The Greenhouse Effekt

The greenhouse effect is the warming of climate that results when the atmosphere traps heat radiating from Earth toward space. Certain gases in the atmosphere resemble glass in a greenhouse, allowing sunlight to pass into the greenhouse, but blocking Earths heat from escaping into space. The gases that contribute to the greenhouse effect include water vapor, carbon dioxide (CO2), methane, nitrous oxides, and chlorofluorocarbons (CFCs). Life on Earth depends on energy coming from the Sun. About half the light reaching Earths atmosphere passes through the air and clouds to the surface, where it is absorbed and then radiated upward in the form of infrared heat. About 90 percent of this heat is then absorbed by the greenhouse gases and radiated back toward the surface, which is warmed to a life-supporting average of 59 dedrees Fahrenheit (F) (15 degrees Celsius (C). On Earth, human activities are changing the natural greenhouse. Over the last century the burning of fossil fuels like coal and oil has increased the concentration of atmospheric CO2. This happens because the coal or oil burning process combines carbon (C) with oxygen (O2) in the air to make CO2. To a lesser extent, the clearing of land for agriculture, industry, and other human activities have increased the concentrations of other greenhouse gases like methane (CH4), and further increased (CO2). The consequences of changing the natural atmospheric greenhouse are difficult to predict, but certain effects seem likely: * On average, Earth will become warmer. Some regions may welcome warmer temperatures, but others may not. * Warmer conditions will probably lead to more evaporation and precipitation overall, but individual regions will vary, some becoming wetter and others dryer. * A stronger greenhouse effect will probably warm the oceans and partially melt glaciers and other ice, increasing sea level. Ocean water also will expand if it warms, contributing to further sea level rise. * Meanwhile, some crops and other plants may respond favorably to increased atmospheric CO2, growing more vigorously and using water more efficiently. At the same time, higher temperatures and shifting climate patterns may change the areas where crops grow best and affect the makeup of natural plant communities. Human Activities Add to Atmospheric (CO2) Atmospheric CO2 has increased about 25 percent since the early 1 800s. Climatologists at NASAs Goddard Space Flight Center, Greenbelt, Md., estimate the increase since 1958 has been about 10 percent. Currently, the level of atmospheric C 2 is increasing at a rate of about 0. 4 percent a year. Human beings add CO2 to the atmosphere mainly by burning fossil fuels like coal and oil. Deforestation is the second major way we increase atmospheric CO2. Felled timber releases CO2 as it burns or decays, and disturbed soils produce CO2 from burned organic matter. Forests give way largely to annual crops that store CO2 for only a season ...