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dc.contributor.authorNautiyal, A.
dc.contributor.authorRawat, G. S.
dc.contributor.authorRamesh, K.
dc.contributor.authorKannan, R.
dc.contributor.authorStephenson, S. L.
dc.date.accessioned2025-01-21T20:48:01Z
dc.date.available2025-01-21T20:48:01Z
dc.date.issued2019-08-07
dc.identifier.citationA. Nautiyal, G. S. Rawat, K. Ramesh, R. Kannan, and S. L. Stephenson "SEASONAL PRECIPITATION SIGNAL IN EARLYWOOD AND LATEWOOD RING WIDTH CHRONOLOGIES OF PINUS ROXBURGHII," Tree-Ring Research 75(2), 86-100, (7 August 2019). https://doi.org/10.3959/1536-1098-75.2.86
dc.identifier.issn1536-1098
dc.identifier.doi10.3959/1536-1098-75.2.86
dc.identifier.urihttp://hdl.handle.net/10150/675611
dc.description.abstractThe growth response of earlywood and latewood to precipitation in chir pine (Pinus roxburghii) was studied by examining a series of core samples from the Garhwal Himalaya, India. Earlywood and latewood were observed to contribute about equal proportions towards the total ring width. Comparison of tree-ring data with the CRU TS3.22 (land) precipitation dataset indicates that earlywood is positively correlated with spring and early summer precipitation, whereas latewood is negatively correlated with pre-monsoon and early monsoon precipitation. This seasonally-reversed climate signal is confirmed when regional weather station precipitation data were used. A similar seasonally reversed climate response was found in earlywood and latewood of two datasets obtained from core samples from two other sites located in Nepal and Bhutan. Because chir pine is a light-demanding species, light limitation during the monsoon season could be an important factor behind the negative correlation between latewood and precipitation. NOAA NCEP-NCAR low cloud data were used to test this hypothesis, and the preliminary results support the hypothesis; however, further analysis will be needed to fully validate this hypothesis.
dc.description.sponsorshipUniversity of Arkansas-Fort Smith
dc.language.isoen
dc.relation.urlhttps://www.treeringsociety.org/
dc.rightsCopyright © 2019 by the Tree-Ring Society
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/
dc.subjectChir pine
dc.subjectclimate
dc.subjectdendrochronology
dc.subjectgrowth response
dc.subjectthe Himalaya
dc.subjecttree rings
dc.subjectintraannual density-fluctuations
dc.subjectwestern himalaya
dc.subjectgrowth
dc.subjectforest
dc.subjectreconstruction
dc.subjectvariability
dc.subjectrainfall
dc.subjectIndia
dc.subjectresponses
dc.titleSeasonal Precipitation Signal in Earlywood and Latewood Ring Width Chronologies of Pinus Roxburghii
dc.typeArticle
dc.typetext
dc.identifier.eissn2162-4585
dc.identifier.journalTree-Ring Research
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.
dc.eprint.versionFinal Published Version
dc.source.journaltitleTree-Ring Research
dc.source.volume75
dc.source.issue2
dc.source.beginpage86
dc.source.endpage100
refterms.dateFOA2025-01-21T20:48:01Z


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