The split quadratic model of a Morse flow #
This file studies the standard split-quadratic example of a negative-gradient flow. On a product of real Hilbert spaces, put
q(x, y) = (‖x‖² - ‖y‖²) / 2.
Its gradient is (x, -y), so its negative-gradient flow is
φ t (x, y) = (exp (-t) • x, exp t • y).
This file constructs that flow and computes its stable and unstable sets exactly. The stable set of the origin is the first coordinate plane and the unstable set is the second coordinate plane. Thus the two sets in this normalized linear example are genuine closed linear subspaces, rather than only sets defined by asymptotic convergence. For a general Morse critical point, the metric and Hessian determine the corresponding linearized gradient flow and its contraction rates.
Main declarations #
TauCeti.splitQuadratic: the standard split quadratic function.TauCeti.gradient_splitQuadratic: its gradient is(x, -y).TauCeti.lipschitzWith_gradient_splitQuadratic: its gradient is globally1-Lipschitz.TauCeti.isNondegenerateCriticalPoint_splitQuadratic_zero: the origin is nondegenerate.TauCeti.splitQuadraticFlow: its explicit negative-gradient flow.Flow.isNegativeGradient_splitQuadraticFlow: the flow solves the negative-gradient equation.TauCeti.negativeGradientFlow_splitQuadratic: the general construction of the negative gradient flow returns this explicit flow.Flow.stableSet_splitQuadraticFlow_zero: the stable set is the first coordinate plane.Flow.unstableSet_splitQuadraticFlow_zero: the unstable set is the second coordinate plane.
References #
- M. Audin and M. Damian, Morse Theory and Floer Homology, Springer Universitext, 2014, Chapters 1--2.
- Heegaard Floer homology roadmap, Lane M, "Morse homology".
The standard split quadratic function, positive on the first factor and negative on the
second. The factor 2⁻¹ normalizes its gradient to (x, -y).
Instances For
Evaluation of the standard split quadratic function.
The gradient of the split quadratic function is the identity on the first factor and minus the identity on the second.
Formula for the gradient of the split quadratic function.
The origin is the unique critical point of the split quadratic function.
The gradient of the split quadratic function is an isometry of the underlying space, hence in
particular globally 1-Lipschitz. This is the hypothesis under which the negative gradient flow
of a function exists on the whole line.
The origin is a nondegenerate critical point of the split quadratic function.
The explicit hyperbolic flow of the split quadratic function. Its first coordinate contracts in forward time and its second coordinate contracts in backward time.
Equations
Instances For
Evaluation of the split quadratic flow.
Every orbit of the explicit split flow solves the negative-gradient equation for
TauCeti.splitQuadratic.
On the split quadratic model, the negative gradient flow built from a globally Lipschitz gradient is the explicit hyperbolic flow.
A point converges to the origin in forward time exactly when its expanding coordinate vanishes.
A point converges to the origin in backward time exactly when its expanding-backward coordinate vanishes.
The stable set of the split quadratic flow at the origin is the first coordinate plane.
The unstable set of the split quadratic flow at the origin is the second coordinate plane.