Dataset:
Transient experiment of MIS 3 performed with LOVECLIM

dc.coverage.spatial Global en_US
dc.date.accessioned 2021-11-26T10:01:44Z
dc.date.available 2021-11-26T10:01:44Z
dc.date.issued 2020 en_US
dc.description.abstract LOVECLIM transiently forced by changes in orbital parameters (Berger 1978), NH ice-sheet topography and albedo (Abe-Ouchi et al., 2013), and pCO2 (Luthi et al., 2008), as well as meltwater input in the North Atlantic to simulate D-O variability en_US
dc.identifier.uri http://hdl.handle.net/1959.4/resource/collection/resdatac_1054/1
dc.language English
dc.language.iso EN en_US
dc.rights CC-BY-ND en_US
dc.rights.uri https://creativecommons.org/licenses/by-nd/4.0/ en_US
dc.subject.other Dansgaard-Oeschger cycles en_US
dc.subject.other Heinrich events en_US
dc.subject.other AMOC en_US
dc.subject.other Abrupt climate changes en_US
dc.title Transient experiment of MIS 3 performed with LOVECLIM en_US
dc.type Dataset en_US
dcterms.accessRights open access
dcterms.rightsHolder Copyright 2014, University of New South Wales en_US
dspace.entity.type Dataset en_US
unsw.accessRights.uri https://purl.org/coar/access_right/c_abf2
unsw.contributor.leadChiefInvestigator Menviel, Laurie
unsw.contributor.researchDataCreator Menviel, Laurie en_US
unsw.description.storageplace CCRC, BEES, Science en_US
unsw.identifier.doi https://doi.org/10.26190/5f3c9d0ade737 en_US
unsw.isPublicationRelatedToDataset Menviel, L, Timmermann, A, Friedrich, T & England, M 2014, 'Hindcasting the continuum of Dansgaard-Oeschger variability: mechanisms, patterns and timing', Climate of the Past, vol. 10, no. 1, pp. 63-77. https://doi.org/10.5194/cp-10-63-2014 en_US
unsw.relation.FunderRefNo FT180100606
unsw.relation.OriginalPublicationAffiliation Menviel, Laurie, Biological| Earth & Env Sci, Faculty of Science, en_US
unsw.relation.faculty Science
unsw.relation.fundingAgency AUSTRALIAN RESEARCH COUNCIL
unsw.relation.fundingScheme FUTURE FELLOWSHIP
unsw.relation.projectDesc the oceanic circulation varied significantly over the last glacial cycle (~140,000 years) and is expected to change over the coming centuries due to rising atmospheric co2. this project aims to understand the impact of changes in ocean circulation on marine biogeochemistry, climate and ultimately the antarctic ice-sheet by combining transient simulations of the last glacial cycle performed with an earth system model with compilation of paleoproxy records. the impact of future changes in oceanic circulation on ocean acidification and oxygen content will be further assessed with a state-of-the-art high-resolution ocean, carbon cycle model. this project will lead to improved understanding of processes and feedbacks within the earth system.
unsw.relation.projectEndDate 2023-02-28
unsw.relation.projectStartDate 2019-02-28
unsw.relation.projectTitle past to future changes in ocean dynamics and biogeochemistry en_US
unsw.relation.school School of Biological, Earth & Environmental Sciences
unsw.relation.unswGrantNo RG173035
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