Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/168869
Title: Deglacial perspectives of future sea level for Singapore
Authors: Shaw, Timothy Adam
Li, Tanghua
Ng, Trina
Cahill, Niamh
Chua, Stephen
Majewski, Jedrzej M.
Nathan, Yudhishthra
Garner, Gregory G.
Kopp, Robert E.
Hanebuth, Till J. J.
Switzer, Adam D.
Horton, Benjamin Peter
Issue Date: 2023
Source: Shaw, 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/s43247-023-00868-5
Project: MOE2019-T3-1-004 
MOE-T2EP50120-0007 
Journal: Communications Earth & Environment 
Abstract: Low 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.
URI: https://hdl.handle.net/10356/168869
ISSN: 2662-4435
DOI: 10.1038/s43247-023-00868-5
DOI (Related Dataset): 10.21979/N9/LI3E6F
Schools: Asian School of the Environment 
Research Centres: Earth Observatory of Singapore 
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/.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:ASE Journal Articles
EOS Journal Articles

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