GEOL 1111_IceCores_questions (1)

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Normandale Community College *

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1111

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Geology

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Jan 9, 2024

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docx

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1

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GEOL 1111 – Environmental Geology Lab: Ice Cores: Questions for submission Climate History & the Cryosphere: Adapted from https://serc.carleton.edu/eslabs/cryosphere/4b.html Part 1: Gas Age vs. Ice Age Questions 1. Does ages increase or decrease down the core? Why? 2. Is the thickness of an annual layer of ice smallest at the top or bottom of the core? Why? Part 3: CO2 and Dust Questions 3. The present atmospheric CO2 concentration is 379 ppmv (IPCC, 2007). Calculate the change in CO2 concentration between the last glacial maximum (~20,000 years ago) and the 18th century, and between the 18th century and today. You can assume that the shallowest ice core measurements represent the environmental conditions in the 18th century. Why were CO 2 and dust concentrations different during the glacial time as compared to the 18th century? 4. Why are these ice core paleoclimate records so important to our understanding and prediction of climate change? 5. Note that there were two major warming events representing two deglaciations in the Vostok calculated temperature data. Look at how CO 2 changes during those deglaciation periods. From the data provided in this lab, can you tell which changes first, temperature or CO 2 concentration? Why is this important?
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