Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/168869
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dc.contributor.authorShaw, Timothy Adamen_US
dc.contributor.authorLi, Tanghuaen_US
dc.contributor.authorNg, Trinaen_US
dc.contributor.authorCahill, Niamhen_US
dc.contributor.authorChua, Stephenen_US
dc.contributor.authorMajewski, Jedrzej M.en_US
dc.contributor.authorNathan, Yudhishthraen_US
dc.contributor.authorGarner, Gregory G.en_US
dc.contributor.authorKopp, Robert E.en_US
dc.contributor.authorHanebuth, Till J. J.en_US
dc.contributor.authorSwitzer, Adam D.en_US
dc.contributor.authorHorton, Benjamin Peteren_US
dc.date.accessioned2023-06-21T03:02:43Z-
dc.date.available2023-06-21T03:02:43Z-
dc.date.issued2023-
dc.identifier.citationShaw, T. A., Li, T., Ng, T., Cahill, N., Chua, S., Majewski, J. M., Nathan, Y., Garner, G. G., Kopp, R. E., Hanebuth, T. J. J., Switzer, A. D. & Horton, B. P. (2023). Deglacial perspectives of future sea level for Singapore. Communications Earth & Environment, 4(1), 204-. https://dx.doi.org/10.1038/s43247-023-00868-5en_US
dc.identifier.issn2662-4435en_US
dc.identifier.urihttps://hdl.handle.net/10356/168869-
dc.description.abstractLow elevation equatorial and tropical coastal regions are highly vulnerable to sea level rise. Here we provide probability perspectives of future sea level for Singapore using regional geological reconstructions and instrumental records since the last glacial maximum ~21.5 thousand years ago. We quantify magnitudes and rates of sea-level change showing deglacial sea level rose from ~121 m below present level and increased at averaged rates up to ~15 mm/yr, which reduced the paleogeographic landscape by ~2.3 million km2. Projections under a moderate emissions scenario show sea level rising 0.95 m at a rate of 7.3 mm/yr by 2150 which has only been exceeded (at least 99% probability) during rapid ice mass loss events ~14.5 and ~9 thousand years ago. Projections under a high emissions scenario incorporating low confidence ice-sheet processes, however, have no precedent during the last deglaciation.en_US
dc.description.sponsorshipMinistry of Education (MOE)en_US
dc.description.sponsorshipNational Environmental Agency (NEA)en_US
dc.description.sponsorshipNational Research Foundation (NRF)en_US
dc.language.isoenen_US
dc.relationMOE2019-T3-1-004en_US
dc.relationMOE-T2EP50120-0007en_US
dc.relation.ispartofCommunications Earth & Environmenten_US
dc.relation.uri10.21979/N9/LI3E6Fen_US
dc.rights© 2023 The Author(s). This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.en_US
dc.titleDeglacial perspectives of future sea level for Singaporeen_US
dc.typeJournal Articleen
dc.contributor.schoolAsian School of the Environmenten_US
dc.contributor.researchEarth Observatory of Singaporeen_US
dc.identifier.doi10.1038/s43247-023-00868-5-
dc.description.versionPublished versionen_US
dc.identifier.scopus2-s2.0-85161423401-
dc.identifier.issue1en_US
dc.identifier.volume4en_US
dc.identifier.spage204en_US
dc.subject.keywordsFuture Sea Levelen_US
dc.subject.keywordsSingaporeen_US
dc.description.acknowledgementThis research was supported by the Earth Observatory of Singapore grants M4430132.B50- 2014, M4430139.B50-2015, M4430188.B50-2016, M4430245.B50-2017 and M4430245.B50-2018. T.A.S., T.L., S.C., J.M.M., A.D.S. and B.P.H. were supported by the Singapore Ministry of Education Academic Research Fund MOE2019-T3-1-004 and MOE- T2EP50120-0007, the National Research Foundation Singapore, the Singapore Ministry of Education under the Research Centers of Excellence initiative, and by Nanyang Techno- logical University. This Research/Project is supported by the National Research Foundation, Singapore, and National Environment Agency, Singapore under the National Sea Level Programme Funding Initiative (award No. USS-IF-2020-1). Any opinions, findings and conclusions or recommendations expressed in this material are those of the author(s) and do not reflect the views of the National Research Foundation, Singapore and the National Environment Agency, Singapore. N.C. research is conducted with the financial support of Science Foundation Ireland and co-funded by Geological Survey Ireland under Grant number 20/FFP-P/8610. R.E.K. and G.G.G. were supported by U.S. National Science Foundation award ICER-2103754 as part of the Megalopolitan Coastal Transformation Hub (MACH) and by the National Aeronautics and Space Administration (award 80NSSC20K1724 and JPL task 105393.509496.02.08.13.31).en_US
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