What Will Happen if Climate Variability and Change Cause Glacier and Polar Ice Cap Melting
This activity is one of a series in the collection, The Potential Consequences of Climate Variability and Change activities.
It engages students in modeling how increased temperatures hasten the melting of ice in the environment, contributing to a rise in sea level and subsequent flooding of coastal areas.
Credit: Institute for Global Environmental Strategies
- Two small aquarium tanks, a glass cover (a plastic cover or plastic food-wrap will work, but should not come in direct contact with the lamp)
- Two clamp lamps with 60-watt bulbs
- Tinted plastic wrap or transparency paper
- Blue food coloring (optional)
- “Icebergs” and “glaciers” (freeze water in paper cups or milk cartons; peel off paper)
- Grease pencil or marker (optional)
- Graph paper
- Student Activity Three lab sheet
Set up Tank 1 and Tank 2 as in Activity One. Add blue food coloring to the water (optional) and carefully pour into the tank. Take a baseline temperature. Measure the water level in the tank. (You may wish to tape a ruler to the front of the tank and mark the water level on the tank glass with a grease pencil or marker.) Record data on the Student Activity Three Lab Sheets for Tanks 1 and 2.
Explain the difference between glaciers and icebergs to the students. Then place one or more “icebergs” and “glaciers” in your tanks (see Figure 3). Note the rise in the water level with the introduction of the ice. Draw a diagram of the tank and measure and record the new temperature and water height on the Student Activity Three Lab Sheets for Tanks 1 and 2.
Place a lamp over Tank 1. Place a glass cover, plastic wrap, and a lamp over Tank 2. (NOTE: Place the plastic wrap material around the lamp bell, not under it. CAUTION: Material in direct contact with the bare bulb may catch fire. Explain to the students this is only being done to prevent the plastic wrap from catching on fire. In the “real” atmosphere, the sun’s rays pass directly through the atmosphere.) Record the temperature and water level changes in the tanks at 1, 5, 10, 30, and 60-minute intervals on the lab sheets.
Complete lab sheets.
Supported NGSS Performance Expectations
Supported Common Core Math
- CC.3.MD.1 Solve problems involving measurement and estimation of intervals of time, liquid volumes, and masses of objects. Tell and write time to the nearest minute and measure time intervals in minutes. Solve word problems involving addition and subtract
- CC.3.MD.4 Represent and interpret data. Generate measurement data by measuring lengths using rulers marked with halves and fourths of an inch. Show the data by making a line plot, where the horizontal scale is marked off in appropriate units—whole numbe
- CC.4.MD.4 Represent and interpret data. Make a line plot to display a data set of measurements in fractions of a unit (1/2, 1/4, 1/8). Solve problems involving addition and subtraction of fractions by using information presented in line plots. For example
- CC.5.MD.2 Represent and interpret data. Make a line plot to display a data set of measurements in fractions of a unit (1/2, 1/4, 1/8). Use operations on fractions for this grade to solve problems involving information presented in line plots. For example,
- Observe and describe changes of the Cryosphere model as variables are changed;
- Explain the relationship between the models and the real world
- Make predictions about future climate changes and some of their potential impacts on Earth
- How do I recognize a change in the Cryosphere?
- How does change in the Cryosphere affect changes in other parts of the Earth System?
- To effectively teach about the effects of climate variability and change, teachers should have a solid understanding of the following concepts:
- The sun provides the heat and light energy that sustains life on Earth. It creates the weather we experience daily (for example, the cycle of precipitation and wind patterns) and the climate characteristics of the place where we live (tropical, sub-tropical, temperate, and polar regions).
- The atmosphere, which is virtually transparent to incoming sunlight, surrounds the Earth and helps trap heat near the Earth ’s surface, much as the glass over a greenhouse traps heat. Without our atmospheric “blanket, “the Earth would be about 60 degrees F cooler in every season.
- The atmosphere consists of many kinds of molecules (nitrogen, oxygen, carbon dioxide, aerosols including water vapor, and others). These molecules absorb, emit, transmit, and reflect heat and light energy.
- Combustion, exhaust, and other by-products of human activities (aerosols) are contributing to the changing mix of molecules in the atmosphere. This change is causing our atmosphere to hold in more heat energy and has raised temperatures in every climate zone.
- A glacier is a large mass of ice formed on land. An iceberg is a large piece of ice that has broken off from a glacier and dropped into a large body of water. About 4/5 to 8/9 of an iceberg is below the water.
- Keep in mind that melting icebergs will not cause a rise in sea level since they are already in the ocean. Melting glaciers, on the other hand, will cause a sea level rise, since they are land-based.
- Rising temperatures may cause changes in the Earth’s climate. Effects might include drought, torrential rains, flooding, rising sea levels, and depletion of groundwater. More positive effects could be increased plant production or warmer winters in northern cities.
- IMPORTANT: The enclosed lab sheets are to be used by Grade 3–4 students, and by 1–2 teachers to help organize their own observations and guide their discussions with students who have limited reading and calculating skills.
- NOTE: These activities deal only with the effects of aerosols and gases on the Earth’s temperature. The effect of albedo, due to cloud cover, is not discussed.
Students must have the following skills and knowledge to complete this activity:
- The sun’s heat creates our weather. It drives the water cycle and wind patterns. Students need to understand the basics of the water cycle, especially the concepts of evaporation and precipitation.
- “Air is there. “It consists of gas molecules and has mass. A simple way to demonstrate this idea is to show your students an “empty” paper lunch bag. When you ask them what is inside, most students will answer, “Nothing.” Next, face each student with the opening of the bag about 18 inches from his or her face. Then, clap the bag between your hands. This forces air out of the bag and “squirts “the student with “nothing. “Now if you ask what was in the bag, your students will answer, “Air.”
- The atmosphere consists of a mixture of molecules. It acts like a blanket to keep the Earth warm enough for us to live. Most of the components of our atmosphere are there naturally, but the activities of people living and working on the Earth have changed the mixture of gases and particles, increasing the amount of heat-trapping gases in the atmosphere. It is much like adding more blankets to your bed at night. The more blankets you add, the warmer you become. The more heat-trapping gases there are in the atmosphere, the more of the sun ’s energy it traps and the higher the temperatures rise.
- Weather is what happens outdoors every- day, whereas climate is the average weather in a particular place over the seasons of the year. Your students should be able to show which zones of the Earth are tropical, subtropical, temperate, and polar.
Located in the Arctic near the North Pole, Greenland is covered by a massive ice sheet three times the size of Texas and a mile deep on average. Greenland is warming almost twice as fast as Antarctica, which is causing the ice to melt and raise global sea levels. NASA is monitoring Greenland’s ice sheet from high up in space to the ocean floor below to provide data for scientists studying the global impact of all its melting ice.
The creation of ICESat-2 is allowing NASA's scientists to make accurate maps of polar ice sheets. These maps help them make informed predictions about weather patterns, climate change, and the effects of changing ice structures. The maps are so accurate they can measure to within 3 centimeters of an ice sheet's actual thickness from a huge distance!
Learn how the second generation of the Ice, Cloud, and Land Elevation Satellite, better known as ICESat-2, is being used to map the ice structures in the world's polar regions. Manipulating the distribution of photons by lasers to create accurate images of these frozen structures allows scientists to study their changes and impact on Earth's climate.
- Research and discuss how and where glaciers form. How would these conditions and regions be affected by climate variability and change?
- Have the students compare the glaciers with the icebergs from their activity. What makes them different? Where do icebergs come from? Ask the students to predict what would happen to an iceberg as it floats in the ocean.