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Environmentalists generally
talk about the ozone hole over
Antarctica. Is it really a hole?
What does ozone hole mean?
Answers
Answer:
Explanation:
Figure Q10-1. Arctic and Antarctic temperatures. Air temperatures in both polar
regions reach minimum values in the lower
stratosphere in the winter season. Average
daily minimum values over Antarctica are
as low as −90°C in July and August in a typical year. Over the Arctic, average minimum
values are near −80°C in late December and
January. Polar stratospheric clouds (PSCs)
are formed in the polar ozone layer when
winter minimum temperatures fall below
the formation temperature of about −78°C.
This occurs on average for 1 to 2 months
over the Arctic and 5 to 6 months over
Antarctica (see heavy red and blue lines).
Reactions on liquid and solid PSC particles
cause the highly reactive chlorine gas ClO
to be formed, which catalytically destroys
ozone (see Q9). The range of winter minimum temperatures found in the Arctic is
much greater than in the Antarctic. In some
years, PSC formation temperatures are not
reached in the Arctic, and significant ozone
depletion does not occur. In contrast, PSC formation temperatures are always present for many months somewhere in the
Antarctic, and severe ozone depletion now occurs in each winter season (see Q11). (Note that the dashed black lines denote
the upper limits of the Antarctic temperature range where they overlap with the Arctic temperature range.)
Answer:
Explanation:The answer is essentially 'because of the weather in the ozone layer'. In order for rapid ozone destruction to happen, clouds (known as PSCs, Stratospheric Clouds Mother of Pearl or Nacreous Clouds) have to form in the ozone layer. In these clouds surface chemistry takes place. This converts chlorine or bromine (from CFCs and other ozone depleting chemicals) into an active form, so that when there is sunlight, ozone is rapidly destroyed.