its the greenhouse effect
Certain gases in the Earth's atmosphere, like carbon dioxide (CO2), methane (CH4), and water vapor (H2O), have the ability to absorb and re-emit infrared radiation. This process, called the greenhouse effect, traps heat in the atmosphere, warming the Earth's surface. When these gases absorb infrared rays, they vibrate and release heat, which helps maintain the planet's temperature suitable for life.
carbon dioxide
At night, the Earth's surface loses heat absorbed during the day through a process called radiative cooling. This heat is emitted in the form of infrared radiation, which is not visible to the human eye but can be detected as thermal energy. The emitted infrared rays are a result of the vibrations of molecules in the surface materials, which cool down as they release energy into the atmosphere. Consequently, this process contributes to the overall temperature balance of the Earth.
The main heating rays of the sun are known as infrared radiation. These rays penetrate the Earth's atmosphere and heat up its surface, contributing to the warming of the planet. The Earth then re-emits this heat as longer-wavelength infrared radiation.
The Earth's atmosphere blocks most of the ultraviolet radiation from the Sun, as well as certain infrared wavelengths. This is important for protecting life on Earth from harmful radiation. Most radio waves, visible light, and some infrared and ultraviolet radiation are able to pass through the atmosphere.
Certain gases in the Earth's atmosphere, like carbon dioxide (CO2), methane (CH4), and water vapor (H2O), have the ability to absorb and re-emit infrared radiation. This process, called the greenhouse effect, traps heat in the atmosphere, warming the Earth's surface. When these gases absorb infrared rays, they vibrate and release heat, which helps maintain the planet's temperature suitable for life.
greenhouse effect. It describes how certain gases in the Earth's atmosphere, such as carbon dioxide and methane, trap heat from the sun and warm the planet's surface. This natural process is essential for maintaining Earth's temperature within a range that supports life.
Other greenhouse gases such as methane and nitrous oxide absorb infrared radiation (heat) that is emitted from the Earth's surface, trapping it in the atmosphere. This trapped heat contributes to the warming of the atmosphere, similar to how the ozone layer absorbs and traps incoming ultraviolet rays from the sun.
infrared rays
Ozone gas in earth's atmosphere absorbs UV rays. It does not absorb infrared rays.
The Earth's atmosphere blocks most gamma rays and X-rays, which are high-energy wavelengths. While some infrared light and microwaves can penetrate the atmosphere, a significant portion of infrared light is absorbed by water vapor and carbon dioxide. Visible light, on the other hand, passes through the atmosphere relatively unimpeded.
carbon dioxide
infrared rays
The main difference between gamma rays and infrared rays is in their wavelengths. Gamma rays have the shortest wavelengths while infrared rays have longer wavelengths. Gamma and infrared rays are types of electromagnetic radiation.
At night, the Earth's surface loses heat absorbed during the day through a process called radiative cooling. This heat is emitted in the form of infrared radiation, which is not visible to the human eye but can be detected as thermal energy. The emitted infrared rays are a result of the vibrations of molecules in the surface materials, which cool down as they release energy into the atmosphere. Consequently, this process contributes to the overall temperature balance of the Earth.
The main heating rays of the sun are known as infrared radiation. These rays penetrate the Earth's atmosphere and heat up its surface, contributing to the warming of the planet. The Earth then re-emits this heat as longer-wavelength infrared radiation.
Visible light rays from the Sun penetrate the atmosphere and heat the Earth's surface. The Earth absorbs this energy and then emits it back as infrared radiation, which is absorbed by greenhouse gases in the atmosphere. This process, known as the greenhouse effect, warms the atmosphere and helps regulate Earth's temperature.