This question is about a description for the EM fields created when an electron decays into a lower energy state spontaneously in a single, isolated atom.
The treatment that I recall from grad school of absorption and emission starts from the model of a plane wave perturbing the atomic Hamiltonian. This model works conceptually for me to describe absorption and stimulated emission on a sort of statistical scale (many atoms), and obviously produces good real-world predictions for things like transition probabilities.
However, consider a single atom in a diffuse medium (say, a gas with low density) which, for some reason, has an electron in an excited state. Perhaps it absorbed some radiation or was jostled by other atoms. Let's consider the case that the excited state is one which decays quickly. The electron may move to a lower energy state, "emitting a photon", and some form of traveling EM fields will be radiated. This could happen even without interacting with neighbors or a passing EM plane wave. Right?
So what traveling EM fields are generated by such a transition? I imagine a sort of wave packet, perhaps the sum of multipole fields, but with a limited spatial/time extent, moving outward from the atom. Perhaps, the initial and final electron orbital states (themselves having multipole components) in the transition would determine the multipole components of the EM wave.
However, this does not seem to really work; one issue is, how would such a packet have a single frequency, as "the photon" does? Limited spatial extent would suggest a superposition of frequencies. A second issue is that, if "the photon" later interacts with some matter somewhere else (say, it is absorbed by a different atom), what happens to the wave front far away from the site of this interaction (say, in the opposite direction from the location of the original emission)?
Does anyone have an explanation, or link to a good treatment of this?
Thank you