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bpcrc.osu.edu Photo courtesy of Lonnie G. Thompson bpcrc.osu.edu Photo courtesy of Lonnie G. Thompson

bpcrc.osu.edu Photo courtesy of Lonnie G. Thompson - PowerPoint Presentation

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bpcrc.osu.edu Photo courtesy of Lonnie G. Thompson - PPT Presentation

Archive β Anions and Cations δ 18 O Dust bpcrcosuedu Ice core cross section bpcrcosuedu 16 O lighter than 18 O preferentially evaporates 18 O heavier than 16 O preferentially precipitates ID: 1026478

data ice task core ice data core task osu 16o proxy nuclear age reference 18o horizon preferentially patterns year

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1. bpcrc.osu.edu

2. Photo courtesy of Lonnie G. Thompson

3.

4. ArchiveβAnions and Cationsδ18ODustbpcrc.osu.eduIce core cross sectionbpcrc.osu.edu

5. 16O (lighter than 18O) preferentially evaporates18O (heavier than 16O) preferentially precipitatesHigher temperatures = more energy to evaporate heavy 18O

6. Ice core dating activityYou will be given data from the Crawford Point, Greenland ice core

7. Task 1: Study the data in front of you and list 5 observations about these data.Consider trends or patterns in the data.Consider how these proxy data relate to the climate.

8.

9. Task 2: Apply the timeline of nuclear bomb testing to the radioactivity data from the ice core.This will give you the known age of the ice at a certain depth (a reference horizon).*Important note*Remember where the oldest ice is located

10. Task 3: Determine the year in which the ice core was drilled (the year at 0 m).Given the nuclear reference horizon, devise a strategy to determine the age of ice at the top.Consider your proxy data and the patterns they display.