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The images in this
Envirocast®
Bulletin were captured by the
Ozone Monitoring Instrument on NASA’s
Aura satellite
on September 29, 2006. They show the ozone
concentration in the stratosphere above the South
Pole. |
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Antarctic Ozone
Hole on September 29, 2006

Greens and yellows
show areas with the highest ozone amounts, while
blues and purples show where ozone amounts
are lowest. A purple veil of extremely low levels
of ozone stretches across most of Antarctica,
which is roughly centered in the image. The 2006
ozone hole is about 10.8 million square miles,
which is larger than the entire continent of North
America (about 9.5 million square miles).
Scientists generally use
Dobson Units to describe ozone
concentrations.
The Dobson Unit
describes how much ozone there would be in a
column of the atmosphere if all the molecules were
squeezed into a single layer.
The average amount of ozone in the atmosphere is
roughly 300 Dobson Units, equivalent to a
layer 0.12 inches thick. Any place where the
concentration drops below 220 Dobson Units
is considered part of the ozone hole. Average
ozone concentrations in the ozone hole are around
100 Dobson Units.
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Related Information:
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Every year when daylight
returns in spring (autumn in the northern hemisphere) to
Antarctica, chemical processes begin that break down the
ozone in the stratosphere, creating a hole in the ozone
layer. The hole begins to develop in mid-August each year
and peaks in late September or early October. When summer
approaches, the conditions become less favorable for the
ozone-destroying reactions and the size of the hole
becomes stable.
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