Date of Award


Degree Type


Degree Name

Master of Science



Major Professor

Henri D. Grissino-Mayer

Committee Members

Sally Horn, Carol Harden


Previous dendroclimatological research has shown that tree growth is primarily a function of temperature and precipitation. At mid-latitude temperate forest sites, trees have been found to be mainly moisture-sensitive rather than temperature-sensitive. Researchers at the 2007 North American Dendroecological Fieldweek were surprised to find a winter temperature signal in a shortleaf pine (Pinus echinata) chronology from Great Smoky Mountains National Park, Tennessee. Building on this finding, I evaluated yellow pine climate-tree growth relationships at five sites on the western end of Great Smoky Mountains National Park using correlation, response function, moving correlation, and wavelet analyses. Winter mean minimum temperatures influenced yellow pine growth at all five sites, but spring precipitation and growing season moisture conditions also affected growth. Growth was positively associated with Atlantic Ocean sea surface temperature anomalies (SSTAs) and North Atlantic Ocean (NAO) index values, suggesting that positive phases of the both the Atlantic Multidecadal Oscillation (AMO) and the NAO lead to above average annual tree growth. Pacific Ocean climate variability did not have a strong influence on yellow pine growth in Great Smoky Mountains National Park.

Climate-growth relationships were temporally unstable at all of the five sites. In the mid-20th century, the response to growing season precipitation and moisture conditions weakened. Simultaneously, the response to winter and fall mean minimum temperatures strengthened. The shift may have been caused by an AMO phase change, age-dependent climate responses, changes in phenology, decreased drought frequency, data quality, or atmospheric pollution. Because the relationship with temperaturestrengthened since 1950, yellow pines in Great Smoky Mountains National Park do not show evidence of divergence between temperature and tree growth. Still, this network of chronologies is not ideal for climate reconstruction because the climate-growth relationships were unstable over time. In the future, climate analysis of other chronologies from the southeastern U.S. will be necessary to determine whether the mid- 20th century shift in climate response at Great Smoky Mountains National Park occurred throughout the region.

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