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A NASA-led study has documented an unprecedented depletion of Earth's protective ozone layer above the Arctic last winter and spring that was caused by an unusually prolonged period of extremely low temperatures in the stratosphere.
. . .
The Antarctic ozone hole forms when extremely cold conditions, common in the winter Antarctic stratosphere, trigger reactions that convert atmospheric chlorine from human-produced chemicals into forms that destroy ozone. While the same ozone-loss processes occur each winter in the Arctic, the generally warmer stratospheric conditions there limit the area affected and the time frame during which the chemical reactions occur. This means there is generally far less ozone loss in most years in the Arctic than in the Antarctic.
www.physorg.com...
The 2011 Arctic ozone loss occurred over an area considerably smaller than that of the Antarctic ozone holes. This is because the Arctic polar vortex, a persistent large-scale cyclone within which the ozone loss takes place, was about 40 percent smaller than a typical Antarctic vortex. While smaller and shorter-lived than its Antarctic counterpart, the Arctic polar vortex is more mobile, often moving over densely populated northern regions. Decreases in overhead ozone lead to increases in surface ultraviolet radiation, which are known to have adverse effects on humans and other life forms.
Originally posted by john_bmth
reply to post by Praetorius
I think the bloody great big hole in the ozone layer is the cause for concern.
The Antarctic ozone hole forms when extremely cold conditions, common in the winter Antarctic stratosphere, trigger reactions that convert atmospheric chlorine from human-produced chemicals into forms that destroy ozone.
Originally posted by kalunom
So, back in the 80's when we were all using Aquanet on our hair and the Chloroflourocabons -CFC-'s were destroying the ozone...and we had to stop using them.
Now...the hole is back anyway.
Work has suggested that a detectable (and statistically significant) recovery will not occur until around 2024, with ozone levels recovering to 1980 levels by around 2068.
Ozone concentrations in the lower stratosphere over Antarctica will increase by 5%–10% by 2020 and return to pre-1980 levels by about 2060–2075
Originally posted by MasterGemini
As the article states this was caused by unusually frigid temperatures in the atmosphere. Interesting to see the "scientific" community of climatologists actually got a prediction right for once.
The scientists found that at some altitudes, the cold period in the Arctic lasted more than 30 days longer in 2011 than in any previously studied Arctic winter, leading to the unprecedented ozone loss.
ScienceDaily (Apr. 8, 2011) — In the past few weeks, exceptional weather conditions have led to unprecedented ozone depletion over the Arctic. Ground and satellite observations by researchers at the Laboratoire Atmosphères, Milieux, Observations Spatiales (CNRS/UVSQ/UPMC) as well as French models show that ozone loss reached around 40% at the end of March. The phenomenon was caused by an extremely cold and persistent stratospheric winter, resulting in significant ozone destruction, which, unusually, continued into spring.
The Arctic ozone hole, that began expanding due to the clouds, radically widened in March and April, coinciding with the Fukushima disaster. The damaged Fukushima reactors and burning fuel rods released many, many tons of of iodine (a highly-reactive ozone-attacking agent) and xenon, which soon transformed into xenon fluoride (produced when xenon comes under UV catalysis to combine with fluorine gas in the atmosphere). Fluorine is abundant over the US Pacific Northwest and Canada. The jet stream carried the iodine and newly-formed XeFl compounds in a northeasterly direction, crossing into the Arctic circle and looping back down over Greenland, Scandinavia and European Russia. This exactly accounts for the oblong shape and direction of the expanded ozone hole.
Some radioactive isotopes of xenon, for example, 133Xe and 135Xe, are produced by neutron irradiation of fissionable material within nuclear reactors.[7]
Xenon is obtained commercially as a byproduct of the separation of air into oxygen and nitrogen. After this separation, generally performed by fractional distillation in a double-column plant, the liquid oxygen produced will contain small quantities of krypton and xenon. By additional fractional distillation steps, the liquid oxygen may be enriched to contain 0.1–0.2% of a krypton/xenon mixture, which is extracted either via adsorption onto silica gel or by distillation.
