Anthropogenic Forcing of Antarctic Ice Loss (AnthroFAIL)
南极冰损的人为强迫(AnthroFAIL)
基本信息
- 批准号:NE/X000397/1
- 负责人:
- 金额:$ 63.42万
- 依托单位:
- 依托单位国家:英国
- 项目类别:Research Grant
- 财政年份:2023
- 资助国家:英国
- 起止时间:2023 至 无数据
- 项目状态:未结题
- 来源:
- 关键词:
项目摘要
Melting ice caps are widely viewed as illustrative of anthropogenic global warming. The largest ice mass on Earth - Antarctica - is losing ice, and may contribute 1 metre or more to global sea level by 2100. However, it is not clear that this ice loss has been caused by human activities. Instead, this ice sheet may be simply responding to natural variability in the climate system.Antarctic ice loss is primarily caused by increased melting of the ice sheet by the ocean. However, it is not known why this melting has changed. The deep ocean waters melting the West Antarctic Ice Sheet have been buried in the deep ocean for centuries, and have not simply warmed alongside the rest of the climate. Instead, changes in the winds are thought to have altered the transport of these warm waters towards Antarctica.This leads to two main possibilities for why Antarctica is losing ice. Firstly, anthropogenic changes in the winds, caused by greenhouse gases and/or the ozone hole, may have gradually increased the supply of warm water towards the ice sheet. Alternatively, natural variability of the winds may have caused a period of high melting that triggered a self-sustaining ice sheet retreat.It is now urgent that we understand whether human activities have increased the ocean melting of Antarctica. If the ice loss is caused by human activities, we must identify the best strategy for minimising future change. If the ice loss is natural and inevitable, we must prepare for the sea-level rise that will play out over the coming centuries. This project will carefully unpick the contributions of natural and human influences using computer simulations of the ocean surrounding West Antarctica. We will first use historical winds from climate models to drive a set of ocean simulations that comprise our 'best guess' of the real history of ocean melting of Antarctica since 1920, under all natural and human forcings. These simulations will be tested against available historical observations from ships, autonomous vehicles, and ocean sediment cores.Once we have this model history, we will work out how it has been influenced by each of the different forcings. We will perform large sets of ocean simulations with and without human greenhouse gases, the ozone hole, and natural climate variability. These simulations will tell us the contribution of each forcing to the oceanic melting of the West Antarctic Ice Sheet. When we have a good understanding of the role of historical forcings, we will be equipped to assess the impact of future forcings. The ozone hole is expected to recover before 2100, so the question is to what extent future emissions of greenhouse gases will overwhelm this recovery, and continue unchecked thereafter. This research will address the fundamental questions of whether humans have caused Antarctic ice loss, and whether there is anything we can now do about it. The answers to these questions are urgently needed to clarify our options for preventing or adapting to future sea-level rise.
