Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula

Estimating future sea level rise (SLR) projections is important for assessing coastal risks and planning of climate-resilient infrastructure. Therefore, in this study, we estimated the future projections of SLR from Coupled Model Intercomparison Project phase 6 (CMIP6) models for three climate targe...

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Published in:Journal of Marine Science and Engineering
Main Authors: Hyun Min Sung, Jisun Kim, Sungbo Shim, Jong-Chul Ha, Young-Hwa Byun, Yeon-Hee Kim
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/jmse9101094
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spelling ftmdpi:oai:mdpi.com:/2077-1312/9/10/1094/ 2023-08-20T04:09:45+02:00 Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula Hyun Min Sung Jisun Kim Sungbo Shim Jong-Chul Ha Young-Hwa Byun Yeon-Hee Kim agris 2021-10-07 application/pdf https://doi.org/10.3390/jmse9101094 EN eng Multidisciplinary Digital Publishing Institute Physical Oceanography https://dx.doi.org/10.3390/jmse9101094 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 9; Issue 10; Pages: 1094 Korean peninsula sea level rise climate change 1.5 °C warming emergence of climate change Text 2021 ftmdpi https://doi.org/10.3390/jmse9101094 2023-08-01T02:53:41Z Estimating future sea level rise (SLR) projections is important for assessing coastal risks and planning of climate-resilient infrastructure. Therefore, in this study, we estimated the future projections of SLR from Coupled Model Intercomparison Project phase 6 (CMIP6) models for three climate targets (1.5 °C (T15), 2.0 °C (T20), and 3.0 °C (T30)) described by the Paris Agreement. The global SLR projections are 60, 140, and 320 mm for T15, T20, and T30, respectively, relative to the present-day levels. Similarly, around the Korean Peninsula, SLR projections become more intense with continuous global warming (20 mm (T15), 110 mm (T20), and 270 mm (T30)). Ocean variables show a slow response to climate change. Therefore, we developed the Emergence of Climate Change (EoC) index for determining the time when the variable is not following the present climate trend. The EoC of SLR appears after the EoC of sea-ice melting near the time of T15 warming. Moreover, the EoC of thermal expansion appears around the 2040s, which is similar to the time of the maximum of the T15 warming period and the median of the T20 warming period. Overall, our analysis suggests that the T15 warming may act as a trigger and SLR will accelerate after the T15 warming. Text Sea ice MDPI Open Access Publishing Journal of Marine Science and Engineering 9 10 1094
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic Korean peninsula
sea level rise
climate change
1.5 °C warming
emergence of climate change
spellingShingle Korean peninsula
sea level rise
climate change
1.5 °C warming
emergence of climate change
Hyun Min Sung
Jisun Kim
Sungbo Shim
Jong-Chul Ha
Young-Hwa Byun
Yeon-Hee Kim
Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula
topic_facet Korean peninsula
sea level rise
climate change
1.5 °C warming
emergence of climate change
description Estimating future sea level rise (SLR) projections is important for assessing coastal risks and planning of climate-resilient infrastructure. Therefore, in this study, we estimated the future projections of SLR from Coupled Model Intercomparison Project phase 6 (CMIP6) models for three climate targets (1.5 °C (T15), 2.0 °C (T20), and 3.0 °C (T30)) described by the Paris Agreement. The global SLR projections are 60, 140, and 320 mm for T15, T20, and T30, respectively, relative to the present-day levels. Similarly, around the Korean Peninsula, SLR projections become more intense with continuous global warming (20 mm (T15), 110 mm (T20), and 270 mm (T30)). Ocean variables show a slow response to climate change. Therefore, we developed the Emergence of Climate Change (EoC) index for determining the time when the variable is not following the present climate trend. The EoC of SLR appears after the EoC of sea-ice melting near the time of T15 warming. Moreover, the EoC of thermal expansion appears around the 2040s, which is similar to the time of the maximum of the T15 warming period and the median of the T20 warming period. Overall, our analysis suggests that the T15 warming may act as a trigger and SLR will accelerate after the T15 warming.
format Text
author Hyun Min Sung
Jisun Kim
Sungbo Shim
Jong-Chul Ha
Young-Hwa Byun
Yeon-Hee Kim
author_facet Hyun Min Sung
Jisun Kim
Sungbo Shim
Jong-Chul Ha
Young-Hwa Byun
Yeon-Hee Kim
author_sort Hyun Min Sung
title Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula
title_short Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula
title_full Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula
title_fullStr Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula
title_full_unstemmed Sea Level Rise Drivers and Projections from Coupled Model Intercomparison Project Phase 6 (CMIP6) under the Paris Climate Targets: Global and around the Korea Peninsula
title_sort sea level rise drivers and projections from coupled model intercomparison project phase 6 (cmip6) under the paris climate targets: global and around the korea peninsula
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/jmse9101094
op_coverage agris
genre Sea ice
genre_facet Sea ice
op_source Journal of Marine Science and Engineering; Volume 9; Issue 10; Pages: 1094
op_relation Physical Oceanography
https://dx.doi.org/10.3390/jmse9101094
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse9101094
container_title Journal of Marine Science and Engineering
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