Lab Exercise: Vostok Ice Core: The Cold Hard Truth
In this lab, students learn how to use data from the Vostok ice core to measure and compare temperature between different temporal periods. Ice core samples contain several climate indicators: the amount of dust in each layer from volcanic debris, airborne continental dust and biological material, and cosmic particles; all the aforementioned mix with snow and act as a barrier between different ice layers. The composition of bubbles of air trapped in the ice is a measure of the makeup of the atmosphere in ancient times. The isotopic composition of water, and in particular, the heavy isotope of oxygen, as well as deuterium, is indicative of the temperatures in the environment. Understanding the historic and contemporary content of ice core samples enables scientists to make accurate predictions regarding the Earth's climate future.
Context for Use
Description and Teaching Materials
The structure and primary components of this lab lesson are sourced from Columbia University's Earth Environmental Systems Climate (EESC) course Lab #10 Vostok Ice Core and the University of Michigan's Analysis of Vostok Ice Core Data.
A review of each of the lab components should provide sufficient preparation for the lab; in particular, the Michigan lab contains helpful context for the purpose and utility of the lab (and could serve to add further depth to Columbia's introductory PowerPoint.
Evidence from paleoclimate research suggests an anthropogenic influence on global warming trends. Ice core samples offer uninterrupted information on significant properties of paleoclimate, including local temperature and precipitation rate, humidity, wind speed; additionally, ice core samples reveal changes in atmospheric composition.
The Vostok core was drilled in East Antarctica, at the Soviet station Vostok from an altitude of 3488 m, and has a total length of 2083 m. Ice samples have been analyzed with respect to isotopic content in 2H, dust, and methane and carbon dioxide trapped in air bubbles. The profiles of 2H, methane, and carbon dioxide concentrations behave in a similar way with respect to depth in the core, showing a short interglacial stage, the Holocene, at the top, a long glacial stage below, and the last interglacial stage near the bottom of the core. The record goes back in time about 160,000 years. (In January 1998, the collaborative ice-drilling project at the Russian Vostok station reaching a depth of 3,623 m. Preliminary data indicate the Vostok ice-core record extends through four climate cycles, with ice slightly older than 400 kyr (Petit et al. 1997, 1999). but for this lab, we will analyze the 160ky data as an exercise.)
The following lab consists of four sections and 10 separate tasks.
A. Gas Age versus Ice Age
Age is calculated in two different ways within an ice core. The ice age is calculated from an analysis of annual layers in the top part of the core, and using an ice flow model for the bottom part. The gas age data accounts for the fact that gas is only trapped in the ice at a depth well below the surface where the pores close up.
Task 1: Open the Vostok ice core Excel file from courseworks. Plot both the ice age and the gas age as a function of depth on the same graph. Describe the graph and answer the following questions:
- What are the units of both age scales?
- What are the depths of the shallowest and deepest data points? For the rest of the lab, assume that the most shallow ice core measurements represent the environmental conditions in the 18th century before the Industrial Revolution.
- Does age increase or decrease down the core?
- Why do the two age curves differ?
- How much younger is a bubble of gas than the ice that surrounds it, at a depth of 250 m?
- Is the thickness of an annual layer of ice smallest at the top or bottom of the core?
B. Delta-Deuterium (δD) As A Proxy For Temperature
Task 2: Next you will calculate the temperature based on the isotopic composition of the ice. Insert a blank column into the table to the right of the delta-deuterium column (δD). Isotopic ratios are used to model temperature. Calculate the temperature at Vostok based on the following formula describing the empirical relationship between temperature and deuterium concentration:
Temperature (°C) = -55.5 + (δD + 440) / 6
*Be sure to save your temperatures for plotting
Now plot your calculated temperature vs. ice age.
· List sources of uncertainty for this paleoclimate record (Hint: think about some of the uncertainties in the age models and compare the age of the Last Glacial Maximum to what scientists consider the age to be today.)
· How long ago did the maximum temperature occur (last interglacial)?
