Lesson Objectives...
Analyze and interpret data on graphs of carbon dioxide levels collected from ice cores to collect evidence of whether the changes in these levels are cyclical in nature and a normal occurrence or are changing at an non-normal rate.
Read, watch, listen, and analyze the StoryMap - Using Ice Cores to Study Carbon Dioxide. What are the ice cores telling us?
How can we figure out what is "normal"?
We can go to the Antarctic! Each year, scientists travel to the ice sheets of Antarctica to see what they can learn from gas bubbles trapped in ice. Antartica is the perfect place to study carbon dioxide levels. The ice sheets are home to few animals and occasionally humans. This means any gas bubbles trapped in ice are there from the atmosphere.
To study carbon dioxide levels, scientists spend up to three months living on the ice sheet. They sleep in special tents that are designed for cold temperatures (pictured below). They eat in wood structures that they temporarily build just for the time they are there. They have to shovel and melt snow for drinking water, for showering, and for doing laundry.
They have to deal with harsh conditions, but their work is very important for understanding if changes in the amount of carbon dioxide in the atmosphere are part of normal cycles that Earth goes through.
Would you want to travel there as part of a science team? Why or why not?
How do the gas bubbles get into the ice?
Teams of scientists go to Antarctic ice sheets that are up to two miles thick. Thick ice sheets can contain gas bubbles that are many years old. Layers of ice form on top of older layers of ice. The deeper you go, the older the ice. Dr. Peter Neff is one of the scientists studying gas bubbles in ancient ice. Take a look at the video to hear how the ice bubbles get trapped deep in the ice sheet.
Is this similar or different from what you observed in the ice cubes made from tap water?
What do you think ancient ice cubes would taste like?
Imagine standing on a sheet of ice that is two miles thick. The ice you want is thousands of feet below the surface. How do you get to it? Once you have it, how do you use it to study carbon dioxide levels in the atmosphere?
First, you use a special drill that cuts "ice cores" that are a few meters long. Depending on how old the ice needs to be, it may take several days or even weeks to go deep enough into the ice sheet.
Once you have the ice you need, you have to get the gas bubbles out. When you looked at the carbonated ice, how did you get the bubbles out? You melted it! That's exactly what the scientists do. They have special equipment that traps the air as the ice cores melt. Then, special sensors tell them how much carbon dioxide was trapped in each layer of ice.
Watch the short video on the right to learn more about how scientists study ice core data. As you watch, think about what the scientists are doing. How is their process similar or different from what you did in class with the ice cubes and the carbon dioxide detector?
Analyze Data Scientists Find in the Ice Cores
Let's look at the data scientists collected using ice core samples. Since we want to figure out changes in carbon dioxide, the graphs will look only at changes in carbon dioxide over time.
We already know that the amount of carbon dioxide in the air has been increasing over the last 100 years, but we want to know if this increase is part of a normal cycle. The first graph (left) shows data scientists have collected since the 1950s. This data was collected using sensors similar to the carbon dioxide detector that you used in your investigation. There are many sensors throughout the world, but we are looking at data collected on Mauna Loa in Hawai'i. The second graph shows data collected from ice cores dating back 800,000 years ago. Analyze the graphs with a partner and record your noticings in your notebook. Be ready to share your findings.
Levels of CO2 are increasing at a faster rate than the normal cycles, which means the new levels are out of the normal range.
CO2 levels over the last 100 years have been rising consistently.
We look back at data from hundreds of thousands of years through analyzing ice core data and find there are cycles, but the last 100 years are not following the normal cycle.