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Author(s): Linda Scott Cummings

Year: 2004

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Development of macrophysical climate models was instrumental in creating archaeoclimatic

models of past climates for specific locations (Bryson, 1998). Modeled mean temperature

and precipitation "by month for each two centuries back to 14,000 years BP" (Bryson, n.d.:1)

can be created. In addition, these parameters may be used to generate a "water budget",

comparing precipitation and potential evapotranspiration, storm intensity and frequency, snowfall,

and other climatic factors. Paleoenvironmental information for a specific location is most

appropriately available through a combination of point specific archaeoclimatic modeling and close interval

stratigraphic pollen or pollen and phytolith sampling.

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ARCHAEOCLIMATIC MODEL FOR SAFFORD, ARIZONA. Linda Scott Cummings. 2004 ( tDAR id: 379234) ; doi:10.6067/XCV80Z72RX


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  Name Size Creation Date Date Uploaded Access
04-104.pdf 293.24kb Dec 13, 2012 10:10:17 AM Public
Arizona State University The Andrew W. Mellon Foundation National Science Foundation National Endowment for the Humanities Society for American Archaeology Archaeological Institute of America