Less ozone means less security. This will cause UV to enter the earth.
The less common form is ozone. It is formed in stratosphere.
Ozone is primarily found in the stratosphere layer of the atmosphere. This region extends from about 12 to 50 kilometers above the Earth's surface. Ozone plays a vital role in absorbing and filtering out harmful ultraviolet radiation from the Sun.
Ozone is a tri oxygen molecule. While the ozone layer is formed by the collection of large number of ozone molecules.
The ozone layer is a region with a relatively high concentration of ozone, and is located near the bottom of the stratosphere. It is located 8 to 50km above sea level. The altitude varies with latitude, placing the stratosphere and the ozone layer closer to the Earth's surface over the poles.The highest concentration is in the lower stratosphere, also called the tropopause. Ozone is found in some concentration in all layers of the atmosphere. Ozone in the troposphere (near Earth's surface) is one component of smog.Ozone concentrations vary from near zero at extreme elevations (high in the exosphere), to a maximum (~9 ppm) at the bottom of the stratosphere, to zero again near Earth's surface. Some ozone is found in every layer of the atmosphere (usually less than 1 ppm, except for the stratosphere).(for more information, see the related question)The ozone layer is in the upper atmosphere of the earth.
There is normally no life that breathes in the stratosphere. In the troposphere, both plants and animals suffer when significant amounts of ozone are present.
The effect of less ozone in stratosphere is the UV's entering the ecosystem. They can cause disturbance in the biosphere.
The less common form is ozone. It is formed in stratosphere.
Ozone is primarily found in the stratosphere layer of the atmosphere. This region extends from about 12 to 50 kilometers above the Earth's surface. Ozone plays a vital role in absorbing and filtering out harmful ultraviolet radiation from the Sun.
Ozone is a tri oxygen molecule. While the ozone layer is formed by the collection of large number of ozone molecules.
The ozone layer is a region with a relatively high concentration of ozone, and is located near the bottom of the stratosphere. It is located 8 to 50km above sea level. The altitude varies with latitude, placing the stratosphere and the ozone layer closer to the Earth's surface over the poles.The highest concentration is in the lower stratosphere, also called the tropopause. Ozone is found in some concentration in all layers of the atmosphere. Ozone in the troposphere (near Earth's surface) is one component of smog.Ozone concentrations vary from near zero at extreme elevations (high in the exosphere), to a maximum (~9 ppm) at the bottom of the stratosphere, to zero again near Earth's surface. Some ozone is found in every layer of the atmosphere (usually less than 1 ppm, except for the stratosphere).(for more information, see the related question)The ozone layer is in the upper atmosphere of the earth.
There is normally no life that breathes in the stratosphere. In the troposphere, both plants and animals suffer when significant amounts of ozone are present.
The mesosphere extends from the stratopause to about 53 miles (85 km) above the earth. The gases, including the oxygen molecules, continue to become thinner and thinner with height. As such, the effect of the warming by ultraviolet radiation also becomes less and less leading to a decrease in temperature with height. On average, temperature decreases from about 5°F (-15°C) to as low as -184°F (-120°C) at the mesopause. However, the gases in the mesosphere are still thick enough to slow down meteorites hurtling into the atmosphere, where they burn up, leaving fiery trails in the night sky.
Ozone is comprised of three oxygen molecules (O3) and is classified as a triatomic allotrope of oxygen. It is a naturally occurring gas found in the Earth's stratosphere and can also be produced at ground level through chemical reactions involving pollutants.
As you move from the troposphere to the stratosphere, the temperature typically increases due to the presence of the ozone layer which absorbs UV radiation. In the stratosphere, the jet stream and most weather phenomena occur, making it a region of significant atmospheric stability and less turbulence compared to the troposphere below.
A decrease in ozone in the stratosphere can lead to increased levels of ultraviolet (UV) radiation reaching the Earth's surface. This can result in higher rates of skin cancer, cataracts, and weakened immune systems in humans. Additionally, it can harm ecosystems and marine life.
When ozone is removed from the stratosphere, there is less protection from harmful ultraviolet (UV) radiation reaching the Earth's surface. This can lead to increased rates of skin cancer, cataracts, and other health problems in humans, as well as adverse effects on marine ecosystems and agriculture.
It is a microscopic effect with observable macroscopic consequences. Daughter products of ozone decay can be found in the atmosphere, and the ozone hole lasts longer, starts sooner, and has less total column ozone in it.