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How to fill out the Investigating Climate Change At The Micro And Macroscopic Level Answer Key online
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- Click ‘Get Form’ button to obtain the form and open it in the editor.
- Begin by filling in your name, period, and date at the top of the form. Ensure that these details are accurate as they serve to identify your submission.
- In Part A, engage with the PhET Glaciers simulation for five minutes. Record your observations in the provided table based on the parameters you adjust. Make sure to note changes in glacier movement and thickness.
- For the claims section regarding snowfall, articulate the relationship between average annual snowfall and glacier movement/thickness. Support your claims with evidence drawn from your observations.
- Next, address the relationship between average temperature and the glacier's movement/thickness, including supporting evidence from the data gathered during the simulation.
- Proceed to Part B, where you will explore the PhET Greenhouse Effect simulation for five minutes. Document your findings in the designated table, particularly noting the effects of different greenhouse gas concentrations.
- Analyze the interaction between different molecules and light in the Photon Absorption Tab and identify which gases qualify as greenhouse gases based on your findings.
- Build an atmosphere with varied gas compositions and note the effects on infrared and visible photons. Relate your observations back to the greenhouse effect.
- In Part C, synthesize your findings from both simulations to draw connections between microscopic observations and macroscopic phenomena related to climate change.
- Once you have completed all sections, review your responses for accuracy before saving your changes. You can then download or print the document as needed, or share it as required.
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Ice cores drawn from Greenland, Antarctica, and tropical mountain glaciers show that Earth's climate responds to changes in greenhouse gas levels. Ancient evidence can also be found in tree rings, ocean sediments, coral reefs, and layers of sedimentary rocks.
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