Greenhouse gases, including carbon dioxide (CO2), are effective at absorbing longwave infrared radiation emitted by the Earth but not shortwave solar radiation. Solar radiation passes through the atmosphere without significant absorption, warming the Earth's surface. The infrared radiation emitted by the Earth has longer wavelengths, which are partially absorbed by CO2. While CO2 does absorb infrared radiation, water vapor plays a more significant role in atmospheric absorption due to its higher concentration and broader absorption spectrum. The relative abundance of water vapor compared to CO2 suggests that CO2 contributes less to greenhouse gas absorption than commonly estimated by the IPCC. Other gases, such as methane and CFCs, also absorb infrared radiation but to a lesser extent than CO2. The greenhouse effect is primarily due to the ability of these gases to trap longwave radiation, which helps maintain the Earth's temperature. The wavelengths of infrared radiation from the sun and human bodies fall within the same range, but their distributions differ based on temperature.