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利用海底锚定帷幕保护冰盖的可行性。

Feasibility of ice sheet conservation using seabed anchored curtains.

作者信息

Keefer Bowie, Wolovick Michael, Moore John C

机构信息

Adjunct, Clean Energy Research Centre, University of British Columbia, 2329 West Mall, Vancouver BC V6T 1Z4, Canada.

College of Global Change and Earth Systems Science, Beijing Normal University, 19 Xinjiekouwai St, Haidian District, Beijing 100875, China.

出版信息

PNAS Nexus. 2023 Mar 28;2(3):pgad053. doi: 10.1093/pnasnexus/pgad053. eCollection 2023 Mar.

DOI:10.1093/pnasnexus/pgad053
PMID:37007716
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10062297/
Abstract

Sea level rise is expected to be rapid and extremely damaging to coastal communities and infrastructure, with unavoidable losses and coastal protection costs in the tens of billions per year. Retreat of the Thwaites and Pine Island Glaciers is likely already in an unstable regime as their oceanic fronts are ablated by deep intruding layers of relatively warm seawater. Warm water can be blocked from reaching the grounding line by thin flexible buoyant curtains anchored to the seabed. The consequent reduction in ice shelf melting could result in increased ice sheet buttressing as the shelf makes contact with seabed highs. Flexible curtains are less costly than solid artificial barriers, more robust against iceberg collisions, and easier to repair or remove in the event of unforeseen side effects. We illustrate the technical viability of this approach by considering curtain design concepts that should withstand oceanographic forces, and feasible methods of installation. Suitable materials are commonly available. Installation of a seabed curtain in temperate ocean waters would be entirely within the capabilities of existing offshore and deep ocean construction techniques. Installing in polar waters presents severe challenges from icebergs, harsh weather, and brief working seasons, which can however, be overcome with present-day technology. An 80 km long curtain installed in 600 m deep waters on alluvial sediments could help stabilize Pine Island and Thwaites glaciers over the next few centuries at much lower cost ($40-80 billion + $1-2 billion/yr maintenance) than the global coastline protection (∼$40 billion/yr) needed due to their collapse.

摘要

预计海平面上升速度将很快,对沿海社区和基础设施造成极大破坏,每年将不可避免地造成损失,沿海保护成本高达数百亿美元。由于相对温暖的海水深层侵入,导致它们的海洋前沿消融,思韦茨冰川和松岛冰川的退缩可能已经处于不稳定状态。通过固定在海床上的薄而灵活的浮力幕帘,可以阻止温水到达接地线。冰架融化的减少可能会导致冰盖支撑作用增强,因为冰架与海底高地接触。灵活的幕帘比坚固的人工屏障成本更低,在抵御冰山碰撞方面更坚固,并且在出现意外副作用时更易于修复或拆除。我们通过考虑应能承受海洋力量的幕帘设计概念以及可行的安装方法,来说明这种方法的技术可行性。合适的材料通常很容易获得。在温带海洋水域安装海底幕帘完全在现有近海和深海建设技术的能力范围内。在极地水域安装则面临来自冰山、恶劣天气和短暂工作季节的严峻挑战,不过,利用当今技术这些挑战是可以克服的。在600米深的冲积沉积物水域中安装一条80公里长的幕帘,在接下来的几个世纪里,有助于稳定松岛冰川和思韦茨冰川,其成本(400亿至800亿美元 + 每年10亿至20亿美元维护费用)远低于因它们崩塌而需要的全球海岸线保护成本(约每年400亿美元)。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/f7975c12a62e/pgad053f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/95806ad1d9ed/pgad053f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/45b7bff7db4c/pgad053f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/f7975c12a62e/pgad053f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/95806ad1d9ed/pgad053f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/45b7bff7db4c/pgad053f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/99bc/10062297/f7975c12a62e/pgad053f3.jpg

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引用本文的文献

1
The potential for stabilizing Amundsen Sea glaciers via underwater curtains.通过水下幕帘稳定阿蒙森海冰川的可能性。
PNAS Nexus. 2023 Mar 27;2(4):pgad103. doi: 10.1093/pnasnexus/pgad103. eCollection 2023 Apr.

本文引用的文献

1
The potential for stabilizing Amundsen Sea glaciers via underwater curtains.通过水下幕帘稳定阿蒙森海冰川的可能性。
PNAS Nexus. 2023 Mar 27;2(4):pgad103. doi: 10.1093/pnasnexus/pgad103. eCollection 2023 Apr.
2
Projections of global-scale extreme sea levels and resulting episodic coastal flooding over the 21st Century.21 世纪全球极端海平面预估及由此引发的突发性沿海洪灾。
Sci Rep. 2020 Jul 30;10(1):11629. doi: 10.1038/s41598-020-67736-6.
3
Pathways of ocean heat towards Pine Island and Thwaites grounding lines.大洋热量向松岛和思韦茨冰架接地线的传输途径。
Sci Rep. 2019 Nov 22;9(1):16649. doi: 10.1038/s41598-019-53190-6.
4
Mechanisms driving variability in the ocean forcing of Pine Island Glacier.驱动派恩岛冰川海洋强迫变化的机制。
Nat Commun. 2017 Feb 17;8:14507. doi: 10.1038/ncomms14507.
5
Marine ice sheet collapse potentially under way for the Thwaites Glacier Basin, West Antarctica.南极西部思韦茨冰川盆地的海洋冰架可能即将崩塌。
Science. 2014 May 16;344(6185):735-8. doi: 10.1126/science.1249055. Epub 2014 May 12.
6
Strong sensitivity of Pine Island ice-shelf melting to climatic variability.松岛冰架融化对气候变率的敏感性很强。
Science. 2014 Jan 10;343(6167):174-8. doi: 10.1126/science.1244341. Epub 2014 Jan 2.
7
A reconciled estimate of ice-sheet mass balance.一个被调和的冰盖物质平衡估计值。
Science. 2012 Nov 30;338(6111):1183-9. doi: 10.1126/science.1228102.