Lecture 18 - Thu_2023 11 09 Bifurcations in the plane. % =============================================================================== Things I must not forget to say: #1 Explain the difference between chaos and stochastic. Chaos is deterministic, albeit hard to compute with precision. Same initial data --> same answer. With a program in the *same* computer: same thing happens. Stochastic equations are not deterministic. Same initial data --> different answer answer. With a program in the *same* computer: same thing happens. If (small) noise is added to a chaotic system, noise will be amplified. #2 Below, intuition for Hopf, #3 Below, Landau hypothesis. % % ----------------------------------------------------------------------------- % HOPF BIFURCATION. 1) INTUITION: soft (nonlinear stabilize) and hard (nonlinear destabilize). Explain scaling intuitively: Why is it the cubic stuff that matters? [the math. reason is resonances 2) ANALYSIS (This was mostly done in the prior lecture, so skip it here). This follows naturally the small gain vdp expansion. Consider \ddot{x} + x = r x + N(x, \dot{x}); N = nonlinear terms. Switches from stable to unstable spiral as r crosses zero going up. Let r = sigma*epsilon, 0 < epsilon << 1, scale x = sqrt{epsilon} X Why sqrt{epsilon}? See intuitive explanation above. Or the math.: In an expansion the quadratic terms cause no resonance, so the linear terms have to balance the cubic terms to suppress resonances. Then (for simplicity assume quadratic terms vanish, though not-needed). \ddot{X} + X = sigma epsilon X + epsilon C(X, \dot{X}) Derive: X ~ A(tau) e^{i t} + c.c., with tau = epsilon t and 2 i A_tau = (i sigma + gamma |A|^2) A. Write A = rho e^{i phi} ==> 2 rho_tau = (sigma + gamma_I rho^2) rho 2 phi_tau = - gamma_R rho^2 gamma_I < 0 Soft Hopf \ Limit cycle amplitude ~ sqrt{|r|} | START gamma_R > 0 Hard Hopf / """"" period ~ O(1). | TABLE! 3) LANDAU's HYPOTHESIS FOR TURBULENCE: sequence of "Hopf on a Hopf" ---> quasi-periodic solutions. Explain; they "live" on Tori. Problems: Cannot happen on dissipative systems [will explain later]; and: The "distance" between two nearby solutions grows linearly in time; breaks sensitive dependence on initial conditions. % % ----------------------------------------------------------------------------- % BIFURCATIONS OF CRITICAL POINTS. We first discuss bifurcations where a critical point is stable on one side. Explain: then, generically, there is a curve along which everything is attracted and where the bifurcation happens. Another way to think of it: intersections of two curves [the null-clines]. Note situation "the same" as 1-D, where the two "curves" for \dot{x} = f(x, mu) are: y = f(x, mu) and y = 0. Saddle node in 1-D ---> Saddle node in 2-D \dot{y} = -y \dot{x} = mu-x^2 Do phase portraits for mu > 0, mu=0, mu < 0. Transcritical: \dot{y} = -y and \dot{x} = mu*x - x^2 Saddle and node "exchange" Example: \dot{x} = -a*x+y ................ nullcline: y = a*x \dot{y} = x^2/(1+x^2) - y ....... nullcline: y = x^2/(1+x^2) Has both saddle-nodes and transcritical. Pitchforks: \dot{y} = -y and \dot{x} = mu*x-x^3 (soft). or \dot{x} = mu*x+x^3 (hard). Note analogy with Hopf: soft (nonlinear stabilize) and hard (nonlinear destabilize). Explain scaling "intuitively" % % ----------------------------------------------------------------------------- % BIFURCATIONS OF LIMIT CYCLES: GLOBAL. Prior bifurcations involved the neighborhood of a critical point: local. 1) Saddle-Node bifurcation of cycles. Two cycles "collide" and annihilate each other. \dot{r} = mu r + r^3 - r^5 = f(r) <-- this eqn. undergoes saddle node \dot{theta} = omega Explain "puzzle": how can two curves approach each other *everywhere* and end up the same at the same value of bifurcation parameter. Why is this not extremely rare? Answer: if one point coincides, then whole solution equal! Limit cycles amplitude ~ O(1) | ADD TO period ~ O(1) | TABLE. 2) Infinite Period Bifurcation: Critical point pops-up on limit cycle; destroys it. \dot{r} = r(1-r^2) \ limit cycle exists for r > 1, \dot{theta} = r - sin theta / does not for r < 1 [note it re-appears at r = -1]. Limit cycles amplitude ~ O(1) period ~ O(1/sqrt{|r-r_c|}) [critical slowing down]. 3) Homoclinic bifurcation. Do the picture. Limit cycles amplitude ~ O(1) period ~ O(1/log|r-r_c|) % % =============================================================================== EOF