Journal of a Sabbatical

the ozone hole

May 7, 1997




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cats

Fufi, Zeus, and Sammy all got adopted since last week. A crew from Channel 7 was at the shelter today interviewing Stacy about feral cats and strays. They filmed some of the cats, including Jaguar, Quincy, and Susie. Filming while we were cleaning slowed things down quite a bit and I had a distinctly workaholic moment when I realized that I resented them for keeping me from getting work done. I ended up leaving early because I'd forgotten to take Motrin for the mysterious knee thing and after standing still washing dishes after being up and down cleaning cages the stupid knee hurt a lot. There must be more to say about the whole cat thing but as I noticed yesterday, my writing is becoming pedestrian.

spell checker

I installed Claris Home Page 2.0 yesterday (it came included with ClarisWorks). Not only does it fix the annoying bugs in 1.0 but it also has a spell checker. So I ran all of March, April and May entries through it just to clean up my typos. Much to my surprise, the spell checker did not recognize: dyke, fuchsia, zooplankton, and a couple of other words I can't remember right now. I can forgive it zooplankton on the grounds that it's a specialized term, but dyke and fuchsia? Give me a break!

the ozone hole

I turned in my paper on the effect of the Antarctic ozone hole on icefish larvae and took the final exam tonight so Oceanography is over for the year except for the field trip to take bottom samples and water samples in Dorchester Bay on Friday. Boy is that a long sentence and awkward!

What you may ask is the ozone hole? And what does it mean to you? I know you all want to know.

The Ozone Layer.

Ozone occurs naturally in the earth's stratosphere. This layer of ozone is what allowed the oceans to form and life to evolve on earth. Before the atmospheric ozone layer, life was possible only in the ocean depths where the seawater absorbed the sun's ultraviolet radiation . Starting about 600 million years ago, oxygen began to build up in the atmosphere as a result of photosynthesis. Ozone is chemically formed from oxygen. As oxygen levels increased, ozone levels increased until there was enough ozone in the atmosphere to absorb effectively the ultraviolet (UV) radiation coming from the sun. Only with this protection, could living organisms emerge from the oceans to live on land.

Ozone and UV-B Radiation.

The key role of the ozone layer is to filter out radiation in the middle of the UV spectrum, which includes UV-B. UV-B is the most biologically damaging part of the UV spectrum. These midrange wavelengths are the ones responsible for health problems in humans, plants, livestock, marine life, etc. DNA absorbs UV-B light and the absorbed energy can break bonds in the DNA.

The Ozone Hole.

The ozone layer has been thinning over the past twenty years. Satellite measurements of ozone started in the early 70's, but the first comprehensive worldwide measurements started in 1978. (Ground based measurements of Ozone were first started in 1956.) Ozone depletion is most dramatic over Antarctica. Each year since 1979, the ozone layer thins dramatically over Antarctica. In the 1980's scientists had predicted about a 7% decline over a 60 year period. Ozone levels have fallen gradually in the more temperate latitudes as predicted. However, the satellite data showed a greater than 50% depletion of the ozone layer over Antarctica that recurs each austral spring for about 10 to 12 weeks. This 50% decline in ozone concentrations over Antarctica is referred to as the Antarctic ozone hole.

There, that wasn't so bad, was it?

 

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