AN ARCHAEOCLIMATIC MODEL OF JACKSON, WYOMING
Author(s): Linda Scott Cummings
Specific, pertinent information can be generated through a combination of
archaeoclimatic modeling and examination of close-interval stratigraphic pollen samples.
Although large trends, such as increased warmth and potential evapotranspiration, can be
postulated for large areas during the middle Holocene and fluctuating conditions can be
postulated for the past four thousand years, paleoenvironmental information for a specific
location is more appropriately available through a combination of point specific archaeoclimatic
modeling and close-interval stratigraphic pollen sampling. These models generate temperature
and precipitation graphs, as well as potential evapotranspiration and "march of precipitation"
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AN ARCHAEOCLIMATIC MODEL OF JACKSON, WYOMING. Linda Scott Cummings. 2006 ( tDAR id: 379340) ; doi:10.6067/XCV8WM1CWC
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