On Earth, temperature inversion occurs
because ozone in the stratosphere absorbs much of the sun's ultraviolet radiation, preventing it from reaching the surface, protecting the biosphere, and therefore warming the stratosphere instead.
Not exact matches
The Antarctic
ozone hole forms and expands during the Southern Hemisphere spring (August and September)
because of the high levels of chemically active forms of chlorine and bromine
in the
stratosphere.
Because ozone in the troposphere is a precursor to OH, they deployed weather balloons equipped with measuring devices known as sondes to measure the amount of
ozone in the air from the surface to the
stratosphere.
Because they are released
in large quantities from tropical oceans, they are rapidly lofted by tropical thunderstorms into the
stratosphere within a month or two where they can destroy
ozone for a larger portion of their lifetimes.
Currently only
ozone - depleting substances with atmospheric lifetimes ranging from a year to over 100 years, are controlled
because they linger
in the atmosphere long enough to reach the upper atmosphere, called the
stratosphere.
Temperature inversion
in Earth's
stratosphere occurs
because of the presence of
ozone, while on Jupiter and Saturn, it is caused by the presence of hydrocarbons.
The
stratosphere is involved
in TMT, TTS and TLS and that is cooling
because of
ozone depletion and increasing CO2.
This is due to the fact that the atmosphere warms with height
in the
stratosphere [
because of the
ozone layer].
And, «fluctuation of
ozone in the
stratosphere is likely a natural phenomenon
because solar radiation is a fluctuating event.»
But scientists have now found that stratospheric
ozone is probably not recovering at lower latitudes, between 60 ⁰ N and 60 ⁰ S (London lies at 51 ⁰ N),
because of unexpected decreases
in ozone in the lower part of the
stratosphere.
'' «It all amounts to a mystery, but a troubling one
because ozone protects life at the surface from incoming ultraviolet radiation, and any thinning of total
ozone in the
stratosphere is cause for concern.
Destruction of
ozone in the
stratosphere takes place as quickly as formation of
ozone,
because the chemical is so reactive.
The
stratosphere has cooled
because of
ozone loss due to moisture arising
in tropical convection overshoot.
So, according to the climate models, the reason why temperatures increase with height
in the
stratosphere is
because of
ozone heating.
Global warming is implicated
in the loss of Arctic
ozone because greenhouse gases trap energy lower down, heating up the atmosphere nearer the ground but cooling the
stratosphere, creating conditions conducive to the formation of the reactive chemicals that break apart the three - oxygen molecules of
ozone.
«
Because of the strong absorption of
ozone in the UV occurring
in the upper
stratosphere and meso - sphere, a solar influence on the thermal structure
in these regions of the atmosphere is plausible.
Omitting OMPS - Limb will result
in the complete loss of precise information about the
ozone - height profile after 2014,
because OMPS - Limb was the only instrument planned to fly after Aura that would be capable of determining
ozone profiles below the peak concentration
in the
stratosphere.
Ozone recovery in the tropical stratosphere is expected to be faster and the recovery of the polar ozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric clo
Ozone recovery
in the tropical
stratosphere is expected to be faster and the recovery of the polar
ozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric clo
ozone hole is expected to be slower
because of the CO2 - induced cooling of the
stratosphere (and increase the number of polar stratospheric clouds).