Ozone present in the troposphere is also called as bad ozone. It is also a
green house gas. It is the major constituent of the urban smog.
Stratus clouds typically form at low altitudes, Cumulus clouds form at varying altitudes depending on their type, and Cirrus clouds form at high altitudes. Stratus clouds are usually seen as layered and overcast, Cumulus as fluffy and white, and Cirrus as thin and wispy.
Cirrus clouds form at higher altitudes because they are composed of ice crystals that require cold temperatures to exist. These clouds typically form in the upper troposphere where temperatures are low enough for the ice crystals to form and remain suspended in the air.
Cirrus clouds are found at high altitudes, typically above 20,000 feet. Cumulus clouds are often found at lower to middle altitudes, usually between 6,500 to 20,000 feet. Stratus clouds form at low altitudes, below 6,500 feet. Nimbostratus clouds can extend through a wide range of altitudes, from low to high, depending on the vertical development of the cloud system.
Fog is usually a very low altitude, probably about ground level.
All clouds are diffiened into four layers as follows- low level clouds-stratus, stratocumulus,nimbostratus and fog(really low stratus) medium level clouds-altocumulus,altostratus high level clouds-cirrocumulus,cirrostratus and cirrus. many level clouds- these are usually convective clouds like cumulonimbuses. stratocumulus for A+
At low altitudes, ozone increases due to the presence of pollutants like nitrogen oxides and volatile organic compounds that undergo chemical reactions in the presence of sunlight. These reactions create ozone as a byproduct, leading to higher ozone levels near the Earth's surface.
There is ozone at all altitudes. So "zero".
Nimbo-stratus and stratus clouds form at low altitudes.
The ozone hole forms over Antarctica. It is because of low temperature.
100% of the ozone is found at elevations higher than Earth's surface.
I don't imagine it correlates because the ozone layer is in the stratosphere, whereas we are in the troposphere. It would vary better with altitude (because atmospheric pressure will influence the partial pressure ('concentration') of oxygen), however the individuals who live at great altitudes adjust by increasing their levels of red blood cells and haemaglobin. It would affect newcomers from low altitudes - they need to adjust gradually to changing altitudes.
Ozone is a greenhouse gas at lower altitudes. It absorbs heat at the ground level.
Stratus clouds typically form at low altitudes, Cumulus clouds form at varying altitudes depending on their type, and Cirrus clouds form at high altitudes. Stratus clouds are usually seen as layered and overcast, Cumulus as fluffy and white, and Cirrus as thin and wispy.
Ozone is generally spread throughout. It can vary with pressure, temperature and altitudes.
just high altitudes
Cirrus clouds form at higher altitudes because they are composed of ice crystals that require cold temperatures to exist. These clouds typically form in the upper troposphere where temperatures are low enough for the ice crystals to form and remain suspended in the air.
The ozone is the triatomic form of ozone. It is present in the form of ozone layer in the atmosphere.