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Article: Reconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability

TitleReconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variability
Authors
KeywordsDrought
Northeastern Tibetan Plateau
Pdsi
Sst
Tree-Ring
Issue Date2010
PublisherSpringer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00382/index.htm
Citation
Climate Dynamics, 2010, v. 35 n. 4, p. 577-585 How to Cite?
AbstractWe present a Palmer Drought Severity Index reconstruction (r = 0.61, P < 0.01) from 1440 to 2007 for the southeastern Tibetan Plateau, based on tree rings of the forest fir (Abies forrestii). Persistent decadal dry intervals were found in the 1440s-1460s, 1560s-1580s, 1700s, 1770s, 1810s, 1860s and 1980s, and the extreme wet epochs were the 1480s-1490s, 1510s-1520s, 1590s, 1610s-1630s, 1720s-1730s, 1800s, 1830s, 1870s, 1930s, 1950s and after the 1990s. Comparisons of our record with those identified in other moisture related reconstructions for nearby regions showed that our reconstructed droughts were relatively consistent with those found in other regions of Indochina, suggesting similar drought regimes. Spectral peaks of 2.3-5.5 years may be indicative of ENSO activity, as also suggested by negative correlations with SSTs in the eastern equatorial and southeastern Pacific Ocean. Significant multidecadal spectral peaks of 29.2-40.9 and 56.8-60.2 years were identified. As indicated by the spatial correlation patterns, the decadal-scale variability may be linked to SST variations in the northern Pacific and Atlantic Oceans. © 2009 Springer-Verlag.
Persistent Identifierhttp://hdl.handle.net/10722/180578
ISSN
2015 Impact Factor: 4.708
2015 SCImago Journal Rankings: 3.623
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorFang, Ken_US
dc.contributor.authorGou, Xen_US
dc.contributor.authorChen, Fen_US
dc.contributor.authorLi, Jen_US
dc.contributor.authorD'arrigo, Ren_US
dc.contributor.authorCook, Een_US
dc.contributor.authorYang, Ten_US
dc.contributor.authorDavi, Nen_US
dc.date.accessioned2013-01-28T01:39:59Z-
dc.date.available2013-01-28T01:39:59Z-
dc.date.issued2010en_US
dc.identifier.citationClimate Dynamics, 2010, v. 35 n. 4, p. 577-585en_US
dc.identifier.issn0930-7575en_US
dc.identifier.urihttp://hdl.handle.net/10722/180578-
dc.description.abstractWe present a Palmer Drought Severity Index reconstruction (r = 0.61, P < 0.01) from 1440 to 2007 for the southeastern Tibetan Plateau, based on tree rings of the forest fir (Abies forrestii). Persistent decadal dry intervals were found in the 1440s-1460s, 1560s-1580s, 1700s, 1770s, 1810s, 1860s and 1980s, and the extreme wet epochs were the 1480s-1490s, 1510s-1520s, 1590s, 1610s-1630s, 1720s-1730s, 1800s, 1830s, 1870s, 1930s, 1950s and after the 1990s. Comparisons of our record with those identified in other moisture related reconstructions for nearby regions showed that our reconstructed droughts were relatively consistent with those found in other regions of Indochina, suggesting similar drought regimes. Spectral peaks of 2.3-5.5 years may be indicative of ENSO activity, as also suggested by negative correlations with SSTs in the eastern equatorial and southeastern Pacific Ocean. Significant multidecadal spectral peaks of 29.2-40.9 and 56.8-60.2 years were identified. As indicated by the spatial correlation patterns, the decadal-scale variability may be linked to SST variations in the northern Pacific and Atlantic Oceans. © 2009 Springer-Verlag.en_US
dc.languageengen_US
dc.publisherSpringer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00382/index.htmen_US
dc.relation.ispartofClimate Dynamicsen_US
dc.subjectDroughten_US
dc.subjectNortheastern Tibetan Plateauen_US
dc.subjectPdsien_US
dc.subjectSsten_US
dc.subjectTree-Ringen_US
dc.titleReconstructed droughts for the southeastern Tibetan Plateau over the past 568 years and its linkages to the Pacific and Atlantic Ocean climate variabilityen_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.doi10.1007/s00382-009-0636-2en_US
dc.identifier.scopuseid_2-s2.0-77956095476en_US
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-77956095476&selection=ref&src=s&origin=recordpageen_US
dc.identifier.volume35en_US
dc.identifier.issue4en_US
dc.identifier.spage577en_US
dc.identifier.epage585en_US
dc.identifier.isiWOS:000281377200002-
dc.publisher.placeGermanyen_US
dc.identifier.scopusauthoridFang, K=19640101200en_US
dc.identifier.scopusauthoridGou, X=7003498424en_US
dc.identifier.scopusauthoridChen, F=7404907075en_US
dc.identifier.scopusauthoridLi, J=35272482700en_US
dc.identifier.scopusauthoridD'Arrigo, R=7003697159en_US
dc.identifier.scopusauthoridCook, E=7202259586en_US
dc.identifier.scopusauthoridYang, T=35191385500en_US
dc.identifier.scopusauthoridDavi, N=6508255585en_US

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