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dc.contributor.authorSeip, Knut Lehre
dc.contributor.authorWang, Hui
dc.date.accessioned2023-06-14T07:36:57Z
dc.date.available2023-06-14T07:36:57Z
dc.date.created2023-02-19T11:55:10Z
dc.date.issued2023
dc.identifier.issn0177-798X
dc.identifier.issn1434-4483
dc.identifier.urihttps://hdl.handle.net/11250/3071271
dc.description.abstractWe find that maximal decadal Northern Hemisphere warming increases as rapidly before as after the industrial revolution (0.86 °C decade−1 before 1880 and 0.60–0.68 °C decade−1 after 1880). However, whereas the number of decadal periods with large increase and decrease rates were about equal before 1880 (267 vs. 273), after 1880 there are more periods with high increase rates (35) than with high decrease rates (9). The same patterns hold for bi-decadal rates. However, for time windows greater than about 20 years, the slope in global warming with time becomes greater after 1880. After 1971, there is only one short 11 year period with negative slopes. This reflects the higher frequency of positive slopes during the industrial period caused by the contribution of greenhouse gases (GHG). Maximum temperature changes for detrended series were associated with the beginning and end of extreme warm or cold sub periods. They occurred throughout all of the Common Era. Because the detrended temperature series showed sign of a pacemaker mechanism (regular cycle periods) we suggest that ocean variabilities were a dominating mechanism for multidecadal temperature variability during the Common Era.en_US
dc.language.isoengen_US
dc.publisherSpringeren_US
dc.relation.ispartofseriesTheoretical and Applied Climatology;
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleMaximum Northern Hemisphere warming rates before and after 1880 during the Common Eraen_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
cristin.ispublishedfalse
cristin.fulltextpostprint
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.doihttps://doi.org/10.1007/s00704-023-04398-0
dc.identifier.cristin2127277
dc.source.journalTheoretical and Applied Climatologyen_US


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