Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)

Despite growing in wet lowland and riparian settings, <i>Taxodium distichum</i> (L.) Rich. (bald cypress) has a strong response to hydroclimate variability, and tree ring chronologies derived from bald cypress have been used extensively to reconstruct drought, precipitation and streamflo...

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Main Authors: Matthew D. Therrell, Emily A. Elliott, Matthew D. Meko, Joshua C. Bregy, Clay S. Tucker, Grant L. Harley, Justin T. Maxwell, Glenn A. Tootle
Format: Article
Language:English
Published: MDPI AG 2020-10-01
Series:Forests
Subjects:
Online Access:https://www.mdpi.com/1999-4907/11/10/1100
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spelling doaj-d101cc67340f408cbe7a7f1c9b9055632020-11-25T03:55:40ZengMDPI AGForests1999-49072020-10-01111100110010.3390/f11101100Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)Matthew D. Therrell0Emily A. Elliott1Matthew D. Meko2Joshua C. Bregy3Clay S. Tucker4Grant L. Harley5Justin T. Maxwell6Glenn A. Tootle7Department of Geography, University of Alabama, Tuscaloosa, AL 35487, USADepartment of Geography, University of Alabama, Tuscaloosa, AL 35487, USADepartment of Geosciences, University of Arizona, Tucson, AZ 85721, USADepartment of Geography, Indiana University, Bloomington, IN 47405, USADepartment of Geography, University of Alabama, Tuscaloosa, AL 35487, USADepartment of Geography and Geological Sciences, University of Idaho, Moscow, ID 83844, USADepartment of Geography, Indiana University, Bloomington, IN 47405, USADepartment of Civil, Construction and Environmental Engineering, University of Alabama, Tuscaloosa, AL 35487, USADespite growing in wet lowland and riparian settings, <i>Taxodium distichum</i> (L.) Rich. (bald cypress) has a strong response to hydroclimate variability, and tree ring chronologies derived from bald cypress have been used extensively to reconstruct drought, precipitation and streamflow. Previous studies have also demonstrated that false rings in bald cypress appear to be the result of variations in water availability during the growing season. In this study 28 trees from two sites located adjacent to the Choctawhatchee River in Northwestern Florida, USA were used to develop a false ring record extending from 1881 to 2014. Twenty false ring events were recorded during the available instrumental era (1931–2014). This record was compared with daily and monthly streamflow data from a nearby gage. All 20 of the false-ring events recorded during the instrumental period occurred during years in which greatly increased streamflow occurred late in the growing season. Many of these wet events appear to be the result of rainfall resulting from landfalling tropical cyclones. We also found that the intra-annual position of false rings within growth rings reflects streamflow variability and combining the false-ring record with tree ring width chronologies improves the estimation of overall summer streamflow by 14%. Future work using these and other quantitative approaches for the identification and measurement of false ring variables in tree rings may improve tree-ring reconstructions of streamflow and potentially the record of tropical cyclone rainfall events.https://www.mdpi.com/1999-4907/11/10/1100<i>Taxodium distichum</i>bald cypressdendrochronologytree ringsintra-annual density fluctuation
collection DOAJ
language English
format Article
sources DOAJ
author Matthew D. Therrell
Emily A. Elliott
Matthew D. Meko
Joshua C. Bregy
Clay S. Tucker
Grant L. Harley
Justin T. Maxwell
Glenn A. Tootle
spellingShingle Matthew D. Therrell
Emily A. Elliott
Matthew D. Meko
Joshua C. Bregy
Clay S. Tucker
Grant L. Harley
Justin T. Maxwell
Glenn A. Tootle
Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)
Forests
<i>Taxodium distichum</i>
bald cypress
dendrochronology
tree rings
intra-annual density fluctuation
author_facet Matthew D. Therrell
Emily A. Elliott
Matthew D. Meko
Joshua C. Bregy
Clay S. Tucker
Grant L. Harley
Justin T. Maxwell
Glenn A. Tootle
author_sort Matthew D. Therrell
title Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)
title_short Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)
title_full Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)
title_fullStr Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)
title_full_unstemmed Streamflow Variability Indicated by False Rings in Bald Cypress (<i>Taxodium distichum</i> (L.) Rich.)
title_sort streamflow variability indicated by false rings in bald cypress (<i>taxodium distichum</i> (l.) rich.)
publisher MDPI AG
series Forests
issn 1999-4907
publishDate 2020-10-01
description Despite growing in wet lowland and riparian settings, <i>Taxodium distichum</i> (L.) Rich. (bald cypress) has a strong response to hydroclimate variability, and tree ring chronologies derived from bald cypress have been used extensively to reconstruct drought, precipitation and streamflow. Previous studies have also demonstrated that false rings in bald cypress appear to be the result of variations in water availability during the growing season. In this study 28 trees from two sites located adjacent to the Choctawhatchee River in Northwestern Florida, USA were used to develop a false ring record extending from 1881 to 2014. Twenty false ring events were recorded during the available instrumental era (1931–2014). This record was compared with daily and monthly streamflow data from a nearby gage. All 20 of the false-ring events recorded during the instrumental period occurred during years in which greatly increased streamflow occurred late in the growing season. Many of these wet events appear to be the result of rainfall resulting from landfalling tropical cyclones. We also found that the intra-annual position of false rings within growth rings reflects streamflow variability and combining the false-ring record with tree ring width chronologies improves the estimation of overall summer streamflow by 14%. Future work using these and other quantitative approaches for the identification and measurement of false ring variables in tree rings may improve tree-ring reconstructions of streamflow and potentially the record of tropical cyclone rainfall events.
topic <i>Taxodium distichum</i>
bald cypress
dendrochronology
tree rings
intra-annual density fluctuation
url https://www.mdpi.com/1999-4907/11/10/1100
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