it helps maintain the temperature of the earth.
The absorption of ultraviolet radiation by the ozone layer help to sustain life because it helps to protect living things from damage of solar radiation.
The ozone layer absorbs ultraviolet radiation. The ozone layer is in the stratosphere. So, the thermosphere does not absorb radiation.
The depletion of the ozone layer decreases the absorption of ultraviolet radiation.
The stratosphere is warmed from below by the ozone layer (ozonosphere) through the absorption of ultraviolet radiation from the sun. This absorption of UV radiation by ozone molecules contributes to the warming of the stratosphere.
The ozone layer absorbs a significant portion of harmful ultraviolet (UV) radiation from the sun, particularly UV-B and UV-C rays. This absorption helps protect living organisms on Earth from the damaging effects of excessive UV radiation, which can cause skin cancer, cataracts, and harm to marine ecosystems. By filtering out harmful UV rays, the ozone layer plays a crucial role in sustaining life on our planet.
The ozone layer that filters ultraviolet radiation originated from
The stratosphere is the layer where the temperature increases due to the absorption of ultraviolet (UV) radiation by ozone. This absorption of UV radiation heats up the stratosphere, creating a temperature inversion where the temperature increases with altitude.
The ozone layer, which is a region of high ozone concentration in the stratosphere, absorbs damaging ultraviolet radiation from the sun. This absorption helps protect Earth's surface from the harmful effects of UV radiation, such as skin cancer and cataracts.
The ozone layer shields us from ultraviolet radiation.
The ozone layer in the stratosphere absorbs harmful ultraviolet radiation from the sun.
The ozone layer absorbs ultraviolet (UV) radiation from the sun, specifically UV-C and most UV-B rays. This absorption helps protect life on Earth by preventing harmful UV radiation from reaching the surface in excess amounts.
The stratosphere is the layer of the atmosphere where temperature increases with altitude. This is due to the absorption of ultraviolet radiation by the ozone layer, which heats up the surrounding air.