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dc.date.accessioned2020-05-27T19:43:26Z
dc.date.available2020-05-27T19:43:26Z
dc.date.created2019-11-22T11:44:51Z
dc.date.issued2019
dc.identifier.citationHolme, Christian Gkinis, Vasileios Lanzky, Mika Morris, Valerie Olesen, Martin Thayer, Abigail Vaughn, Bruce H Vinther, Bo M. . Varying regional δ18O–temperature relationship in high-resolution stable water isotopes from east Greenland. Climate of the Past. 2019, 15(3), 893-912
dc.identifier.urihttp://hdl.handle.net/10852/76364
dc.description.abstractThis study examines the stable water isotope signal (δ18O) of three ice cores drilled on the Renland peninsula (east Greenland coast). While ice core δ18O measurements qualitatively are a measure of the local temperature history, the δ18O variability in precipitation actually reflects the integrated hydrological activity that the deposited ice experienced from the evaporation source to the condensation site. Thus, as Renland is located next to fluctuating sea ice cover, the transfer function used to infer past temperatures from the δ18O variability is potentially influenced by variations in the local moisture conditions. The objective of this study is therefore to evaluate the δ18O variability of ice cores drilled on Renland and examine the amount of the signal that can be attributed to regional temperature variations. In the analysis, three ice cores are utilized to create stacked summer, winter and annually averaged δ18O signals (1801–2014 CE). The imprint of temperature on δ18O is first examined by correlating the δ18O stacks with instrumental temperature records from east Greenland (1895–2014 CE) and Iceland (1830–2014 CE) and with the regional climate model HIRHAM5 (1980–2014 CE). The results show that the δ18O variability correlates with regional temperatures on both a seasonal and an annual scale between 1910 and 2014, while δ18O is uncorrelated with Iceland temperatures between 1830 and 1909. Our analysis indicates that the unstable regional δ18O–temperature correlation does not result from changes in weather patterns through strengthening and weakening of the North Atlantic Oscillation. Instead, the results imply that the varying δ18O–temperature relation is connected with the volume flux of sea ice exported through Fram Strait (and south along the coast of east Greenland). Notably, the δ18O variability only reflects the variations in regional temperature when the temperature anomaly is positive and the sea ice export anomaly is negative. It is hypothesized that this could be caused by a larger sea ice volume flux during cold years which suppresses the Iceland temperature signature in the Renland δ18O signal. However, more isotope-enabled modeling studies with emphasis on coastal ice caps are needed in order to quantify the mechanisms behind this observation. As the amount of Renland δ18O variability that reflects regional temperature varies with time, the results have implications for studies performing regression-based δ18O–temperature reconstructions based on ice cores drilled in the vicinity of a fluctuating sea ice cover.en_US
dc.languageEN
dc.publisherCopernicus Publications under license by EGU – European Geosciences Union GmbH
dc.rightsAttribution 4.0 International
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.titleVarying regional δ18O–temperature relationship in high-resolution stable water isotopes from east Greenlanden_US
dc.typeJournal articleen_US
dc.creator.authorHolme, Christian
dc.creator.authorGkinis, Vasileios
dc.creator.authorLanzky, Mika
dc.creator.authorMorris, Valerie
dc.creator.authorOlesen, Martin
dc.creator.authorThayer, Abigail
dc.creator.authorVaughn, Bruce H
dc.creator.authorVinther, Bo M.
cristin.unitcode185,15,22,60
cristin.unitnameSeksjon for naturgeografi og hydrologi
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin1750921
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Climate of the Past&rft.volume=15&rft.spage=893&rft.date=2019
dc.identifier.jtitleClimate of the Past
dc.identifier.volume15
dc.identifier.issue3
dc.identifier.startpage893
dc.identifier.endpage912
dc.identifier.doihttps://doi.org/10.5194/cp-15-893-2019
dc.identifier.urnURN:NBN:no-79430
dc.type.documentTidsskriftartikkelen_US
dc.type.peerreviewedPeer reviewed
dc.source.issn1814-9324
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/76364/1/cp-15-893-2019.pdf
dc.type.versionPublishedVersion


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