EDUCATION: GLOBAL METHANE INVENTORYLesson 1-1: The Role of the Atmosphere and Greenhouse Effect in Determining the Surface Temperature of the EarthThe following lesson is a Methane Project Interactive Lesson. SpecificationsTime: 2 to 3 class periods Learning ObjectivesAt the end of this lesson, students will be able to:
CreditsDeveloped at the Institute on Climate and Planets, NASA Goddard Institute for Space Studies by Harvey Augenbraun, Teacher of Earth Science, The Mott Hall School, I. S. 223 (Grades 4-8), New York City, August 1997. The interactive courseware module for this lesson was created by Samuel Borenstein, Professor of Physics York College, City University of New York. Using the Interactive SoftwareTo use the interactive courseware module described in this lesson, you will need:
Science ContentThe Greenhouse Effect is an important and timely topic in the study of Earth science. In topic 1 the student will use an interactive computer module to investigate the nature of the natural greenhouse effect and its effect on making the Earth a habitable planet. By looking at the relationship between insolation at the Earth's surface and radiation of infra energy from the surface, the student will investigate:
At the completion of this section the student will determine that the greenhouse effect is natural and necessary for making the Earth a habitable planet. Continuing with this module, students will investigate historical changes and trends in greenhouse gas concentrations, both natural and anthropogenic (created by people), for the pre- and post-industrial era. They will also investigate:
At the completion of this section, students will discover that greenhouse gases vary naturally. They will also discover the human influence on changing rates of increase in greenhouse gas concentrations during the post-industrial era. Science SkillsSkills used:
Students will interpret historical graphical data for atmospheric concentrations of greenhouse gases derived from analyses of ice core samples and more recent direct measurements of air. From this they will derive atmospheric concentrations of carbon dioxide and methane for 120,000 and 20,000 years ago and compute the percent change for each gas over the time period. These values may then be input to the computer program which will calculate the change in temperature that results*. They will repeat the procedure for the time period from 1800 to the present. From the analysis of these data the student will see that:
The student can predict what might occur to concentrations of greenhouse gases if present trends continue. As an optional activity they can vary the concentrations of these gases and use the program to compute temperature changes*. * The resulting temperatures are what would occur if the change in greenhouse gas(es) were the only factor. In reality there are other factors involved which produce the final surface temperature. Teacher Notes
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