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dc.contributor.authorLjungqvist, Fredrik Charpentier
dc.date.accessioned2021-08-17T00:37:05Z
dc.date.available2021-08-17T00:37:05Z
dc.date.issued2011
dc.date.issued2011
dc.identifier.urihttp://hdl.handle.net/20.500.11956/133136
dc.description.abstractThis article presents a review of the spatio-temporal pattern of the mid-Holocene Thermal Maximum as it occurs in 60 different reconstructions of annual mean temperature from locations around the globe. The geographical coherency of multi-centennial periods with annual mean temperatures at least 1°C and 2°C above the pre-industrial (~1750 AD) equivalents are presented. Although the reconstructions show a heterogeneous temperature pattern for the period c. 10-8 ka BP, a rather coherent period of temperatures exceeding the pre-industrial ones are seen for c. 8-4 ka BP. The onset of the Neoglaciation takes place 4-3 ka BP and cumulates during the Little Ice Age (c. 1300-1900 AD). Overall, our review points towards a more homogeneous mid-Holocene Thermal Maximum than hitherto reported. However, the still limited data coverage, especially for the Southern Hemisphere, restricts the possibility to draw any firm conclusion regarding the amplitude and spatio-temporal pattern of the maximum mid- Holocene warming.en
dc.language.isoen
dc.relation.urihttp://geography.cz/sbornik/wp-content/uploads/2011/06/g11-2-1ljungqvist.pdf
dc.titleThe spatio-temporal pattern of the mid-holocene thermal maximum =Časoprostorový model teplotních maxim středního holocénuen
dc.description.startPage91
dc.description.endPage110
dcterms.isPartOf.nameGeografie. Sborník České geografické společnostien
dcterms.isPartOf.journalYear2011
dcterms.isPartOf.journalVolume116
dcterms.isPartOf.journalIssue2
dcterms.isPartOf.issn1212-0014
dc.identifier.lisID000164561


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