Ozone amounts in the depletion layer are the lowest seen in the 21 year record of ozone profile measurements at the South Pole.
Partial column
ozone amounts in this layer declined from an average of 125 Dobson Units in July / August 2006 to 1.5 DU on October 6..
A balloon - borne, ozone instrument used to vertically profile
the ozone amount in the atmosphere.
Not exact matches
And while I researched it enough to know that the
amount of
ozone produced is very minimal and perfectly fine for the average household, I make sure to turn the machine off when it starts the deodorizing cycle, just
in case.
However, it blocks the excessive
amounts that can harm your child, especially
in today's world of global warming and
ozone depletion.
«While
ozone depletion from dichloromethane is currently quite modest, it is uncertain how the
amount of this gas
in the atmosphere will change
in the future.
But
in March, researchers with England's University of East Anglia reported finding four new
ozone - depleting compounds
in the atmosphere — three chlorofluorocarbons (CFCs) and one hydrochlorofluorocarbon (HCFC)--
amounting to about 81,000 tons.
The researchers found that while the
amount of
ozone depletion arising from VSLS
in the atmosphere today is small compared to that caused by longer - lived gases, such as CFCs, VSLS - driven
ozone depletion was found to be almost four times more efficient at influencing climate.
If the chemicals that were now discovered
in unexpectedly large
amounts can reach the
ozone layer
in significant quantities, they can cause damage.
Dichloromethane was found
in large
amounts, and so was 1,2 - dichloroethane, an
ozone - depleting substance used to make PVC.
They then compared their yearly September
ozone measurements with model simulations that predict
ozone levels based on the
amount of chlorine that scientists have estimated to be present
in the atmosphere from year to year.
Over the last 50 years satellite and ground - based records over Antarctica show
ozone column
amounts ranging from 100 to 400 Dobson units, which translates to about 1 millimeter (1/25 inch) to 5 millimeters (1/6 inch) of
ozone in a layer if all of the
ozone were brought down to the surface.
«When we ran these calculations, we found that
in some cases, there was a significant
amount of
ozone that built up
in the atmosphere, despite there not being any oxygen flowing into the atmosphere,» said Shawn Domagal - Goldman of NASA's Goddard Space Flight Center
in Greenbelt, Maryland.
They find that even if
ozone - damaging chemicals (chiefly CFCs) are phased out
in line with current international agreements, the
amount of chlorine - bearing material
in the stratosphere will continue to increase for several decades.
Twenty to 40 % of
ozone coverage might have been lost —
in turn, doubling the
amount of UV radiation that reached Earth's surface, the team reports
in a paper
in press
in Gondwana Research.
At precisely these altitudes, the
amount of
ozone in the stratosphere declined between three and six months after the eruption.
She collected pollen and irradiated it
in a lab for 3 minutes with UV light, simulating the
amount of UV that can reach the Earth's surface
in Patagonia and other regions
in the southern hemisphere under the seasonal
ozone hole.
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.
Inert gases such as neon (Ne), helium (He), and krypton (Kr) and other constituents such as nitrogen oxides, compounds of sulfur, and compounds of
ozone are found
in lesser
amounts.
A team of researchers from the NASA's Jet Propulsion Laboratory
in California and the Wageningen University
in the Netherlands measured the
amount of
ozone between 10,000 and 30,000 feet above the Earth's surface.
The transport processes are also very variable from winter to winter and the
amount of
ozone pumped into the Arctic is also correlated with temperature (this is not a causal relationship — the correlation exists, because variability
in temperatures and
in ozone transport are both driven by the same atmospheric processes).
According to a study published
in the March 2002 Journal of Geographical Research by a joint research team from the University of Maryland and NASA, overall, the increased
amount of CO2
in the atmosphere is speeding up the recovery of the
ozone layer — including the hole at the South Pole.
But near the poles and
in the upper stratosphere, CO2 is increasing the
amount of
ozone by preventing nitrogen oxide from breaking it down.
In his book «The Way Things Ought To Be» (1993) Limbaugh stretched the facts still further: «Mount Pinatubo in the Philippines spewed forth more than a thousand times the amount of ozone - depleting chemical in one eruption than all the fluorocarbons manufactured by wicked, diabolical, and insensitive corporations in history.&raqu
In his book «The Way Things Ought To Be» (1993) Limbaugh stretched the facts still further: «Mount Pinatubo
in the Philippines spewed forth more than a thousand times the amount of ozone - depleting chemical in one eruption than all the fluorocarbons manufactured by wicked, diabolical, and insensitive corporations in history.&raqu
in the Philippines spewed forth more than a thousand times the
amount of
ozone - depleting chemical
in one eruption than all the fluorocarbons manufactured by wicked, diabolical, and insensitive corporations in history.&raqu
in one eruption than all the fluorocarbons manufactured by wicked, diabolical, and insensitive corporations
in history.&raqu
in history.»
Response # 2: A different (probably equivalent, but I find it easier to understand) explanation is that the stratosphere is heated by absorbing solar / uv by
ozone; increasing the
amount of CO2 (which is only significantly active
in the IR) increases the ability of the stratosphere to lose heat, so it does.
