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Climate Change Expedition

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Earth & Environmental Sciences

Students will analyze historical, long-term trends in climate and explore environmental processes to gain an understanding of weather and climate in Northern Canada.

In the first activity, students will go on a guided exploration to discover the ideal location to build a new Arctic weather research station. Students will re-create the deconstruction of an ice core sample to describe past climate. They will relate to their own experiences with local weather patterns to discuss the changing climate in the north. The workshop concludes with a discussion on the potential local and national impact of climate change and solutions to lessen our impact on the environment.

What You Need

Physical Requirements

  • Access to computer and projector for the PowerPoint presentation (optional).

Activity 1: Research Centre

Activity 2: Ice Cores 

Activity 3: Discussion 

Guide:

PowerPoint:

 

Safety Notes

Ensure you are familiar with Let's Talk Science's precautions with respect to safe delivery of virtual outreach to youth. These precautions can be found in the manual for this activity.

What To Do

Activity Prep

  • Print Climate or Weather? worksheet (1 per student), Ice Core worksheet (1 per student) and Risk Assessment worksheet (1 per student). 
  • Draw a blank graph on the classroom board for Activity 1A- Climate or Weather, with the date on the x-axis and average annual temperature on the y-axis. 

Introduction

  • Introduce the three main factors that contribute to weather: sun, air and water.
  • Ask students how the sun affects the weather.
    • The sun provides heat and light. 
    • The sun provides energy.
    • The sun powers the water cycle.
  • Either show the PowerPoint slide of the water cycle or draw it on the board as you talk about the different steps.
  • Explain the water cycle in terms of evaporation, condensation and precipitation. Ask the class to identify the three spheres involved in the water cycle.
    • Atmosphere (air surrounding the planet)
    • Lithosphere (the ground)
    • Hydrosphere (all water on/under the surface of the Earth)
  • Define climate and weather.
    • Discuss the climate in their community and compare it to other regions in Canada such as the Arctic or the equator. 
  • Discuss the different types of data scientists use to study climate. 
  • Explain how the cryosphere (includes many components that make up the Arctic environment) is very sensitive to the effects of climate change. Today they will be looking at data collected from Arctic research stations to observe if the data supports a changing climate. 

Activity 1: Research Centre

  • Separate students into groups of 3 to 4. Each group should have a calculator, a laminated Arctic map grid and a washable marker.
  • Explain the scenario: they are scientists that will be undergoing an important expedition in the Arctic to find a safe place to build a long-term research centre. 
  • Show a map of Canada (on PowerPoint) highlighting Cambridge Bay. 
  • The coloured squares on the Arctic maps represent:
    • Light blue: water that may or may not be frozen
    • Dark blue: open water
    • Brown: land mass 
    • White: Frozen ice patches
  • Have students predict a location on the map to build their research facility before receiving any scientific data or evidence of climate change. Students will mark this location on their map.

Activity 1A: Climate or Weather?

  • Give each group a bag containing 12 weather data chips, Climate or Weather? task card and Climate or Weather? worksheet. 
    • Each bag represents the weather for one year ranging between 1954-2013 (indicated by the colour of the chips).
  • Students will remove the weather chips out of the bag and record the temperature from each chip on their worksheet. 
  • As the students work through the data, draw a blank graph on the classroom board.
  • Students will decide what the average weather event was and calculate the average temperature for that time.
  • Ask students if this activity is an example of weather or climate. Is any one bag enough data to determine a climate?
  • Have one person from each group record their calculated average temperature for their year on the graph drawn on the classroom board.
    • The end result should be a graph containing the average annual temperature over 70 years. 
  • Display the weather graphics alongside the laminated map of the Arctic. Ask the following questions:
    • Is this enough data to determine the area for the new Arctic research site?
    • Does this graph contain enough data to identify a climate?
    • What is the overall trend on the graph? Is it changing? Do you see any outliers?

