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dc.contributor.authorKipfmueller, Kurt F.
dc.contributor.authorElliott, Grant P.
dc.contributor.authorLarson, Evan R.
dc.contributor.authorSalzer, Matthew W.
dc.date.accessioned2017-02-17T23:09:55Z
dc.date.available2017-02-17T23:09:55Z
dc.date.issued2010-07
dc.identifier.citationKipfmueller, K.F., Elliott, G.P., Larson, E.R., Salzer, M.W., 2010. An assessment of the dendroclimatic potential of three conifer species in northern Minnesota. Tree-Ring Research 66(2):113-126.en
dc.identifier.issn2162-4585
dc.identifier.issn1536-1098
dc.identifier.urihttp://hdl.handle.net/10150/622621
dc.description.abstractRing-width chronologies from Pinus resinosa Ait., Pinus strobus L., and Thuja occidentalis L. were developed in two areas of the Boundary Waters Canoe Area Wilderness to assess their growth climate response and their potential for developing reconstructions of climate. New red pine chronologies were combined with existing chronologies to extend the ring-width record both into the past and into the present. Ring-width response to climate, assessed using correlation analysis and response functions, was broadly similar among all three species with relatively significant positive relationships with June–July precipitation and significant negative (but less consistent) associations with June–July temperatures (p < 0.05). White-cedar appeared to have a broader phenological window of response with a stronger spring influence when compared to other species included in this study. Comparisons with other nearby proxies showed relatively strong coherence overall but with some important regional differences. Overall, these species may be useful for placing current climatic patterns in the Boundary Waters within a longer term perspective but care should be taken with respect to identifying appropriate climatic records for calibration.
dc.language.isoen_USen
dc.publisherTree-Ring Societyen
dc.relation.urlhttp://www.treeringsociety.orgen
dc.rightsCopyright © Tree-Ring Society. All rights reserved.en
dc.subjectDendrochronologyen
dc.subjectTree Ringsen
dc.subjectPinus resinosaen
dc.subjectPinus strobusen
dc.subjectThuja occidentalisen
dc.subjectMinnesotaen
dc.subjectBoundary Waters Canoe Area Wildernessen
dc.titleAn Assessment Of The Dendroclimatic Potential Of Three Conifer Species In Northern Minnesotaen_US
dc.typeArticleen
dc.typetexten
dc.contributor.departmentDepartment of Geography, University of Minnesotaen
dc.contributor.departmentDepartment of Geography, University of Missourien
dc.contributor.departmentDepartment of Social Sciences, University of Wisconsin-Plattevilleen
dc.contributor.departmentLaboratory of Tree-Ring Research, University of Arizonaen
dc.identifier.journalTree-Ring Researchen
dc.description.collectioninformationThis item is part of the Tree-Ring Research (formerly Tree-Ring Bulletin) archive. For more information about this peer-reviewed scholarly journal, please email the Editor of Tree-Ring Research at editor@treeringsociety.org.en
refterms.dateFOA2018-08-14T09:03:39Z
html.description.abstractRing-width chronologies from Pinus resinosa Ait., Pinus strobus L., and Thuja occidentalis L. were developed in two areas of the Boundary Waters Canoe Area Wilderness to assess their growth climate response and their potential for developing reconstructions of climate. New red pine chronologies were combined with existing chronologies to extend the ring-width record both into the past and into the present. Ring-width response to climate, assessed using correlation analysis and response functions, was broadly similar among all three species with relatively significant positive relationships with June–July precipitation and significant negative (but less consistent) associations with June–July temperatures (p < 0.05). White-cedar appeared to have a broader phenological window of response with a stronger spring influence when compared to other species included in this study. Comparisons with other nearby proxies showed relatively strong coherence overall but with some important regional differences. Overall, these species may be useful for placing current climatic patterns in the Boundary Waters within a longer term perspective but care should be taken with respect to identifying appropriate climatic records for calibration.


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