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Introduction to Paleoclimatology → Synthesizing Proxy Records into a Climate Reconstruction
A foundational learning path for high school students interested in climate history, covering the principles of paleoclimatology and the use of ice cores, tree rings, and sediments as climate proxies. Learners will explore how these records are analyzed to infer past temperatures and understand ice ages and climate variability.
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14 steps · 3 stages. Click any step to inspect it and see it on the Path Map.
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