Originally posted by Phage
Originally posted by MasterGemini
As the article states this was caused by unusually frigid temperatures in the atmosphere. Interesting to see the "scientific" community of climatologists actually got a prediction right for once.
Actually, it the article says it was the unusually prolonged period of cold temperatures at high altitudes, not that the temperatures were unusually low.
The scientists found that at some altitudes, the cold period in the Arctic lasted more than 30 days longer in 2011 than in any previously studied Arctic winter, leading to the unprecedented ozone loss.
www.sciencedaily.com...
The prolonged period allowed polar stratospheric clouds to persist longer that usual and thus allowing the reactions between CFCs and O3 to persist longer than usual. This resulted in a greater net loss of O3.
edit on 10/3/2011 by Phage because: (no reason given)
un·u·su·al
[uhn-yoo-zhoo-uhl, -yoozh-wuhl] Show IPA
adjective
not usual, common, or ordinary; uncommon in amount or degree; exceptional: an unusual sound; an unusual hobby; an unusual response.
Origin:
1575–85; un-1 + usual
Related forms
un·u·su·al·ly, adverb
un·u·su·al·ness, noun
Synonyms
extraordinary, remarkable; rare, strange, singular, curious, queer, odd.
Originally posted by kalunom
So, back in the 80's when we were all using Aquanet on our hair and the Chloroflourocabons -CFC-'s were destroying the ozone...and we had to stop using them.
Now...the hole is back anyway. Imagine that, us humans really aren't the ones affecting such large planetary phenomena....
Shocking.
^sarcasm^
"In the 2010-11 Arctic winter, we did not have temperatures that were lower than in the previous cold Arctic winters," said Walker. "What was different about this year was that the temperatures were low enough to generate ozone-depleting forms of chlorine for a much longer period of time
Originally posted by Phage
reply to post by MasterGemini
Please show where the article says "unusually frigid temperatures" were found.
That may be difficult because the article says this:
"In the 2010-11 Arctic winter, we did not have temperatures that were lower than in the previous cold Arctic winters," said Walker. "What was different about this year was that the temperatures were low enough to generate ozone-depleting forms of chlorine for a much longer period of time
www.sciencedaily.com...
As I said, the temperatures were not unusually "frigid". They persisted for an unusually long period.
edit on 10/3/2011 by Phage because: (no reason given)
A NASA-led study has documented an unprecedented depletion of Earth's protective ozone layer above the Arctic last winter and spring that was caused by an unusually prolonged period of extremely low temperatures in the stratosphere
"In the 2010-11 Arctic winter, we did not have temperatures that were lower than in the previous cold Arctic winters," said Walker. "What was different about this year was that the temperatures were low enough to generate ozone-depleting forms of chlorine for a much longer period of time
Uranium tetrafluoride (UF4) is a green crystalline solid compound of uranium with an insignificant vapor pressure and very slight solubility in water. Uranium in its tetravalent (uranous) state is very important in different technological processes. In the uranium refining industry it is known as green salt. UF4 is generally an intermediate in the conversion of uranium hexafluoride (UF6) to either uranium oxides (U3O8 or UO2) or uranium metal. It is formed by the reaction of UF6 with hydrogen gas in a vertical tube-type reactor or by the action of hydrogen fluoride(HF) on uranium dioxide. UF4 is less stable than the uranium oxides and reacts slowly with moisture at ambient temperature, forming UO2 and HF, which are very corrosive; it is thus a less favorable form for long-term disposal. The bulk density of UF4 varies from about 2.0 g/cm3 to about 4.5 g/cm3 depending on the production process and the properties of the starting uranium compounds.
Originally posted by Phage
reply to post by MasterGemini
No.
"In the 2010-11 Arctic winter, we did not have temperatures that were lower than in the previous cold Arctic winters," said Walker. "What was different about this year was that the temperatures were low enough to generate ozone-depleting forms of chlorine for a much longer period of time
www.sciencedaily.com...
edit on 10/3/2011 by Phage because: (no reason given)
"What was different about this year was that the temperatures were low enough to generate ozone-depleting forms of chlorine for a much longer period of time.