The transport processes are also very variable from winter to winter and the
amount of
ozone pumped into the Arctic is also correlated with temperature (this is not a causal relationship — the correlation exists, because variability
in temperatures and
in ozone transport are both driven by the same atmospheric processes).
The depletion has persisted well into October 2006 and
ozone amounts are lowest seen
in the 21 - year observation record.
RE: Solar Sunshades The number of heavy lift rockets that would have to be launched to deploy the «sunshade
in space» would need to be so large that their exhaust emissions into the stratosphere would deplete a significant
amount of
ozone.
In the stratosphere, it from solar and LW absorption by
ozone, and a small
amount from water vapour, but what ever the temperature is, there is radiation from the CO2.
There are enough health - damaging pollutants
in the air today such that, if they (tropospheric
ozone, its principal precursor methane, black soot, and some other trace gases that contribute to the global warming) were reduced by feasible
amounts, the planet's energy balance could be restored, or nearly so.
Every increase
in ethanol use as fuel will increases the
amount of
ozone pollution
in the United States.
The remainder is made up with the other minor greenhouse gases,
ozone and methane for instance, and a small
amount from particles
in the air (dust and other «aerosols»).
In the worst years, two - thirds of the Arctic ozone column (the total amount of ozone between the ground and the top of the atmosphere) is destroyed in the most severely depleted region
In the worst years, two - thirds of the Arctic
ozone column (the total
amount of
ozone between the ground and the top of the atmosphere) is destroyed
in the most severely depleted region
in the most severely depleted regions.
This occurs because transportation
in North America produces a substantial
amount of black carbon (soot) and
ozone (a main ingredient
in smog), both of which warm climate, while power generation leads to a large
amount of sulfate particles, which cool climate even as they also lead to acid rain and damage human health.
The
amount of
ozone - depleters
in the atmosphere has dropped by more than 10 percent since peaking
in the late 1990s.
Current research combines the climate and chemistry changes
in the GISS model to predict future stratospheric
ozone amounts both over the polar regions and at lower latitudes.
While the buildup of greenhouse gases leads to global warming at Earth's surface, it also cools the stratosphere, which increases the
amount of
ozone depletion
in the polar regions.
The number of particles that form, and therefore the
amount of chemical
ozone destruction, is extremely sensitive to small changes
in stratospheric temperature.
Variations
in temperatures,
ozone amounts, and the altitude at which the atmosphere has a given pressure have been correlated with the solar cycle.
His invention of an electron capture device that was able to detect tiny
amounts of chemicals enabled other scientists both to understand the dangers of DDT to the egshells of birds and to figure out the ways
in which chlorofluorocarbons were eroding the
ozone layer.
Moonbats: «Jacobson found that domes of increased carbon dioxide concentrations — discovered to form above cities more than a decade ago — cause local temperature increases that
in turn increase the
amounts of local air pollutants, raising concentrations of health - damaging ground - level
ozone as well as particles
in urban air.»
The experiment would have the same
amount of energy
in each case; but how efficient each frequency energy would alter the temperature of, say,
ozone.
'' «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.
The change
in total solar irradiance over recent 11 - year sunspot cycles
amounts to < 0.1 %, but greater changes at ultraviolet wavelengths may have substantial impacts on stratospheric
ozone concentrations, thereby altering both stratospheric and tropospheric circulation patterns... This model prediction is supported by paleoclimatic proxy reconstructions over the past millennium.
The
amount of
ozone in the upper troposphere depends on dynamical processes [waves] and transport mechanisms between controlling the downward intrusions of
ozone from the stratosphere, thus driven from below.
As the Antarctic sea ice reached record levels, scientists floated several hypotheses, including possible changes
in the
ozone hole over Antarctica, or increased
amounts of fresh water — which freezes more easily — on the surface of the ocean around Antarctica.
26 If the
ozone blocks ultraviolet radiation...... then a decrease in ozone means and increase in the amount of ultraviolet radiation that reaches Earth's surface RESULTS OF OZONE DEPL
ozone blocks ultraviolet radiation...... then a decrease
in ozone means and increase in the amount of ultraviolet radiation that reaches Earth's surface RESULTS OF OZONE DEPL
ozone means and increase
in the
amount of ultraviolet radiation that reaches Earth's surface RESULTS OF
OZONE DEPL
OZONE DEPLETION
Using a computer model, they showed that weather conditions would have lowered the
amount of
ozone over Antarctica anyways, and that the big hole was a result of winds from the tropics carrying less
ozone to the area than
in the years before.
It will not rise at all if the absorption is balanced by an equal
amount of emission (as would occur if its emissivity would be increased from a change
in its molecular composition — e.g. the formation of
ozone from UV radiation or mixing a little CO2 within it).
There was one WUWT thread which discussed the organic molecules plankton puts into the air, and how they can reach the upper atmosphere, and, (because they included elements ending
in «ine,» such as Bromine, Fluorine, Chlorine, and Iodine,) alter the
amount of
Ozone, which
in turn effected the types and powers of sunlight.