Earth's Atmosphere and the Greenhouse Effect
Our atmosphere is a thin layer of gases (78% nitrogen, 21% oxygen, 1% other gases) that protects Earth and makes life possible. When solar radiation reaches Earth, some is reflected back to space while the rest is absorbed by the surface and atmosphere.
The greenhouse effect is a natural process where certain gases trap heat and maintain Earth's temperature. When the Earth's surface gives off infrared radiation, greenhouse gases like water vapor, carbon dioxide, methane, and nitrous oxide absorb and redirect this energy back to the surface instead of letting it escape to space.
Global warming occurs when the greenhouse effect intensifies due to increased greenhouse gas concentrations. While some temperature fluctuations are natural, human activities significantly contribute to the problem. We release carbon dioxide through burning fossil fuels and deforestation, while methane comes from livestock, rice cultivation, and landfills.
💡 Think of the greenhouse effect like a blanket around Earth - we need it to stay warm, but adding too many layers (extra greenhouse gases) makes the planet overheat!





