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dc.contributor.authorHartland, Adamen_NZ
dc.contributor.authorHu, Chaoyongen_NZ
dc.contributor.authorEnge, Gabrielen_NZ
dc.contributor.authorZitoun, Rebeccaen_NZ
dc.contributor.authorLehto, Niklasen_NZ
dc.contributor.authorSalmanzadeh, Mahdiyehen_NZ
dc.contributor.authorFox, Beth R.S.en_NZ
dc.contributor.authorDosseto, Anthonyen_NZ
dc.contributor.authorBreitenbach, Sebastianen_NZ
dc.coverage.spatialVienna, Austriaen_NZ
dc.date.accessioned2019-07-25T03:09:40Z
dc.date.available2018en_NZ
dc.date.available2019-07-25T03:09:40Z
dc.date.issued2018en_NZ
dc.identifier.citationHartland, A., Hu, C., Enge, G., Zitoun, R., Lehto, N., Salmanzadeh, M., … Breitenbach, S. (2018). Towards a quantitative proxy of cave dripwater hydrology. In European Geosciences Union General Assembly 2018 (Vol. 20, pp. 13780–13780). Vienna, Austria.en
dc.identifier.urihttps://hdl.handle.net/10289/12729
dc.description.abstractSpeleothems capture a wide range of geochemical signals related to hydroclimate variability. However, the quantification of climatic parameters (e.g. rainfall, temperature) using traditional proxies is hampered by the multitude of influencing factors.
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.relation.urihttps://meetingorganizer.copernicus.org/EGU2018/EGU2018-13780.pdfen_NZ
dc.rights© Author(s) 2018. CC Attribution 4.0 license.
dc.titleTowards a quantitative proxy of cave dripwater hydrologyen_NZ
dc.typeConference Contribution
dc.relation.isPartOfEuropean Geosciences Union General Assembly 2018en_NZ
pubs.begin-page13780
pubs.elements-id238834
pubs.end-page13780
pubs.publisher-urlhttps://www.egu.eu/en_NZ
pubs.volume20en_NZ


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