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Ground Truth Studies Teacher Handbook - Aspen Global Change ...

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A <strong>Global</strong> <strong>Change</strong> Primer (continued)<br />

wonder chemicals. The chlorine from CFCs, and the bromine from halons, destroy<br />

stratospheric ozone molecules, and each atom of these elements can destroy<br />

thousands of ozone molecules.<br />

The Ozone Hole<br />

In the 1970s, two scientists predicted that CFCs would cause a global decline in<br />

stratospheric ozone. Years later satellite sensors recorded a drop in ozone over<br />

Antarctica, and even flagged the lowest values, but the ozone levels were so low,<br />

they were outside the range the computers had been programmed to accept as valid<br />

data and so the early warning was missed. Looking back at the data revealed that in<br />

1984, the unsuspected ozone hole was already larger than the continental U.S. By<br />

1987, the average ozone concentration over the South Pole was down 50%; during<br />

springtime it was down 70%, and in some spots, had essentially disappeared<br />

altogether. By 1992, the ozone hole had grown in area to nearly three times the size<br />

of the continental U.S. Though scientists had predicted the global decline in<br />

stratospheric ozone, no one had anticipated that ozone loss would appear so<br />

dramatically and suddenly in the form of a “hole” in the ozone layer over Antarctica.<br />

1979<br />

1980<br />

1981<br />

1982<br />

< 390 DU<br />

< 240 DU<br />

Concentration<br />

< 240 DU<br />

< 390 DU<br />

If chlorine and bromine from CFCs and halons released from populated areas cause<br />

ozone destruction, then why is the ozone hole at the South Pole? The CFCs and<br />

halon sources are primarily from the mid-latitudes and after their release are<br />

transported by convection to the upper atmosphere and eventually the stratosphere.<br />

There are a couple of unique features that make the stratosphere over the poles<br />

particularly the South Pole more susceptible: First, Antarctica and the air above it<br />

is extremely cold and this leads to the formation of Polar Stratospheric Clouds<br />

(PSCs). Tiny ice crystals in PSCs provide chemically-active sites where the<br />

chlorine and bromine can catalyze the breakup of the ozone. The other feature is<br />

the polar vortex, a spiral of winds that swirls around the South Pole, isolating the<br />

Antarctic stratosphere during the winter and early Spring so the ozone destruction<br />

process goes on without Antarctic ozone being replenished by ozone rich air from<br />

lower latitudes.<br />

1983<br />

1984<br />

1985 1985<br />

<strong>Global</strong> Ozone Depletion<br />

But ozone losses are not confined to the South Pole. In 1988, over 100 international<br />

experts reported that the ozone layer around the entire globe was eroding much<br />

faster than anticipated. Between 1969 and 1986, the average global concentration<br />

of ozone in the stratosphere had fallen by approximately 2%. By 1991, losses of 6<br />

to 8% per decade had been measured at high latitudes (nearer to the poles) and<br />

Figure 7<br />

These pictures show the<br />

increase in size of the Antarctic<br />

ozone hole during successive<br />

winters. October monthly<br />

average TOMS total O 3<br />

. The<br />

crosses indicate South Pole.<br />

© ASPEN GLOBAL CHANGE INSTITUTE 1995 GROUND TRUTH STUDIES<br />

25

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