Volcanoes don't inject significant chlorine into the stratosphere but they do increase small particles, which increase the amount
of polar stratospheric clouds with which the human - made chlorine reacts.
Chlorine eats away at ozone, but only if light is present and if the atmosphere is cold enough to create
polar stratospheric clouds on which chlorine chemistry can occur — a relationship that Solomon was first to characterize in 1986.
(Such low air temperatures encourage the formation of icy clouds in the upper atmosphere known
as polar stratospheric clouds, which foster the chemical reactions that turn harmless chlorine compounds into ozone eradicators.)
The temperature of the stratosphere is one of the key factors in the springtime depletion of ozone above the Antarctic where in winter it gets colder than anywhere else on Earth, encouraging icy particles to form
in polar stratospheric clouds.
In both the past two winters, researchers
saw polar stratospheric clouds over parts of Britain, said Jonathan Shanklin of the British Antarctic Survey.
Unusually low temperatures in the stratosphere, even cold records, are at fault — creating conditions whereby ice crystals form in so
called polar stratospheric clouds.
An eerie «
polar stratospheric cloud,» which destroys ozone at a rapid rate, hangs above Kiruna, Sweden, in January 2000.
At the surface of
polar stratospheric clouds, chemical reactions take place, converting passive chlorine compounds into reactive compounds that trigger stratospheric ozone depletion.
On the basis of its intended flight route, the Perlan glider might be able to provide the first direct observations of
polar stratospheric clouds, a unique type of ice cloud that forms in the polar stratosphere and helps to deplete ozone, Gong adds.
Research: reaction mechanisms and numerical simulation of atmospheric chemistry and transport; photochemistry of ozone and organic trace gases;
polar stratospheric clouds and denitrification.
Particles composed of such hydrates are thought to be the principal component of
the polar stratospheric clouds that initiate the destruction of ozone.
It normally reaches its widest extent in the southern hemisphere in the spring (August and September), as extreme cold temperatures in the stratosphere facilitate chemical reactions on the surface of
polar stratospheric clouds.
We show that chemical loss of column ozone (Î O3) and the volume of Arctic vortex air cold enough to support the existence of
polar stratospheric clouds (VPSC) both exceed levels found for any other Arctic winter during the past 40 years.
Subsequently it was shown variation was due to a combination of variation in UV, extremely cold temperatures, formation of
polar stratospheric clouds (PSC) and intense atmospheric circulation.
It is caused by chemical reactions that take place primarily on the surface of
polar stratospheric clouds, ice particles or liquid droplets which form at high altitudes in extreme cold.
Ozone holes are caused by chemical reactions that take place primarily on the surface of
polar stratospheric clouds, ice particles, or liquid droplets, which form at high altitudes in the extreme cold of the polar regions.
But last year, Susan Solomon of MIT — who back in the 1980s became one of the world's most celebrated scientists for uncovering the chemistry of
the polar stratospheric clouds — declared that she had detected the first «fingerprints» of the hole closing.
Solomon blamed 2015 on the Calbuco volcano in Chile, which ejected sulphur particles that enhanced the ozone - destroying properties of
polar stratospheric clouds.
An unusual persistence of cold temperatures in the stratosphere into March, allowing longer lifetimes for
the polar stratospheric clouds that enable conversion of pollutant gases into ozone - destroying chlorine.
The process occurs most readily at temperatures below -77 C, at which point
a polar stratospheric cloud can develop (UNEP image below).
Particles composed of such hydrates are thought to be the principal component of
the polar stratospheric clouds that initiate the destruction of ozone.