冰盖融化被广泛认为是人为全球变暖的例证。地球上最大的冰块-南极洲-正在失去冰,到2100年可能会对全球海平面造成1米或更多的影响。然而,目前还不清楚这种冰层流失是由人类活动造成的。相反,这块冰盖可能只是对气候系统中的自然变化做出了反应。南极冰层的消失主要是由于海洋增加了冰盖的融化。然而,目前还不知道为什么这种融化会发生变化。融化了西南极冰盖的深海海水已经在深海中埋藏了几个世纪,而不仅仅是与其他气候一起变暖。相反,风的变化被认为改变了这些温暖的海水向南极洲的运输。这导致了南极洲正在融化冰的两种主要可能性。首先,温室气体和/或臭氧空洞引起的风的人为变化可能逐渐增加了向冰盖供应温暖的水。或者,风的自然变异性可能导致了一段时间的高度融化,引发了自我维持的冰盖后退。现在我们迫切需要了解人类活动是否加剧了南极洲的海洋融化。如果冰的流失是由人类活动造成的,我们必须确定将未来变化降至最低的最佳策略。如果冰层的消失是自然的和不可避免的,我们必须为海平面上升做好准备,海平面上升将在未来几个世纪上演。该项目将通过对西南极周围海洋的计算机模拟,仔细分析自然和人类影响的影响。我们将首先使用气候模型中的历史风来驱动一组海洋模拟,这些模拟包括我们对1920年以来在各种自然和人为因素作用下南极洲海洋融化的真实历史的最佳猜测。这些模拟将与来自船舶、自动驾驶车辆和海洋沉积物岩心的可用历史观测进行测试。一旦我们有了这个模型历史,我们就会计算出它是如何受到每一种不同的作用力的影响的。我们将在有或没有人类温室气体、臭氧空洞和自然气候变异性的情况下进行大量的海洋模拟。这些模拟将告诉我们每个作用力对西南极冰盖海洋融化的贡献。当我们对历史力量的作用有了很好的了解后,我们就有能力评估未来力量的影响。臭氧空洞预计将在2100年之前恢复,因此问题是,未来的温室气体排放将在多大程度上压倒这种恢复,并在此后继续不受控制。这项研究将解决人类是否导致南极冰川消失的根本问题,以及我们现在是否可以对此做些什么。迫切需要这些问题的答案,以澄清我们防止或适应未来海平面上升的各种选择。
项目成果
期刊论文数量(0)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
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Paul Holland其他文献
The Effect Technology has on Student Comprehension and Motivation
技术对学生理解和动机的影响
- DOI:
- 发表时间:
2016 - 期刊:
- 影响因子:0
- 作者:
Paul Holland - 通讯作者:
Paul Holland
Warm bath for an ice sheet
对冰原来说是温暖的沐浴
- DOI:
10.1038/ngeo801 - 发表时间:
2010-02-14 - 期刊:
- 影响因子:16.100
- 作者:
Paul Holland - 通讯作者:
Paul Holland
913. Histone Deacetylase Inhibitors Improve Gene Transfer To Mature Skeletal Muscle
- DOI:
10.1016/j.ymthe.2006.08.1003 - 发表时间:
2006-01-01 - 期刊:
- 影响因子:
- 作者:
Nancy Larochelle;Jatinderpal R. Deol;Paul Holland;George Karpati;Josephine Nalbantoglu - 通讯作者:
Josephine Nalbantoglu
66 Quantification of differences between semi-automated lung nodule volumetry software packages
66 半自动化肺结节体积测量软件包之间差异的量化
- DOI:
10.1016/j.lungcan.2025.108176 - 发表时间:
2025-02-01 - 期刊:
- 影响因子:4.400
- 作者:
Paul Holland;Emma O'Dowd;Bindu George;Iain Au-Yong;David Baldwin - 通讯作者:
David Baldwin
Paul Holland的其他文献
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{{ truncateString('Paul Holland', 18)}}的其他基金
Simulating UNder ice Shelf Extreme Topography (SUNSET)
模拟冰架下极端地形(日落)
- 批准号:
NE/X014061/1 - 财政年份:2023
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Drivers of Oceanic Change in the Amundsen Sea (DeCAdeS) (Joint Reference: W2980705)
阿蒙森海海洋变化的驱动因素 (DeCAdeS)(联合参考号:W2980705)
- 批准号:
NE/V010484/1 - 财政年份:2020
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Quantifying Human Influence on Ocean Melting of the West Antarctic Ice Sheet
量化人类对南极西部冰盖海洋融化的影响
- 批准号:
NE/S011994/1 - 财政年份:2019
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
The UK Earth system modelling project.
英国地球系统建模项目。
- 批准号:
NE/N01801X/1 - 财政年份:2016
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Characterising the Ice Shelf/Ocean Boundary Layer
描述冰架/海洋边界层的特征
- 批准号:
NE/N010027/1 - 财政年份:2016
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Is ice loss from West Antarctica driven by ocean forcing or ice and ocean feedbacks?
南极洲西部的冰损失是由海洋强迫还是冰和海洋反馈驱动的?
- 批准号:
NE/M001660/1 - 财政年份:2014
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Multi-Technique Bio-Analytical Investigation at the Single / Sub-Cellular Level Using a New Lab-On-A-Chip Technology Platform
使用新的芯片实验室技术平台在单/亚细胞水平上进行多技术生物分析研究
- 批准号:
EP/I038799/1 - 财政年份:2011
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Calculating the rate of Antarctic Bottom Water formation using new theory, fine-scale modelling and observations
利用新理论、精细尺度建模和观测计算南极底层水形成率
- 批准号:
NE/I025867/1 - 财政年份:2011
- 资助金额:
$ 63.42万 - 项目类别:
Research Grant
Collaborative Research on Social Networks: Mathematical Theory, Methods and Application
社交网络协同研究:数学理论、方法与应用
- 批准号:
7726823 - 财政年份:1978
- 资助金额:
$ 63.42万 - 项目类别:
Standard Grant
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