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ContributorThe Pennsylvania State University CiteSeerX Archives-
AuthorEdward R. Cook-
AuthorRosanne D. D’arrigo-
AuthorJonathan G. Palmer-
Other Identifierhttp://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.568.8271-
Other Identifierhttp://ruby.fgcu.edu/courses/twimberley/EnviroPhilo/CookPalmer.pdf-
URIhttps://www.amad.org/jspui/handle/123456789/65835-
Descriptionin the Southern Hemisphere is uncertain because of the paucity of well-dated, high-resolution paleo-temperature records covering the past 1,000 years. We describe a new tree-ring reconstruction of Austral summer temperatures from the South Island of New Zealand, covering the past 1,100 years. This record is the longest yet produced for New Zealand and shows clear evidence for persistent above-average temperatures within the interval commonly assigned to the MWP. Comparisons with selected temperature proxies from the Northern and Southern Hemispheres confirm that the MWP was highly variable in time and space. Regardless, the New Zealand temperature reconstruction supports the global occurrence of the-
Formatapplication/pdf-
Languageeng-
RightsMetadata may be used without restrictions as long as the oai identifier remains attached to it.-
Keywords3344 Meteorology and-
KeywordsClimatology (1620-
KeywordsDynamics-
Dewey Decimal Classification940-
TitleEvidence for a ‘‘Medieval Warm Period’’ in a 1,100 year tree-ring reconstruction of past austral summer temperatures-
Typetext-
AMAD ID568318-
Open Access1-
Appears in Collections:BASE (Bielefeld Academic Search Engine)
General history of Europe


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