Dendroclimatic Analysis Using Thornwaite-Mather-Type Evapotranspiration Models: A Bridge Between Dendroevology and Forest Simulation Models
Affiliation
Department of Biology, Ball State University, Muncie, INIssue Date
2001
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Copyright © Tree-Ring Society. All rights reserved.Collection Information
This item is part of the Tree-Ring Research (formerly Tree-Ring Bulletin) archive. It was digitized from a physical copy provided by the Laboratory of Tree-Ring Research at The University of Arizona. For more information about this peer-reviewed scholarly journal, please email the Editor of Tree-Ring Research at editor@treeringsociety.org.Publisher
Tree-Ring SocietyJournal
Tree-Ring ResearchCitation
LeBlanc, D., Terrell, M. 2001. Dendroclimatic analyses using Thornthwaite-Mather-type evapotranspiration models: a bridge between dendroecology and forest simulation models. Tree-Ring Research 57(1):55-66.Abstract
The objective of this study was to document correlations between radial growth of white oak (Quercus alba L.) at 128 sites in the eastern US and variables related to early growing season site water balance, including the ratio of actual to potential evapotranspiration (AE/PE) computed based on the procedure described by Thornthwaite and Mather (1957). White oak radial growth was strongly correlated with all measures of early growing season water balance, but was most consistently and strongly correlated with Palmer Drought Severity Index (PDI) and AE /PE ratio computed using a modified Thornthwaite-Mather model. We propose that dendroecological analyses of tree growth responses to climate based on AE /PE variables could provide empirical data useful for improving climate response algorithms in forest simulation models. This change of standard practice could also improve biological interpretations derived from such dendroecological analyses.ISSN
2162-45851536-1098