georefid:2006-012277SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1029/2002PA000825<gco:CharacterString>Timing of ice-age terminations determined by wavelet methods</gco:CharacterString>2003-01-01publicationgeorefid:2006-012277doi:10.1029/2002PA000825Hargreaves, Julia C.Frontier Research System for Global Change, Yokohama, JapanauthorAbe-Ouchi, AyakoUniversity of Tokyo, JapanauthorAmerican Geophysical Union, Washington, DC, United StatespublisherdocumentDigitalPaleoceanography18 (2)This paper presents a new analysis of four time series of paleoclimate data, using wavelet methods to determine the timings and characteristics of the ice-age terminations. An antisymmetric wavelet which detects locations in the time series where there are large changes is used. At the terminations the interval between atmospheric carbon dioxide changes and sea level is about 7 kyr. (modified journ. abstr.)completedQuaternary geologyAntarcticacarbon dioxideCenozoicchemical compositionclimate changeEast PacificEquatorial Pacificglaciationice coresisotope ratiosisotopesLeg 138North PacificNortheast PacificO-18/O-16Ocean Drilling ProgramODP Site 849oxygenPacific Oceanpaleo-oceanographypaleoatmospherepaleoclimatologypaleotemperatureQuaternarysea-level changesstable isotopesstatistical analysistime series analysiswaveletsurn:org.iodp:exp:138urnlargerWorkCitationcampaignurn:org.iodp:exp:138:site:849urnlargerWorkCitationstudyurn:org.iodp:exp:138urnlargerWorkCitationcampaignEnglishgeoscientificInformation-110.3111-110.31100.10580.1100application/pdfunknownSEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContacthttp://www.agu.org/journals/pa/pa0302/2002PA000825/2002PA000825.pdfdownload