Lulla, Kamlesh P. Ph.D.Earth From Space.NASA, 2000

The Ozone Layer: An Introduction

The ozone layer is a layer of gas, which is made up of three oxygen atoms.It is created when oxygen gas is broken down by sunlight.The oxygen molecules that are apart bond to other molecules and form ozone.The Ozone is broken down as well to form oxygen gas.This cycle is how ozone maintains the same amount.Ozone is extremely poisonous, however, even when breathing a very small amount of the gas.Ozone gas does help in the prevention of Ultraviolet sunrays getting through the atmosphere, which are harmful to humans.

Global Warming

Environmental Protection Agency, 2000

Global warming is what happens when the ozone layer breaks down and Ultraviolet rays are allowed to enter the Earth’s atmosphere.This event is called the Greenhouse effect.Holes in the ozone layer allow Ultraviolet rays to come into the atmosphere, and then are trapped by ozone gases such as water vapor and carbon dioxide.Without this trapping of heat energy, climates and temperatures in the world would be much cooler and life on earth could not survive.Global Warming, however, is a case in which the ozone layer has too large of holes in it, and too much UV rays are getting through, thereby trapping too much energy and extremely heating up the Earth’s surface and atmosphere.Below are effects of the so-called global warming.

Sea Level Rise                      Global Temperatures                     Precipitation Increase

Sea Level Rise

One cause of global warming in the atmosphere is the rise of the sea level.The sea level has risen about 6-8 inches in the past century.About 1-2 of those inches of sea level rise came from the melting of mountain glaciers.Another 1-2 inches of sea level rise came from the expansion of oceanic water due to the increase in temperature from global warming.On the U.S. coast, there is a rise of about 3 millimeters of water per year.

 

Environmental Protection Agency, 2000

Global Temperatures

Temperatures around the globe have also risen, to an estimated 0.8-1.0° F Over the last century.This could be an effect of global warming, which is what scientists are estimating.There are differences in the climate changes though, like in areas of Canada and Alaska, where winters there are rising more so than the summers.Also, nighttime temperatures are rising about twice as fast as the daytime temperatures.This global increase in temperatures has more steeply taken place from 1900-1940.The temperature increase came more slowly in the years of 1940-1970, but has picked up again in the last 25 years.These increases show what could be an indicator to the effects of global warming.

Precipitation Increase

An increase in precipitation has also showed where the world has gained about one percent of precipitation in the last century.The high latitude areas are gaining in precipitation; however, the tropical areas are in fact loosing a little precipitation.Among these facts, rainfall has increased in North America by about five percent in the last century, and along the northern states and southern Canada, the increase is at around 10-15 percent.Rainfall is found to be increasing more between September and November, and is showing to be coming down in harder downpours than normal.

 

 

Johannes-Kepler-Gymnasium Reutlingen.The Ozone Layer.The Ozone Layer.[Online].Available: www.schwaben.de/home/kepi/ozone2.htm.[April 10, 2000]

 

Environmental Protection Agency.Global Warming.Environmental Protection Agency.[Online].Available: www.epa.gov/globalwarming.[April 10, 2000]

 

Introduction picture taken from:

Lulla, Kamlesh P. Ph.D.Earth From Space.NASA.[Online].Available: earth.jsc.nasa.gov.[April 10, 2000].

This web page was created by Ryan Rondo and Dr. Todd M. Hamilton for Chemistry 299, Computers in Science, Adrian College, Spring 2000.