Manykin et al. have suggested atmospheric Rydberg matter as an explanation of ball lightning phenomena. Rydberg matter is a condensed form of highly excited atoms in many aspects similar to electron-hole droplets in semiconductors. However, in contrast to electron-hole droplets, Rydberg matter has an extended life-time—as long as hours. This condensed excited state of matter is supported by experiments, mainly of a group led by Holmlid. It is similar to a liquid or solid state of matter with extremely low (gas-like) density. Lumps of atmospheric Rydberg matter can result from condensation of highly excited atoms that form by atmospheric electrical phenomena, mainly from linear lightning. Stimulated decay of Rydberg matter clouds can, however, take the form of an avalanche, and so appear as an explosion.