$, $d\Omega/dt$, and $\comega/dt$.\\ b) A radial perturbation to gravity, which is itself a radial force, is an example of a central force. So angular momentum must be conserved. Show that your equations conserve the angular momentum vector and describe the constraints that this imposes on these orbits. \\ c) Now let $R=Ar^n$ where $A$ is a constant. Take the time average of your expressions over a single unperturbed Keplerian orbit (this step assumes that the perturbation is small). Show that $ = 0$ and argue, on physical ground, that $<\cos\nu>$ is negative (or zero) and that $ = 0$. It can be shown that $$ is negative for $n>-2$ and positive for $n<-2$. Use this fact to determine how the sign of your time-averaged $d\comega/dt$ depends on $A$ and $n$. Use the Central Force Integrator to check your results numerically.\\ d) Finally, consider the General Relativistic (GR) Perturbation $R = A r^{-4}$ where $A$ is a small negative constant. The integral $ = a^{-4}e(1-e^2)^{-5/2}$. Solve, analytically, for the value of $A$ that will give 30 degrees of precession per orbit for $e=0.5$ (The true effects of GR on Mercury's orbit are almost exactly a million times weaker). Convert your prediction into the proper initial conditions for the Central Force Integrator, and test it! Start your orbit at pericenter and turn in a copy of your plot. 3. Using the paper by Burns et al. (1979), fill in the missing steps in the derivations of Eqs 24 and 28 for $da/dt$ and $de/dt$. Show enough work that I can see that you understand the derivations! \enddocument{}