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This study explores the climatic records from PRISM Modeled Precipitation and Temperature data, specifically focused on key river basins including the Columbia River, Missouri River, and Hudson Bay. It emphasizes the impact of population doubling over approximately 30 years in these regions and examines paleoclimate evidence from lake sediment records. The findings contribute to understanding climate variations and transitions from the Holocene to the Pleistocene, as well as their implications for future climate scenarios and population dynamics.
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Nelson/Churchill Rivers (Hudson Bay) Columbia River (Pacific) Missouri River (Gulf of Mexico)
PRISM Modeled Precipitation and Temperature From: The PRISM Group, http://www.ocs.oregonstate.edu/prism/index.phtml
Human Interface: Population Doubling ~30 years Holocene-Pleistocene Lake Sediment Paleoclimate Records