July 26, 2007
NEW CLUES TO OZONE DEPLETION
LARGE quantities
of ozone-depleting chemicals
have been discovered in the Antarctic atmosphere by researchers from
the
The team of
atmospheric chemists carried out
an 18-month study of the make-up of the lowest part of the earth's
atmosphere
on the Brunt Ice Shelf, about 20 km from the
The source of the halogens is natural – sea-salt in the case of bromine, and in the case of iodine, almost certainly bright orange algae that coat the underside of the sea ice around the continent.
These halogens cause a substantial depletion in ozone above the ice surface. This affects the so-called oxidising capacity of the atmosphere - its ability to "clean itself" by removing certain - often man-made - chemical compounds. The iodine oxides also form tiny particles (a few nanometres in size), which can grow to form ice clouds, with a consequent impact on the local climate.
Scientists now
plan to carry out further research
to assess what impact this may be having on the local environment. Very
recent
satellite observations by one of the team, Dr Alfonso Saiz-Lopez, have
confirmed that iodine oxides are widespread throughout coastal
John Plane,
professor of atmospheric
chemistry at the
Using high-tech measuring equipment, a beam of light was projected across the ice shelf and the spectrum of the reflected light analysed and chemical levels measured. The work was carried out in a new atmospheric observatory at Halley Station, operated by the British Antarctic Survey, and was supported by funding from the U.K.’s Natural Environment Research Council.
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