Sea-level rise in Denmark: Bridging local reconstructions and global projections

Q2 Earth and Planetary Sciences Geological Survey of Denmark and Greenland Bulletin Pub Date : 2019-07-01 DOI:10.34194/GEUSB-201943-01-01
W. Colgan, J. Box, S. Ribeiro, K. Kjeldsen
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引用次数: 1

Abstract

Between 1850 and 2006 global mean sea level rose by 24 ± 18 cm. It is projected to rise a further 52 ± 21 cm under the Representative Concentration Pathway (RCP) 4.5 scenario, which approximates the carbon emissions reductions of the ‘Paris Agreement’ climate pathway. It is projected to rise 74 ± 28 cm under the RCP8.5 scenario, which represents a ‘business-as-usual’ climate pathway (Box & Colgan 2017). These rates of recent and future sea-level rise are faster than those reconstructed for previous warm intervals, such as the Medieval Climatic Optimum (c. 1000 to 1400 CE) and the Holocene Thermal Maximum (c. 7000 to 3000 BCE) (Gehrels & Shennan 2015). Moreover, palaeo reconstructions indicate a global sea-level sensitivity of two metres per degree of warming (Levermann et al. 2013). The forces driving global sea-level change are complex. The global sea-level budget includes the transfer of land ice into the ocean, thermal expansion of seawater, changes in land water storage, and changes in ocean basin volume (Church et al. 2013). At the local scale, the evolving planetary gravity due to shifting water and ice masses, shifting oceanic and atmospheric currents and persistent tectonic and glacial isostatic adjustment processes can also be important. Sea-level changes around the globe are therefore far from uniform (Jevrejeva et al. 2016). Here, we highlight the value of combining palaeo reconstructions of sea level, the measured tide gauge record, and projections of future sea level. This allows us to understand local sea-level changes from the recent past in the context of global projections for the near future (0 to 2100 CE). We explore the strong differences in local sea-level histories and future projections at three Danish cities: Skagen and Esbjerg, as they have contrasting glacio-isostatic adjustment histories, and Copenhagen, where we also compare local and global drivers of present-day sea-level rise based on previously published research.
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丹麦海平面上升:连接当地重建和全球预测
1850年至2006年间,全球平均海平面上升了24±18厘米。在代表性浓度路径(RCP) 4.5情景下(接近《巴黎协定》气候路径的碳减排),预计海平面将进一步上升52±21厘米。在RCP8.5情景下,预计海平面将上升74±28厘米,这代表了“一切照旧”的气候路径(Box & Colgan 2017)。这些近期和未来的海平面上升速度比以前的温暖间隔重建的速度要快,例如中世纪气候最佳期(公元前1000年至1400年)和全新世热最大值期(公元前7000年至3000年)(Gehrels & Shennan 2015)。此外,古重建表明,全球海平面的敏感度为每升温一度2米(Levermann et al. 2013)。推动全球海平面变化的力量是复杂的。全球海平面预算包括陆地冰向海洋的转移、海水的热膨胀、陆地储水量的变化和海洋盆地体积的变化(Church et al. 2013)。在局部尺度上,由移动的水和冰块、移动的海洋和大气流以及持续的构造和冰川均衡调整过程引起的行星重力演化也可能是重要的。因此,全球海平面变化远非均匀(Jevrejeva et al. 2016)。在这里,我们强调将古海平面重建、测潮仪记录和未来海平面预测结合起来的价值。这使我们能够在对不久的将来(公元0年至2100年)的全球预测的背景下,了解最近的过去的局部海平面变化。我们探索了丹麦三个城市在当地海平面历史和未来预测方面的巨大差异:斯卡恩和埃斯比约,因为它们具有对比鲜明的冰川均衡调整历史;哥本哈根,我们还根据先前发表的研究比较了当前海平面上升的本地和全球驱动因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
2.30
自引率
0.00%
发文量
0
审稿时长
>12 weeks
期刊介绍: GEUS Bulletin publishes geoscience research papers, monographs and map descriptions with a focus on Denmark, Greenland and the wider North Atlantic and Arctic region. We welcome submissions that fit this remit. Specifically, we publish: 1.Short articles intended as rapid communications that are of immediate interest to the international geoscience community (these include new research, datasets, methods or reviews) 2.Regular-length articles that document new research or a review of a topic of interest 3.Monographs (single volume works, by arrangement with the editorial office) 4.Maps and descriptive texts (produced by GEUS for Greenland and Denmark, by arrangement with the editorial office) GEUS Bulletin serves a broad geoscientific readership from research, industry, government agencies, NGOs and special interest groups.
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