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5. Conclusions

Ultraviolet radiation is a small but significant portion of the Sun’s output. Its effects on humans is neutral or beneficial in small doses (Vitamin D formation), but exposure to higher levels may produce a painful or even life-threatening sunburn. Chronic exposure to ultraviolet radiation is associated with increased aging of the skin as well as skin cancers and cataracts.

Stratospheric ozone protects us and many living things from high levels of ultraviolet radiation. Unfortunately, chlorofluorocarbons and similar compounds destroy stratospheric ozone as demonstrated by the development of a dramatic seasonal ozone hole over Antarctica. Fortunately, this was recognized in a reasonably timely fashion, and these compounds are no longer being manufactured or used to anywhere near their previous levels; hopefully, they will not contribute further damage to the ozone layer.

Where this will all end in the next 50 to 100 years and what more we should be doing about it are interesting and important questions far beyond the scope of this essay. Let us hope they are properly answered in enough time for us to mitigate and reverse any unintentional damage we have ignorantly done to our protective atmosphere.


References

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American Academy of Dermatology (AAD) web site at: http://www.aad.org/public/DermatologyA-Z/Index.htm. 2006.

Aura mission. Web pages at: http://aura.gsfc.nasa.gov/. and http://www.nasa.gov/mission_pages/aura/main/index.html.

Australian Government Bureau of Meteorology (Austr. Gov) web site at: http://www.bom.gov.au/announcements/uv/. 2006.

Brannon H. About Health and Fitness web site. UVA radiation. Web essay at: http://dermatology.about.com/cs/agingskin/g/uva.htm. 2006.

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Dorland's Illustrated Medical Dictionary. 26th Edition, W.B. Saunders, Co., 1981, Philadelphia.

U.S. Environmental Protection Agency (EPS) SunWise Program at: http://www.epa.gov/sunwise/glossary.html#du.

Ferrini RL, Perlman M, Hill L. Skin protection from ultraviolet light exposure. American College of Preventive Medicine Practice Policy Statement at: http://www.acpm.org/skinprot.htm. 1998.

Foster J. Sunburn. Emedicine web essay at: http://www.emedicine.com/emerg/topic798.htm. October 24, 2005.

Gardner E, Gray DJ, O’Rahilly. Anatomy, W.B. Saunders Co., 1963, Philadelphia, pages 72-81.

Goodsell DS. The Oncologist Web Site. Web essay. The molecular perspective: ultraviolet light and pyrimidine dimers at: http://theoncologist.alphamedpress.org/cgi/content/full/6/3/298. June 2001.

McKenzie R, Connor B, Bodeker. Increased summertime UV radiation in New Zealand in response to ozone loss. Science 10 September 1999; 285: 1709-1711.

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National Oceanic and Atmospheric Administration (NOAA) / Environmental Protection Agency (EPA). NOAA/EPA Ultraviolet Index/UVI/ Forecast at: http://iwin.nws.noaa.gov/iwin/us/ultraviolet.html. 2006.

NOAA Frequently Asked Questions (FAQ) about ozone at: http://www.ndsc.ncep.noaa.gov/news/freq_qu/faq1.html 1998.

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Notes

[1] Ultraviolet light was discovered by Johann Wilhelm Ritter (1776-1810) in 1801 after hearing of William Herschel’s discovery of infrared light beyond the red end of the visible spectrum.  Ritter noted blue light caused silver chloride to turn black more efficiently than red light.  He also discovered that “light” beyond the violet portion of the visible spectrum displayed an intense reaction in this regard.  From: http://coolcosmos.ipac.caltech.edu//cosmic_classroom/classroom_activities/ritter_bio.html.

[2] UVA, UVB, and UVC are sometimes used in a hyphenated form, such as UV-B.

[3] “Germicidal” or “bactericidal” agents are chemicals, medications, or forms of radiation that kill bacteria.  These agents often kill viruses as well.  Bacteriostatic agents are those which stop the growth of bacteria but do not necessarily kill them. 

[4] “Acute” is a medical term for a rapid (minutes to hours) effect while “chronic” is a medical term for a long duration (weeks to months) effect. 

[5] Inflammation is a term used since ancient times to describe a combination of redness, swelling, pain, and heat in an area subject to physical, chemical, or infectious injury.  It is part of the body’s response to injury, and it is the first part of the healing mechanism.  It is mediated through a complex system of chemicals released from injured cells, chemicals and cells brought to the injured area via the blood stream, and cells that make their own way to the injured area through cellular locomotion. 

[6] Vitamin D consists of a complex group of hormones that help regulate body levels of calcium and phosphorus which in turn controls the mineralization of bone.  Individuals with adequate exposures to sunlight do not require dietary vitamin D.  Lack of vitamin D leads to various childhood and adult diseases, such as rickets.

[7] In 1839 Christian Schonbein (1799-1868) smelled a previously unknown component of air during electrolysis of water, ascribing this smell to a new compound he called “ozone” which means ill-smelling in Greek.  Jacques-Louis Soret (1827-1890) in 1864 recognized the structure of ozone (the dioxide of the O atom).  From Crutzen (2000).

[8] The troposphere is the lowest level of the Earth’s atmosphere.  It extends up to a height of approximately 10 to 15 km, and its temperature decreases steadily with altitude.  The troposphere and the stratosphere were named by Leon-Philippe Teisserenc de Bort (1855-1913) in 1902 after years of atmospheric measurements with unmanned balloons. He found that at altitudes above 8-10 km the temperature did not decline further.  He called the region of more constant temperature maintained by the ozone absorption of Solar UVR the “stratosphere” and the region below it the “troposphere.”  The tropopause is the region where the temperature remains constant before increasing in the stratosphere.  Teisserenc’s balloons only reached the tropopause and did advance into the stratosphere.  From: Crutzen (2000).

[9] At Oxford G.M.B. Dobson (1889-1976) together with F.A. Lindemann (1886-1957) (later Lord Cherwell) studied meteor trails from which they deduced the temperature profile above the troposphere was not constant.  Dobson followed on earlier work of Charles Fabry (1867-1945) and Henri Buisson (1873-1944) and measured ozone by observing its absorption in the Solar ultraviolet spectrum.  He was conferred the title of Oxford Professor in 1945, and his work with Alan Brewer led to the Brewer-Dobson Circulation model for the stratosphere.  From: http://www-atm.physics.ox.ac.uk/user/barnett/ozoneconference/dobson.htm. and other sources.

[10] The official name for this treaty is The Montreal Protocol on Substances That Deplete the Ozone Layer.  It was originally signed in 1987 and substantially amended in 1990 and 1992.  The Vienna Convention for the Protection of the Ozone Layer (1985) established the framework for the later Montreal Protocol.  From: http://www.ciesin.org/TG/PI/POLICY/montpro.html

[11] Halons are hydrocarbon compounds containing a combination of fluorine, chlorine, or bromine substituted for some or all of the hydrogen atoms.  They are mainly used in fire extinguishers.  Carbon tetrachloride was formally used as an aerosol can propellant, a solvent, a cleaning fluid, and in fire extinguishers. It is carcinogenic and can cause liver, kidney, and nervous system damage.  Methyl chloroform is used as a solvent for adhesives and for metal degreasing as well as a dry cleaning agent.

Essay posted Sunday 11 March 2007

 

 

 

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