The source of the warmth of the stratosphere is the absorption of UV radiation by ozone, hence reduced ozone leads to cooling.
Small intestine is concerned primarily with absorption of nutrients whereas the large intestine is concerned primarily with the absorption of water.
Ozone depletion in the stratosphere is primarily caused by the release of certain chemicals known as ozone-depleting substances (ODS), such as chlorofluorocarbons (CFCs) and hydrochlorofluorocarbons (HCFCs). These chemicals contain chlorine and bromine atoms that are released into the atmosphere through human activities. When these molecules reach the stratosphere, they are broken down by ultraviolet (UV) radiation, releasing chlorine and bromine atoms that can then catalytically destroy ozone molecules. This process leads to the depletion of ozone in the stratosphere.
Ozone is generally found in most parts of the Earth's atmosphere, but the highest levels are recorded on the stratosphere region, namely the ozone layer. The plethora of ozone, represented by O3, serves to absorb the Sun's ultraviolet high frequency radiations, which life depends on.
aviod the absorption of the light or other radiations in the atmosphere of earth
temperature
the troposphere and the stratosphere
Small intestine is concerned primarily with absorption of nutrients whereas the large intestine is concerned primarily with the absorption of water.
The layers are defined primarily by the "lapse rate", or change in temperature with increasing altitude. The lapse rate is negative (temperature falls) in the troposphere, but positive (temperature rises) in the stratosphere. Temperatures decrease again when ascending into the Mesosphere.
Its function is primarily the absorption of water from fecal matter.
Its function is primarily the absorption of water from fecal matter.
d. intensity
Ozone depletion in the stratosphere is primarily caused by the release of certain chemicals known as ozone-depleting substances (ODS), such as chlorofluorocarbons (CFCs) and hydrochlorofluorocarbons (HCFCs). These chemicals contain chlorine and bromine atoms that are released into the atmosphere through human activities. When these molecules reach the stratosphere, they are broken down by ultraviolet (UV) radiation, releasing chlorine and bromine atoms that can then catalytically destroy ozone molecules. This process leads to the depletion of ozone in the stratosphere.
Ozone is generally found in most parts of the Earth's atmosphere, but the highest levels are recorded on the stratosphere region, namely the ozone layer. The plethora of ozone, represented by O3, serves to absorb the Sun's ultraviolet high frequency radiations, which life depends on.
No. The Moon is "in" the exosphere, and the levels of ozone there are non-detect. The ozone layer is primarily in the stratosphere.
Ultraviolet (UV) light treatment is used primarily in cases of severe psoriasis that have not responded to other medications or in cases affecting large portions of the body.
latitude and altitude
This is primarily the ionosphere that contains the ions.