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Article: Drought variations in the eastern part of northwest China over the past two centuries: Evidence from tree rings

TitleDrought variations in the eastern part of northwest China over the past two centuries: Evidence from tree rings
Authors
KeywordsAsian Monsoon
Dendrochronology
Northwest China
Pdsi
Issue Date2009
PublisherInter-Research. The Journal's web site is located at http://www.int-res.com/journals/cr/
Citation
Climate Research, 2009, v. 38 n. 2, p. 129-135 How to Cite?
AbstractDrought reconstruction from 1794 to 2003 in the eastern part of NW China was developed by calibrating tree rings of Picea wilsonii on Xinglong Mountain with the Palmer drought severity index (PDSI). The reconstruction explains 40% of the actual PDSI variance during the period from 1951 to 2003. The most significant drought period over the reconstructed time span occurred during the 1920s to 1930s. The drought reconstructions show a climate transition in 1921 on a decadal scale and significant cyclic patterns that were identified in intervals of 10.5, 7.9-8.3, -3.5, 3.0-3.2, 2.7-2.8 and -2 yr. This reconstruction is representative of regional drought patterns in eastern NW China and demonstrates that they are different from patterns in western NW China. © Inter-Research 2009.
Persistent Identifierhttp://hdl.handle.net/10722/180563
ISSN
2015 Impact Factor: 1.69
2015 SCImago Journal Rankings: 1.107
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorFang, Ken_US
dc.contributor.authorGou, Xen_US
dc.contributor.authorChen, Fen_US
dc.contributor.authorYang, Men_US
dc.contributor.authorLi, Jen_US
dc.contributor.authorHe, Men_US
dc.contributor.authorZhang, Yen_US
dc.contributor.authorTian, Qen_US
dc.contributor.authorPeng, Jen_US
dc.date.accessioned2013-01-28T01:39:52Z-
dc.date.available2013-01-28T01:39:52Z-
dc.date.issued2009en_US
dc.identifier.citationClimate Research, 2009, v. 38 n. 2, p. 129-135en_US
dc.identifier.issn0936-577Xen_US
dc.identifier.urihttp://hdl.handle.net/10722/180563-
dc.description.abstractDrought reconstruction from 1794 to 2003 in the eastern part of NW China was developed by calibrating tree rings of Picea wilsonii on Xinglong Mountain with the Palmer drought severity index (PDSI). The reconstruction explains 40% of the actual PDSI variance during the period from 1951 to 2003. The most significant drought period over the reconstructed time span occurred during the 1920s to 1930s. The drought reconstructions show a climate transition in 1921 on a decadal scale and significant cyclic patterns that were identified in intervals of 10.5, 7.9-8.3, -3.5, 3.0-3.2, 2.7-2.8 and -2 yr. This reconstruction is representative of regional drought patterns in eastern NW China and demonstrates that they are different from patterns in western NW China. © Inter-Research 2009.en_US
dc.languageengen_US
dc.publisherInter-Research. The Journal's web site is located at http://www.int-res.com/journals/cr/en_US
dc.relation.ispartofClimate Researchen_US
dc.subjectAsian Monsoonen_US
dc.subjectDendrochronologyen_US
dc.subjectNorthwest Chinaen_US
dc.subjectPdsien_US
dc.titleDrought variations in the eastern part of northwest China over the past two centuries: Evidence from tree ringsen_US
dc.typeArticleen_US
dc.identifier.emailLi, J: jinbao@hku.hken_US
dc.identifier.authorityLi, J=rp01699en_US
dc.description.naturelink_to_subscribed_fulltexten_US
dc.identifier.doi10.3354/cr00781en_US
dc.identifier.scopuseid_2-s2.0-62249119256en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-62249119256&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume38en_US
dc.identifier.issue2en_US
dc.identifier.spage129en_US
dc.identifier.epage135en_US
dc.identifier.isiWOS:000270149600004-
dc.publisher.placeGermanyen_US
dc.identifier.scopusauthoridFang, K=19640101200en_US
dc.identifier.scopusauthoridGou, X=7003498424en_US
dc.identifier.scopusauthoridChen, F=7404907075en_US
dc.identifier.scopusauthoridYang, M=7404925844en_US
dc.identifier.scopusauthoridLi, J=35272482700en_US
dc.identifier.scopusauthoridHe, M=25923352500en_US
dc.identifier.scopusauthoridZhang, Y=36109723900en_US
dc.identifier.scopusauthoridTian, Q=8564415000en_US
dc.identifier.scopusauthoridPeng, J=15760581700en_US

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