Activity 1B: Sea Ice Extent

  • Begin by showing Ice Thickness vs Date plot on PowerPoint slide.
  • Point to where the ice breaks and ice forms on the plot. 
  • Have students analyze the data for a few minutes- is there a trend?
    • If they say that the data trends downwards- discuss the amount of data present and if it is enough to be confident in that trend.
    • If they say that they notice that each year is different but similar- discuss the variability in weather when it comes to climate. 
  • Ask “what do the smaller and narrower peaks represent?”.
    • Small peaks represent thinner ice.
    • Narrow peaks represent a short freeze and thaw season.
    • It’s rare to see tall, short peaks because that would represent very thick ice being formed in a short amount of time- it takes time for ice to form.
  • Draw a bell curve on the classroom board and use two different coloured markers to show the difference in freezing (slow and gradual) and thawing (quick and steep). 
  • Discuss temperature and its role in the freeze/thaw cycle (feedback loop).
  • Refer back to the student’s map. Let them know that the map represents a winter month. 
  • Based on that knowledge, students will begin to cross off squares on their map that it would be unsafe or not ideal to put the new research center. 
    • Students should mark off the light blue squares (seasonal ice), dark blue squares (open water) and brown squares (land, because it would make travelling tricky).
  • Tell students that an elder from a nearby Indigenous community is able to provide local knowledge of the arctic. Ask “Why is it important to connect with local people and Indigenous communities? What kind of knowledge can they provide?”.
  • Hand each group a large map and ice extent pieces from 1970 and 2018. 
    • The red dots are a point of reference to connect the pieces together. They do not specify the ideal location of the research centre.
  • Have students compare the sea ice extent pieces from 1970 to 2018. 
  • Students will predict what the ice extent will look like in 2030 by drawing the shape of the ice on the 2018 ice piece. 
  • Hand out the 2030 ice piece to each group. Allow students to compare the scientist’s predictions to their own predictions. 
  • Repeat this for the years 2050 and 2100.
  • Have students place the circle representing sea ice in 2100 over the map again and cross off any corresponding sections that fall outside of the circle on their Arctic map.

Activity 1C: Ice Thickness

  • Hand out the Ice Thickness task card and activity bag (including a ruler and the Ice Thickness worksheet) to each group. The 3D model should be set-up.
  • Students will predict which core sample is the thickest and which is the thinnest without taking the pegs out of the 3D model.
  • Afterwards, each group will measure each peg using a ruler. 
  • They will record predictions and actual measurements on a piece of scrap paper. 
  • Display the Ice Thickness graph (PowerPoint). 
  • Allow groups to choose an area to build the research station. Did the location change from their original prediction?
  • Once each group has chosen a location, let them know whether or not they have chosen the right location. 
    • Refer to the Ice Thickness Peg Sample Map, the area where peg samples 3-5 (or squares 7E, 8E and 8F) represents the ideal location to build a new research station.

Activity 2: Ice Cores

  • Discuss some of the ways that climatologists (climate scientists) study climate change.
  • Explain why scientists use ice to study the climate record.
    • Have students provide examples of different types of ice. Point out that ice can form differently so they contribute a different type of evidence for climate change.
  • Show pictures of ice cores (PowerPoint) and point out where the oldest ice is located.
  • Explain what scientists look for in the layers of ice.
    • Briefly mention greenhouse gases. Ask “what happens when the concentration of greenhouse gases increases?”.
  • Show students a sample resin ice core. Each core is made up of 10 connected tubes. Demonstrate how to detach a tube from the core.
  • Each tube represents a different layer of ice in the core over 1,000 years. The vials inside the tube represent what the ice layer looks like when it has been melted for analysis.
  • Show students a sample vial.
  • Hand out an Ice Core task card and a bag of 10 melted sample vials to each group, along with an Ice Core worksheet for each student.
  • Instruct students to carefully observe the melted samples, looking for as many different materials and changes between the vials. 
  • Students will answer the questions on the worksheet using the Ice Core task card and Ice Core information sheet.
  • When the students are finished, have them put the ice core back together in the original order and place the melted sample vials back into the bag.
  • Wrap up by discussing the impacts of global warming, the impact of melting sea ice, the importance of understanding the Earth’s climate history and ways to reduce your carbon footprint.

Activity 3: Climate Change Discussion

  • Begin by asking students to share a way climate change has impacted their life.
  • Show an image depicting the negative climate change impacts in Canada.
  • Split the class into groups. Give each group a set of Risk Assessment task cards and each student a Risk Assessment worksheet. 
  • Tell the class that they are going to analyze, assess and plan for the associated climate-related risks of one scenario.
  •  After students have discussed these topics in their groups, briefly go through each scenario with the class and have the groups share their answers. 

Wrap-Up

  • Show the time lapse video depicting the loss of Arctic Sea ice. 
  • Review the impacts of climate change in terms of Arctic Sea ice by asking questions such as:
    • How does rising temperatures impact the ice cores/our ability to study the climate record?
    • How will it impact the Arctic and the weather where we live?
    • What will happen as sea levels rise?
  • Ask students to share any other evidence that they have experienced due to climate change.
  • Discuss possible careers related to the topics covered and what students would need to do (schooling, experience, etc...) to get into those careers. 

