Editing Paleoclimatology (section)

== <span style="color: #FFFFFF;">Analyzing</span> ==
{| class="wikitable"
|+ Climate Proxies
! Proxy !! Time Range !! What it tells us
|-
| Tree Rings || 1-2,000 years || Local Rain and Temperature
|-
| Coral Reefs || 1-5,000 years || Ocean Temperature and Chemistry
|-
| Ice Cores || 1-800,000 years || Atmosphere Gases and Global Temp
|-
| Ocean Sediments || 1-100 million years || Deep History of the Earth and Ice Sheets
|}

'''The Concept of "Signal vs. Noise"''': Analyzing why it's hard to be a climate detective. In a "Yearly" record, there is a lot of "Noise" (like a one-day storm). Paleoclimatologists must use "Math" to "Smooth the lines" to find the "Signal"—the long-term trend that shows where the world is actually going.
</div>

<div style="background-color: #483D8B; color: #FFFFFF; padding: 20px; border-radius: 8px; margin-bottom: 15px;">