Poles apart: why has Antarctic sea ice increased, and why can't coupled climate models reproduce observations?

两极分化：为什么南极海冰增加，为什么耦合气候模型不能重现观测结果？

• 批准号: NE/K011561/1
• 负责人: Yevgeny Aksenov
• 金额: $ 8.61万
• 依托单位: NATIONAL OCEANOGRAPHY CENTRE
• 依托单位国家: 英国
• 项目类别: Research Grant
• 财政年份: 2014
• 资助国家: 英国
• 起止时间: 2014 至 无数据
• 项目状态: 已结题
• 来源: https://gtr.ukri.org/projects?ref=NE%2FK011561%2F1
• 关键词: Poles; apart; why; Antarctic; sea

Due to its pale colour, sea ice reflects much of the incoming solar radiation back into space, keeping local temperatures relatively cold. However, if warming occurs and sea ice melts, it is replaced by darker ocean. This absorbs more solar energy, causing warming, and so the cycle, the so-called 'ice-albedo feedback' loop, continues. Sea ice also modifies the regional surface energy balance by capping the upper layer of the ocean, reducing its loss of heat to the atmosphere. In addition, sea ice is important because it plays a role in the exchange of carbon dioxide between the atmosphere and ocean, thereby affecting how much of this greenhouse gas is in the atmosphere and contributing to global warming. Moreover, sea ice formation is an important element in driving the global thermohaline circulation of heat and salt through the world's oceans. One component of this circulation is the North Atlantic Drift current that carries warm tropical water across the Atlantic and keeps the UK's winter temperatures much warmer than they would be otherwise.The Intergovernmental Panel on Climate Change (IPCC) assessment reports are an important tool in drivng government policy around the world. However, the present generation of climate models, which are used to predict the future climate scenarios described in these reports, are unable to consistently reproduce the recent increase in Antarctic sea ice. As a result considerable uncertainty must be attached to their predictions of future climate.This proposal aims to both advance our understanding of the Earth's climate and facilitate improved predictions of its future change to aid policy makers. This will be achieved through the following objectives: 1. To explain the key climate processes involved in the recent Antarctic sea ice increase. We know from observations that changes in the near-surface wind around Antarctica are predominantly responsible for the observed increase in sea ice but we don't know exactly how the wind and the ice interact. Using a state-of-the-art computer model of sea ice and the ocean forced by the latest atmospheric data we will establish the key processes through which changes in the wind are causing the ice to increase.2. To establish the ultimate driver of the sea ice increase. Policymakers need to know whether we can attribute the observed changes in Antarctic sea ice to human activity. This might happen through changes in the near-surface winds around Antarctica caused by the 'ozone hole' or greenhouse gas increases for example. Alternatively, it may be simply due to natural variations in the Antarctic climate system. If the former is true, we must determine which human activities are responsible. If the latter is correct, we must try to understand connections between the key processes and wider aspects of the climate system.3. To understand why current climate models fail to simulate the growth in Antarctic sea ice. We will examine the current UK climate model in detail to diagnose which components are to blame and, with our Met Office partner, we will design a development programme to ensure that our findings are transferred into future model improvements in time for the next IPCC report. To help other climate model developers around the world, we will also analyse whether the failings are common to the other models used in the IPCC reports.

由于颜色苍白，海冰将大部分进入太空的太阳辐射反射回太空，使当地温度保持在相对较低的水平。然而，如果发生变暖和海冰融化，它就会被更暗的海洋所取代。这会吸收更多的太阳能，导致气候变暖，因此这种循环，即所谓的“冰-反照率反馈”循环，会继续下去。海冰还通过覆盖海洋上层来改变区域表面能量平衡，减少其向大气中的热量损失。此外，海冰很重要，因为它在大气和海洋之间的二氧化碳交换中发挥作用，从而影响大气中这种温室气体的数量，并导致全球变暖。此外，海冰的形成是推动通过世界海洋的热和盐的全球温盐循环的重要因素。这种环流的一个组成部分是北大西洋漂流，它携带温暖的热带水横跨大西洋，使英国的冬季气温比其他情况下高得多。政府间气候变化专门委员会(IPCC)的评估报告是推动世界各地政府政策的重要工具。然而，用于预测这些报告中描述的未来气候情景的当代气候模型，无法始终如一地再现最近南极海冰的增加。因此，他们对未来气候的预测必须具有相当大的不确定性。这项建议旨在增进我们对地球气候的了解，并促进对未来气候变化的更好预测，以帮助决策者。这将通过以下目标来实现：1.解释最近南极海冰增加所涉及的关键气候过程。我们从观测中得知，南极洲周围近地表风的变化是观测到的海冰增加的主要原因，但我们不清楚风和冰是如何相互作用的。使用最先进的海冰和受最新大气数据强迫的海洋的计算机模型，我们将建立关键的过程，通过这些过程，风的变化导致冰的增加。以确定海冰增加的终极驱动力。政策制定者需要知道，我们是否可以将观察到的南极海冰变化归因于人类活动。例如，这可能是因为南极洲周围近地表的风发生了变化，而这些风是由“臭氧层空洞”或温室气体增加引起的。或者，这可能仅仅是由于南极气候系统的自然变化。如果前者是真的，我们必须确定哪些人类活动负有责任。如果后者是正确的，我们必须努力理解气候系统的关键过程和更广泛的方面之间的联系。来理解为什么目前的气候模型不能模拟南极海冰的生长。我们将详细研究英国当前的气候模型，以诊断哪些因素是罪魁祸首，并将与英国气象局合作伙伴一起，设计一项发展计划，以确保我们的研究结果及时转化为未来的模型改进，以便IPCC下一份报告。为了帮助世界各地的其他气候模型开发者，我们还将分析这些失败是否与IPCC报告中使用的其他模型相同。

项目成果

Waves, Ice and Ocean in future projections of the Arctic and Southern Ocean.

北冰洋和南大洋未来预测中的波浪、冰和海洋。

• 发表时间: 2018
• 作者: Aksenov, Y.

Model sensitivity of the Weddell and Ross seas, Antarctica, to vertical mixing and freshwater forcing

• DOI: 10.1016/j.ocemod.2015.08.003
• 发表时间: 2015-10
• 期刊: Ocean Modelling
• 影响因子: 3.2
• 作者: J. Kjellsson;P. Holland;G. Marshall;P. Mathiot;Y. Aksenov;A. Coward;S. Bacon;A. Megann;J. Ridley

The effects of tides on the water mass mixing and sea ice in the Arctic Ocean

• DOI: 10.1002/2014jc010310
• 发表时间: 2015-10
• 期刊: Journal of Geophysical Research
• 作者: M. Luneva;Y. Aksenov;J. Harle;J. Holt

GO5.0: The joint NERC-Met Office NEMO global ocean model for use in coupled and forced applications

• DOI: 10.5194/gmd-7-1069-2014
• 发表时间: 2013-11
• 期刊: Geoscientific Model Development
• 影响因子: 5.1
• 作者: A. Megann;D. Storkey;Y. Aksenov;S. Alderson;D. Calvert;T. Graham;P. Hyder;J. Siddorn;B. Sinha-B.-S

Impact of sea ice floe size distribution on seasonal fragmentation and melt of Arctic sea ice

• DOI: 10.5194/tc-14-403-2020
• 发表时间: 2020-02-04
• 期刊: CRYOSPHERE
• 影响因子: 5.2
• 作者: Bateson, Adam W.;Feltham, Daniel L.;Aksenov, Yevgeny
• 通讯作者: Aksenov, Yevgeny