Impact of Southern Ocean convection on the climate and carbon cycle

doi:10.26190/5efe7c8c75bd5

Dataset:

Impact of Southern Ocean convection on the climate and carbon cycle

dc.coverage.spatial	Global	en_US
dc.date.accessioned	2021-11-26T09:53:08Z
dc.date.available	2021-11-26T09:53:08Z
dc.date.issued	2020	en_US
dc.description.abstract	Transient simulations of the last glacial period performed with two Earth System models of intermediate complexity (LOVECLIM and the UVic ESM). The impact of North Atlantic meltwater input, and Southern Ocean convection on climate and carbon cycle are studied.	en_US
dc.identifier.uri	http://hdl.handle.net/1959.4/resource/collection/resdatac_1038/1
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	Heinrich events	en_US
dc.subject.other	atmospheric CO2	en_US
dc.subject.other	Southern Ocean convection	en_US
dc.subject.other	AMOC	en_US
dc.title	Impact of Southern Ocean convection on the climate and carbon cycle	en_US
dc.type	Dataset	en_US
dcterms.accessRights	open access
dcterms.accrualMethod	Transient simulations of the last glacial period performed with two Earth System models of intermediate complexity (LOVECLIM and the UVic ESM). The models are forced by changes in insolation (Berger, 1978), and NH ice-sheet topography, extent and albedo (Abe-Ouchi et al., 2007). Meltwater input in the North Atlantic are added to simulate the millennial-scale variability. Atmospheric CO2 is prognostic.	en_US
dcterms.rightsHolder	Copyright 2015, 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, Science	en_US
unsw.identifier.doi	https://doi.org/10.26190/5efe7c8c75bd5	en_US
unsw.isPublicationRelatedToDataset	Menviel, L, Spence, P & England, M 2015, 'Contribution of enhanced Antarctic Bottom Water formation to Antarctic warm events and millennial-scale atmospheric CO2 increase', Earth and Planetary Science Letters, vol. 413, pp. 37-50, https://doi.org/10.1016/j.epsl.2014.12.050	en_US
unsw.isPublicationRelatedToDataset	Skinner, L., Menviel, L., Broadfield, L. et al. Southern Ocean convection amplified past Antarctic warming and atmospheric CO2 rise during Heinrich Stadial 4. Commun Earth Environ 1, 23 (2020). https://doi.org/10.1038/s43247-020-00024-3	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