Stability is defined by how the atmosphere responds to a parcel of air displaced vertically. In stable air the displaced parcel is cooler and denser than its surroundings and returns to where it started, so vertical motion is resisted. The signature that follows is consistent: clouds form in flat layers rather than building vertically, because moisture spreads horizontally along the level where it condenses; precipitation is steady and light rather than showery; air is smooth; and pollutants and moisture accumulate near the surface because nothing mixes them away. That last consequence is the operational one for a remote pilot, since the visibility requirement is three statute miles and stable conditions erode surface visibility over hours while presenting as pleasant flying weather. The distractors all describe the unstable case — rapid vertical motion, a steep lapse rate, turbulence and building cumulus — which produces rough air and good visibility, the opposite pairing.