Activity 1: Arctic Research Centre

Weather is defined as the short-term state of the atmosphere for a given period of time. The three main factors that contribute to the weather are the sun, air and water. Climate refers to the weather in an area over a long period of time (30+ years). Scientists will look at the average precipitation, temperature, humidity, sunshine, wind velocity, and phenomena such as fog, frost and hail storms to determine the climate of an area. While the Earth’s climate is naturally variable, its average state is regulated by factors such as the Earth’s orbit around the sun and the natural greenhouse gas effect.

In Activity 1A: Climate or Weather? each group is provided with the information for one year between 1954-2022. Individually, the data only represents the weather for the area but collectively can be used to describe the climate over the past 70 years. According to the information provided, the average annual temperature in Cambridge Bay, Nunavut is increasing.

The Ice Thickness vs Date plot helps to visualize the freeze-thaw cycle. When ice freezes, the data looks like a gentle bell curve because it takes time for ice to form. The size of the peak is directly related to the amount of ice that froze that winter (small peaks = thin ice). Narrow peaks means that the freeze-thaw cycle was shorter than the year before. As ice melts, there is more of a drop off in the shape of the peak because thawing occurs faster than freezing. This is because melting is impacted by a feedback loop. As it gets warmer outside, the water and ground around the ice also warms up and it causes the ice to melt faster. Therefore, any areas with seasonal ice, open ground or open water would be unsuitable to build a research centre.

Students will learn that the average ice thickness has decreased by almost 10 cm. Safe travel throughout the Arctic depends on the ice being thick enough to support people and vehicles on it. Students should conclude that the ice peg samples 3-5 on the map represent the best area to build a new research facility.

Ice Cores

Scientists study climate change by monitoring the gas composition in the atmosphere, comparing air temperatures to historical records, monitoring weather patterns, studying changes in ice in the Arctic and exploring sediment cores. Ice is used to study the climate record because it preserves or protects things like dust and particles from changing over time. Scientists can look at the thickness of the ice and snow layers to determine the temperature and duration of the winter. Scientists also look for particles stuck in the ice, chemicals in the ice, and the thickness of the different types of layers and bubbles of gas (i.e., greenhouse gases) in the ice. All this information provides scientists with clues about what the environment on Earth was like at the time. 

The temperature on Earth is in constant fluctuation, but historically the changes occur over thousands of years. This would give animals and plants time to adapt and adjust to different conditions. This current episode of global warming is occurring much more quickly and is cause for concern.

The impacts of climate change spread far beyond the Arctic, across Canada and around the world. Climate change endangers global ecosystems, human health, Indigenous ways of life, coastal communities, global transportation systems and much more. It is important to limit our impact on the environment by reducing greenhouse gas emissions and prepare our communities for a changing landscape.

  • As an extension for Activity 1A-Climate or Weather? students can record the total rainfall and snowfall from the back of each chip onto the two blank columns of the table. After confirming with them that each chip represents a month of data, they can guess which month each chip represents. They can also calculate the total rainfall and total snowfall by taking the sum of each column; these values can be plotted with the class to look for any possible trends in the precipitation data.
  • For Activity 1B- Sea Ice Extent, have students find the approximate area of the circles (πr2). Ask them what they notice about the difference in area with a change in radius. They should note that reducing the diameter/radius of a circle will significantly reduce the area of the circle. Cutting the radius in half leads to a reduction of 4 times the area. As the sea ice extent decreases in radius the area decreases much faster.
  • Clothing4Climate (Project)- encourages youth in Grades 7 to 12 to learn about the science behind climate change and the impact our clothing system has on the environment. https://letstalkscience.ca/clothing4climate
  • Ice on Earth- The Cryosphere (Backgrounders)- more information about the cryosphere and how it is being impacted by climate change. https://letstalkscience.ca/educational-resources/backgrounders/ice-on-earth-cryosphere
  • Let’s Talk Pollution Resources (Backgrounders)- a set of resources designed to get you thinking about pollution. https://letstalkscience.ca/educational-resources/backgrounders/lets-talk-pollution-resources
  • What is the Greenhouse Effect? (Hands-on Activities) - students explore the greenhouse effect and learn about the impacts it can have on the environment. This activity is suitable for grades 1 to 5. https://letstalkscience.ca/educational-resources/hands-on-activities/what-greenhouse-effect

Web

Ocean Networks Canada: http://www.oceannetworks.ca/learning/ocean-sense/cambridge-bay

National Ocean Service: https://oceanservice.noaa.gov/welcome.html

Barnola, J.-M., D. Raynaud, C. Lorius, and N.I. Barkov. 2003. Historical CO2 record from the Vostok ice core. In Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.

