Page 9: Research news on greenhouse effect

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.

Solar radiation could cool Earth, not replace emissions

Techniques to reflect an additional small portion of sunlight back into space could help cool the planet if deployed globally, but they cannot address the full range of climate impacts or replace emission cuts, according ...

page 9 from 14