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Name Period Date Investigating Climate Change at the Micro and Macroscopic Level Objectives Discover some causes and effects of increasing global temperature. Determine the environmental factors that.

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Follow the steps to successfully complete the answer key.

  1. Click ‘Get Form’ button to obtain the form and open it in the editor.
  2. 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.
  3. 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.
  4. 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.
  5. Next, address the relationship between average temperature and the glacier's movement/thickness, including supporting evidence from the data gathered during the simulation.
  6. 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.
  7. 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.
  8. Build an atmosphere with varied gas compositions and note the effects on infrared and visible photons. Relate your observations back to the greenhouse effect.
  9. In Part C, synthesize your findings from both simulations to draw connections between microscopic observations and macroscopic phenomena related to climate change.
  10. 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.

Start filling out your Investigating Climate Change At The Micro And Macroscopic Level Answer Key online today!

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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.

More frequent and intense drought, storms, heat waves, rising sea levels, melting glaciers and warming oceans can directly harm animals, destroy the places they live, and wreak havoc on people's livelihoods and communities. As climate change worsens, dangerous weather events are becoming more frequent or severe.

Burning fossil fuels, cutting down forests and farming livestock are increasingly influencing the climate and the earth's temperature.

Global warming is a process of the Earth's temperature rising, due to radiation from sunlight that is being trapped in the earth by greenhouse gases such as methane and carbon dioxide. The process starts with the greenhouse gases allowing the sunlight to access the Earth; letting the necessary amount in.

10 Causes of Global Warming #1. Power plants. ... #2. Agriculture. ... #3. Vehicles and transport. ... #4. Landfills. ... #5. Offshore drilling. ... #6. Fracking. ... #7. Deforestation. ... #8. Overfishing.

Causes of Climate Change Heat-trapping Greenhouse Gases And The Earth's Climate. ... Greenhouse Gases. ... Reflectivity or Absorption of the Sun's Energy. ... Changes in the Earth's Orbit and Rotation. ... Variations in Solar Activity. ... Changes in the Earth's Reflectivity. ... Volcanic Activity.

Earth-orbiting satellites and new technologies have helped scientists see the big picture, collecting many different types of information about our planet and its climate all over the world. These data, collected over many years, reveal the signs and patterns of a changing climate.

Ice cores are scientists' best source for historical climate data.

Ancient air bubbles trapped in ice enable us to step back in time and see what Earth's atmosphere, and climate, were like in the distant past. They tell us that levels of carbon dioxide (CO2) in the atmosphere are higher than they have been at any time in the past 400,000 years.

The consequences of climate change now include, among others, intense droughts, water scarcity, severe fires, rising sea levels, flooding, melting polar ice, catastrophic storms and declining biodiversity.

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