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Causes of Reduced North Atlantic Storminess During the Last Glacial Maximum from CCSM3

Causes of Reduced North Atlantic Storminess During the Last Glacial Maximum from CCSM3. Aaron Donohoe UW COGS talk April 12, 2007. Why Study North Atlantic Storms During the LGM?. d 18 O Temperature Proxy from GISP 2, Greenland Summit. 12 C. Warmer. (Stuiver and Grooves, 2000). TIME.

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Lgm storm growth - PowerPoint PPT Presentation

Causes of Reduced North Atlantic Storminess During the Last Glacial Maximum from CCSM3