· How long ago did the minimum temperature occur(last glacial maximum)?
· How do these temperature compare to the current average Vostok temperature? (Note: you will need to compute an average of the temperatures given on this site (24h average temperature).)
C. CO2,CH4,and Dust
Task 4: Plot CO2 as a function of gas age. How closely does the plot of CO2 resemble that of temperature? Now plot CO2 (x axis) against temperature (y axis). Add a trendline and record the R2 value. Based on your work in previous labs, do you think this correlation is significant?
Task 5: Make the same plots for CH4.(CH4 vs gas age, CH4 (x axis) vs temperature (y axis), Add a trendline and record the R2 value ). Is CO2or CH4more closely correlated with temperature? Why do you think that is? Now make a plot of dust as a function of ice age. Compare this to the temperature vs ice age plot. And plot the dust against temperature. How well do the changes in dust concentration correlate with the temperature changes?
Task 6: The present atmospheric CO2 and CH4 concentrations are 379 ppmv and 1,774 ppbv, respectively, according to IPCC (2007). Calculate the changes in CO2 and CH4 concentrations between the last glacial maximum (~20 kyr ago) and the 18th century, and between the 18th century and today. Whether the change in recent 200yr is larger than the change in last 20 kyr before 18th century?
Task 7: Insert today's CO2 concentration (use the IPCC value given above) into the linear regression equation from question #4 to determine what the past relationship between CO2 and temperature predicts that today's temperature should be at Vostok. How does your calculation compare with the known value?
You can calculate the rate of change of temperature (degrees/ka) by subtracting one temperature from the next oldest and dividing by the ice-age difference. That is:
(younger temp - older temp)/(younger ice age - older ice age) = rate of change (positive for warming, negative for cooling). Recall that younger means shallower here.
Task 8: Calculate the warming rate for the entire time series and plot warming rate vs. ice age. What is the most rapid warming that occurred during the deglaciation that began around 15,000-20,000 years ago? How do the rates of warming that you've calculated compare with the current warming characterized in the 2007 assessment report from the IPCC (see link to the report and estimate a value from the graph (degC/year))?
Task 9: Now calculate the rate of change in greenhouse gas concentrations (CO2 and CH4) versus gas age for this time period. How do these rates of change compare with the changes in carbon dioxide and methane concentrations that have occurred over the past 100 years (see the link to the 2007 assessment report of the IPCC)?
Task 10: Note that there were two major warming events representing two deglaciations in the Vostok calculated temperature data. Then plot (since last 30 kyr) and look at how CO2 and CH4 change during last deglaciation period. From the data provided in this lab, can you tell which changes first, temperature or greenhouse gas (CO2, CH4) concentrations?
Note: in case you want to plot secondary y axis:
- in the graph, right click on the line you want to have the y-axis on the other side.
- select "format data series" menu
- select "axis" tab
- click on "secondary axis"
1. Why do ice age and gas age change with depth in the core? Why does the thickness of annual layers change?
2. Why were CO2, CH4, and dust concentrations different during the glacial time as compared to the 18th century?
3. How did conditions during the last glacial maximum (around 20,000 years ago) differ from today's conditions?
4. How do the glacial/interglacial changes in temperature, carbon dioxide, and methane compare to the changes since the 18th century?
Below are the links for source material and resources:
· EESC course page:https://courseworks.columbia.edu/
· University of Michigan: http://www.globalchange.umich.edu/gctext/Inquiries/Inquiries_by_Unit/Unit_8a.htm
· IPCC 2007 Report (Chapter 6 Paleoclimate and Chapter 10 Global Climate Projections): http://www.ipcc.ch/publications_and_data/publications_ipcc_fourth_assessment_report_wg1_report_the_physical_science_basis.htm
Handouts and Directions:
· Lab instructions
· Lab data
· Computer lab or moveable laptops with Internet access and Excel.
· LCD projector
· Handouts - lab instructions
· "Writing a Lab Report" (may have already been disseminated)