The greenhouse effect is the radiative process by which certain atmospheric gases (notably water vapor, carbon dioxide, methane, nitrous oxide, and ozone) absorb and re-emit longwave (infrared) radiation emitted by Earth’s surface and lower atmosphere, thereby reducing the net outgoing longwave flux to space and warming the lower troposphere and surface. It arises from molecular vibrational and rotational absorption bands that are transparent to most incoming shortwave solar radiation but partially opaque to outgoing terrestrial radiation. In climate science, the greenhouse effect is quantified via radiative forcing, feedbacks (e.g., water vapor and cloud feedbacks), and its role in establishing Earth’s energy balance and global mean temperature.
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