This lesson is a lab in which students use thermometers, white and …
This lesson is a lab in which students use thermometers, white and dark paper, and lamps to measure differences in albedo between the light and dark materials. Connections are made to albedo in Antarctica.
In this activity students learn how Earth's energy balance is regulating climate. …
In this activity students learn how Earth's energy balance is regulating climate. This activity is lesson 4 in the nine-lesson module Visualizing and Understanding the Science of Climate Change.
Students analyze and interpret graphs to compare the flow of shortwave energy …
Students analyze and interpret graphs to compare the flow of shortwave energy from the Sun toward China over the course of a year on cloudy versus clear days.
This is a STEM activity to learn how different colors absorb light …
This is a STEM activity to learn how different colors absorb light better than others. Vocabulary and investigating questions are included to facilitate discussion, and a rubric is provided for assessment.
This interactive visualization adapted from NASA and the U.S. Geological Survey illustrates …
This interactive visualization adapted from NASA and the U.S. Geological Survey illustrates the concept of albedo, which is the measure of how much solar radiation is reflected from Earth's surface.
Students perform a lab to explore how the color of materials at …
Students perform a lab to explore how the color of materials at Earth's surface affect the amount of warming. Topics covered include developing a hypothesis, collecting data, and making interpretations to explain why dark-colored materials become hotter.
Hands-on laboratory activity that allows students to investigate the effects of distance …
Hands-on laboratory activity that allows students to investigate the effects of distance and angle on the input of solar radiation at Earth's surface, the role played by albedo, the heat capacity of land and water, and how these cause the seasons. Students predict radiative heating based on simple geometry and experiment to test their hypotheses.
This activity introduces students to different forms of energy, energy transformations, energy …
This activity introduces students to different forms of energy, energy transformations, energy storage, and the flow of energy through systems. Students learn that most energy can be traced back to nuclear fusion on the sun.
This 15-panel interactive from NOVA Online describes some of the factors (such …
This 15-panel interactive from NOVA Online describes some of the factors (such as Earth's rotation and the sun's uneven heating of Earth's surface) contributing to the formation of the high-speed eastward flows of the jet streams, found near the top of the troposphere. These jet streams play a major role in guiding weather systems.
A simple click-through animation from Scripps Institute's Earthguide program breaks the complex …
A simple click-through animation from Scripps Institute's Earthguide program breaks the complex topic of the global energy balance into separate concepts. Slides describe the different pathways for incoming and outgoing radiation.
Build your own miniature "greenhouse" out of a plastic container and plastic …
Build your own miniature "greenhouse" out of a plastic container and plastic wrap, and fill it with different things such as dirt and sand to observe the effect this has on temperature. Monitor the temperature using temperature probes and digitally plot the data on the graphs provided in the activity.
Explore how the Earth's atmosphere affects the energy balance between incoming and …
Explore how the Earth's atmosphere affects the energy balance between incoming and outgoing radiation. Using an interactive model, adjust realistic parameters such as how many clouds are present or how much carbon dioxide is in the air, and watch how these factors affect the global temperature.
This is a kinesthetic activity that demonstrates how shortwave radiation emitted by …
This is a kinesthetic activity that demonstrates how shortwave radiation emitted by the sun and longwave thermal radiation emitted by the earth interact differently in the atmosphere. It allows students to experience this difference and reinforces their understanding of greenhouse gases as well. Students should have an understanding of shortwave and longwave thermal radiation and of greenhouse gases before doing this activity, but there is a minimal amount of background information about those topics included in this pdf. Additional resources/background info for teachers can be found on the website for the Little Shop of Physics.
This is the first of nine lessons in the Visualizing and Understanding …
This is the first of nine lessons in the Visualizing and Understanding the Science of Climate Change website. This lesson is an introduction to Earth's climate and covers key principles regarding Earth's unique climate, atmosphere, and regional and temporal climate differences.
This activity introduces students to the process of converting sunlight into electricity …
This activity introduces students to the process of converting sunlight into electricity through the use of photovoltaics (solar cells). Students complete a reading passage with questions and an inquiry lab using small photovoltaic cells.
Students gain experience using a spreadsheet and working with others to decide …
Students gain experience using a spreadsheet and working with others to decide how to conduct their model 'experiments' with the NASA GEEBITT (Global Equilibrium Energy Balance Interactive Tinker Toy). This activity helps students become more familiar with the physical processes that made Earth's early climate so different from that of today. Students also acquire first-hand experience with a limitation in modeling, specifically, parameterization of critical processes.
In this activity, learners use the STELLA box modeling software to determine …
In this activity, learners use the STELLA box modeling software to determine Earth's temperature based on incoming solar radiation and outgoing terrestrial radiation. Starting with a simple black body model, the exercise gradually adds complexity by incorporating albedo, then a 1-layer atmosphere, then a 2-layer atmosphere, and finally a complex atmosphere with latent and sensible heat fluxes. With each step, students compare the modeled surface temperature to Earth's actual surface temperature, thereby providing a check on how well each increasingly complex model captures the physics of the actual system.
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