time-dependent perturbation theory
Time-dependent perturbation theory describes what happens when the disturbance is not static but changes with time — switched on, oscillating, or pulsed. Now the natural question is no longer how energy levels shift but how the system jumps, or makes transitions, from one state to another. A system that started cleanly in one energy state gradually acquires some amplitude to be found in others, and the theory estimates how that amplitude grows.
We track this by writing the actual state as a changing blend of the unperturbed states, with coefficients that drift in time. Starting from the system sitting in one state, the leading estimate for the probability of ending up in another involves integrating the disturbance's matrix element against an oscillating factor over the time it acts. A disturbance that oscillates near a transition's natural frequency drives that transition efficiently — the quantum echo of resonance.
This framework is how quantum mechanics describes light interacting with matter: absorption, stimulated emission, and the rates at which atoms hop between levels. When the disturbance acts steadily over a long time, the result settles into a constant transition rate captured by a famous formula. Its honesty is in the word 'estimate': the predictions are reliable only while the probability of transition stays small, so the system has not been driven far from where it began.
The transition probability is the squared time-integral of the disturbance against an oscillating factor.
This is not the same as a measurement collapsing the state. Time-dependent perturbation theory describes smooth, unitary evolution; the 'transition probability' is the chance you would later find the system in another state if you measured.