Yearly Antarctic ozone depletion begins

 
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29 August 2011
 

The onset of summer at the South Pole has triggered the annual cycle of ozone depletion over the Antarctic, creating what is commonly known as the 'Ozone hole'.

Signs of ozone depletion are again appearing over the Antarctic, the United Nations reported today, adding that prevailing temperatures and polar stratospheric clouds indicate that the degree of ozone loss this year will most likely be about average in comparison to the past decade.

However, the World Meteorological Organization (WMO) noted that it is still too early to make a definitive statement on the level of depletion of ozone – which serves as a shield to protect life on Earth from harmful levels of ultraviolet rays – for 2011.

In Antarctica, the so-called ozone hole is an annually recurring winter/spring phenomenon due to the existence of extremely low temperatures in the stratosphere and the presence of ozone-depleting substances.

Despite international progress in cutting production and consumption of ozone-depleting chemicals, they have a long atmospheric lifetime and it will take several decades before their concentrations are back to pre-1980 levels, according to the WMO's first Antarctic Ozone Bulletin for this year.

In mid-August, the ozone hole area was normal compared to recent years – larger than in 2008 and 2010, but smaller than in 2009, according to the bulletin. As the sun returns to Antarctica after the polar night, it is expected that ozone destruction will speed up. The extent of ozone loss will to a large extent depend on meteorological conditions.

The depletion of the ozone layer is also due to a very cold winter in the stratosphere, which is the second major layer of the Earth's atmosphere, just above the troposphere.

WMO and the scientific community will use ozone observations from the ground, weather balloons and satellites, as wells as meteorological data, to monitor the development of the ozone hole in the coming weeks and months.

The onset of ozone depletion varies considerably from one year to the next, depending on the position of the polar vortex and availability of daylight after the polar night.

Measurements with ground based instruments and with weather balloons show first signs of ozone depletion at some sites located close to the vortex edge.

As the sun returns to Antarctica after the polar night, it is expected that ozone destruction will speed up, according to the WMO bulletin.

Source: UN News Centre

 

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