The cause was an unusually long spell of cold weather at altitude. In cold conditions, the chlorine chemicals that destroy ozone are at their most active. It is currently impossible to predict if such losses will occur again, the team writes in the journal Nature.
"Winter in the Arctic stratosphere is highly variable - some
are warm, some are cold, but over the last few decades, the winters that are cold have been getting colder.Why this occurred will take years of detailed study.” said Michelle Santee from Nasa's Jet
Propulsion Laboratory (JPL).
"So given that trend and the
high variability, we'd anticipate that we'll have other cold ones, and
if that happens while chlorine levels are high, we'd anticipate that
we'd have severe ozone loss."
Ozone-destroying chemicals originate in substances such as
chlorofluorocarbons (CFCs) that came into use late last century in
appliances including refrigerators and fire extinguishers.Their destructive effects were first documented in the Antarctic, which now sees severe ozone depletion in each of its winters.
Their use was progressively restricted and then eliminated by the 1987 Montreal Protocol and its successors. The ozone layer blocks ultraviolet-B rays from the Sun, which can cause skin cancer and other medical conditions.
Winter temperatures in the Arctic stratosphere do not generally fall as low as at the southern end of the world. Longer, not colder. Ozone destruction takes place within polar stratospheric clouds, with chlorine the main culprit. No records for low temperature were set this year, but the air
remained at its coldest for an unusually long period of time, and
covered an unusually large area. In addition, the polar vortex was stronger than usual. Here,
winds circulate around the edge of the Arctic region, somewhat isolating
it from the main world weather systems.
Some monitoring stations in northern Europe and Russia
recorded enhanced levels of ultraviolet-B penetration, though it is not
clear that this posed any risk to human health.
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