Chandler, D. (2005). Record ice cores reveals Earths’ ancient atmosphere. New Scientist Environment, Retrieved from: http://www.newscientist.com/article/dn8369-record-ice-core reveals-earths-ancient-atmosphere.html

Dust in ice cores. Online article, Centre for Ice and Climate Niels Bohr institute, University Of Copenhagen. Copenhagen, Denmark. Retrieved from: http://www.iceandclimate.nbi.ku.dk/research/past_atmos/ice_core_impurities/dust_in_ice_cores/

Exploring climate events and human development. (2008, August 20). NOAA paleoclimatology, Retrieved from: http://www.ncdc.noaa.gov/paleo/ctl/cliihis100.html

NOAA,National Oceanic and Atmospheric Administration (August 2021). Climate Change Impacts. Retrieved from: https://www.noaa.gov/education/resource-collections/climate/climate-change-impacts

Freedman, A. & Mooney, C. Earth’s carbon dioxide levels hit record high, despite coronavirus-related emissions drop. The Washington Post. https://www.washingtonpost.com/weather/2020/06/04/carbon-dioxide-record-2020/

McKie, R. (2010). Antarctic ice reveals trapped secrets of climate change. The Guardian, Retrieved from http://www.guardian.co.uk/environment/2010/nov/28/antarctica-ice-climate-change

NASA Earth Observatory. (n.d.). Explaining rapid climate change: Tales from the ice. Retrieved from: http://earthobservatory.nasa.gov/Features/Paleoclimatology_Evidence/paleoclimatology_evidence_2.php

N.A.S.A Earth Observatory (n.d.). Explaining rapid climate changes: Tales from the Ice. Retrieved from: http://earthobservatory.nasa.gov/Features/Paleoclimatology_Evidence/paleoclimatology_evidence_2.php

Riebeek, H. (2005, December 2005). Paleoclimatology: The ice core record. Retrieved from: http://earthobservatory.nasa.gov/Features/Paleoclimatology_IceCores/

Attachments

What's Happening?

Activity 1: Arctic Research Centre

Weather is defined as the short-term state of the atmosphere for a given period of time. The three main factors that contribute to the weather are the sun, air and water. Climate refers to the weather in an area over a long period of time (30+ years). Scientists will look at the average precipitation, temperature, humidity, sunshine, wind velocity, and phenomena such as fog, frost and hail storms to determine the climate of an area. While the Earth’s climate is naturally variable, its average state is regulated by factors such as the Earth’s orbit around the sun and the natural greenhouse gas effect.

In Activity 1A: Climate or Weather? each group is provided with the information for one year between 1954-2022. Individually, the data only represents the weather for the area but collectively can be used to describe the climate over the past 70 years. According to the information provided, the average annual temperature in Cambridge Bay, Nunavut is increasing.

The Ice Thickness vs Date plot helps to visualize the freeze-thaw cycle. When ice freezes, the data looks like a gentle bell curve because it takes time for ice to form. The size of the peak is directly related to the amount of ice that froze that winter (small peaks = thin ice). Narrow peaks means that the freeze-thaw cycle was shorter than the year before. As ice melts, there is more of a drop off in the shape of the peak because thawing occurs faster than freezing. This is because melting is impacted by a feedback loop. As it gets warmer outside, the water and ground around the ice also warms up and it causes the ice to melt faster. Therefore, any areas with seasonal ice, open ground or open water would be unsuitable to build a research centre.

Students will learn that the average ice thickness has decreased by almost 10 cm. Safe travel throughout the Arctic depends on the ice being thick enough to support people and vehicles on it. Students should conclude that the ice peg samples 3-5 on the map represent the best area to build a new research facility.

Ice Cores

Scientists study climate change by monitoring the gas composition in the atmosphere, comparing air temperatures to historical records, monitoring weather patterns, studying changes in ice in the Arctic and exploring sediment cores. Ice is used to study the climate record because it preserves or protects things like dust and particles from changing over time. Scientists can look at the thickness of the ice and snow layers to determine the temperature and duration of the winter. Scientists also look for particles stuck in the ice, chemicals in the ice, and the thickness of the different types of layers and bubbles of gas (i.e., greenhouse gases) in the ice. All this information provides scientists with clues about what the environment on Earth was like at the time. 

