secondary atmosphere javv-e dovomân, havâsepehr-e ~ Fr.: atmosphère secondaire An atmosphere of a planet that forms after primordial gases had been lost or had failed to accumulate. A secondary atmosphere develops from internal volcanic outgassing, or by accumulation of material from comet impacts. It is characteristic of terrestrial planets, such as Earth, Mercury, Venus, and Mars. → primordial atmosphere. → secondary; → atmosphere. |