The temperature on Earth is in constant fluctuation, but historically the changes occur over thousands of years. This would give animals and plants time to adapt and adjust to different conditions. This current episode of global warming is occurring much more quickly and is cause for concern.

Why does it matter?

The impacts of climate change spread far beyond the Arctic, across Canada and around the world. Climate change endangers global ecosystems, human health, Indigenous ways of life, coastal communities, global transportation systems and much more. It is important to limit our impact on the environment by reducing greenhouse gas emissions and prepare our communities for a changing landscape.

Investigate further

  • As an extension for Activity 1A-Climate or Weather? students can record the total rainfall and snowfall from the back of each chip onto the two blank columns of the table. After confirming with them that each chip represents a month of data, they can guess which month each chip represents. They can also calculate the total rainfall and total snowfall by taking the sum of each column; these values can be plotted with the class to look for any possible trends in the precipitation data.
  • For Activity 1B- Sea Ice Extent, have students find the approximate area of the circles (πr2). Ask them what they notice about the difference in area with a change in radius. They should note that reducing the diameter/radius of a circle will significantly reduce the area of the circle. Cutting the radius in half leads to a reduction of 4 times the area. As the sea ice extent decreases in radius the area decreases much faster.
  • Clothing4Climate (Project)- encourages youth in Grades 7 to 12 to learn about the science behind climate change and the impact our clothing system has on the environment. https://letstalkscience.ca/clothing4climate
  • Ice on Earth- The Cryosphere (Backgrounders)- more information about the cryosphere and how it is being impacted by climate change. https://letstalkscience.ca/educational-resources/backgrounders/ice-on-earth-cryosphere
  • Let’s Talk Pollution Resources (Backgrounders)- a set of resources designed to get you thinking about pollution. https://letstalkscience.ca/educational-resources/backgrounders/lets-talk-pollution-resources
  • What is the Greenhouse Effect? (Hands-on Activities) - students explore the greenhouse effect and learn about the impacts it can have on the environment. This activity is suitable for grades 1 to 5. https://letstalkscience.ca/educational-resources/hands-on-activities/what-greenhouse-effect

Resources

Web

Ocean Networks Canada: http://www.oceannetworks.ca/learning/ocean-sense/cambridge-bay

National Ocean Service: https://oceanservice.noaa.gov/welcome.html

Barnola, J.-M., D. Raynaud, C. Lorius, and N.I. Barkov. 2003. Historical CO2 record from the Vostok ice core. In Trends: A Compendium of Data on Global Change. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, U.S. Department of Energy, Oak Ridge, Tenn., U.S.A.

Chandler, D. (2005). Record ice cores reveals Earths’ ancient atmosphere. New Scientist Environment, Retrieved from: http://www.newscientist.com/article/dn8369-record-ice-core reveals-earths-ancient-atmosphere.html

Dust in ice cores. Online article, Centre for Ice and Climate Niels Bohr institute, University Of Copenhagen. Copenhagen, Denmark. Retrieved from: http://www.iceandclimate.nbi.ku.dk/research/past_atmos/ice_core_impurities/dust_in_ice_cores/

Exploring climate events and human development. (2008, August 20). NOAA paleoclimatology, Retrieved from: http://www.ncdc.noaa.gov/paleo/ctl/cliihis100.html

NOAA,National Oceanic and Atmospheric Administration (August 2021). Climate Change Impacts. Retrieved from: https://www.noaa.gov/education/resource-collections/climate/climate-change-impacts

Freedman, A. & Mooney, C. Earth’s carbon dioxide levels hit record high, despite coronavirus-related emissions drop. The Washington Post. https://www.washingtonpost.com/weather/2020/06/04/carbon-dioxide-record-2020/

McKie, R. (2010). Antarctic ice reveals trapped secrets of climate change. The Guardian, Retrieved from http://www.guardian.co.uk/environment/2010/nov/28/antarctica-ice-climate-change

NASA Earth Observatory. (n.d.). Explaining rapid climate change: Tales from the ice. Retrieved from: http://earthobservatory.nasa.gov/Features/Paleoclimatology_Evidence/paleoclimatology_evidence_2.php

N.A.S.A Earth Observatory (n.d.). Explaining rapid climate changes: Tales from the Ice. Retrieved from: http://earthobservatory.nasa.gov/Features/Paleoclimatology_Evidence/paleoclimatology_evidence_2.php

Riebeek, H. (2005, December 2005). Paleoclimatology: The ice core record. Retrieved from: http://earthobservatory.nasa.gov/Features/Paleoclimatology_IceCores/

Attachments