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Asymmetries in ocean heat and carbon uptake, and effects on marine hazards

海洋热量和碳吸收的不对称性及其对海洋危害的影响

基本信息

批准号：
NE/T007788/1
负责人：
Richard Williams
金额：
$ 82.36万
依托单位：
University of Liverpool
依托单位国家：
英国
项目类别：
Research Grant
财政年份：
2020
资助国家：
英国
起止时间：
2020 至无数据
项目状态：
未结题

来源：
https://gtr.ukri.org/projects?ref=NE%2FT007788%2F1
关键词：
Asymmetries ocean heat carbon uptake

项目摘要

We need to understand what the future holds for the ocean, as more heat and carbon are supplied to the climate system. We know that the ocean is taking up over 90% of the extra heat supplied to the climate system and typically 25% of the extra carbon emitted to the climate system. We know that the ocean plays a central role in determining how global-mean surface warming is proportional to the cumulative amount of carbon emitted to the atmosphere. However, there are large uncertainties in this linear dependence of warming on carbon emissions. Reducing this uncertainty is an urgent task for climate science in order to reliably estimate the remaining carbon budget for specific warming targets, such as those set by the Paris Agreement.Our work has demonstrated that the inter-model uncertainty in how surface warming relates to carbon emissions depends on the uncertainties in climate feedbacks involving clouds, ocean heat uptake and ocean carbon uptake. In order to gain understanding and to reduce the uncertainties, we need to identify the regional contributions to climate feedbacks, ocean heat and carbon uptake that make up the global response of the climate system.How the regional ocean takes up the extra heat and carbon supplied to the climate system are also important in affecting the likelihood of marine hazards occurring, such as marine heatwaves and ocean acidifying events. Accordingly, we need to know why some ocean regions are gaining the extra heat or carbon added to the climate system faster than other regions over the globe. We need to understand the drivers for this regional ocean heat and carbon uptake. These drivers range from 1. The extra heat and carbon supplied to the ocean is carried by a steady circulation over the global ocean, suggesting that the patterns of extra heat and carbon gain are similar in sign to each other;2. The ocean drives changes in heat and carbon gain by time-varying changes in the circulation, suggesting that the patterns of extra heat and carbon gain may have opposing signs to each other;3. The atmosphere drives changes in heat and carbon by differences in air-sea exchange, with cloud feedbacks acting to strengthen warm anomalies in the subtropics and weaken warm anomalies in the Southern Ocean. We need to understand the drivers of these ocean heat and carbon anomalies as the resulting changes in the ocean environment affects the likelihood of marine hazards. For example, marine heatwaves are periods of enhanced temperature, lasting weeks to months, and their likelihood is affected by the regional pattern of how the ocean takes up the extra heat supplied to the climate system. The combination of temperature and carbon changes may alter the pH of the ocean leading to ocean acidifying events. We need to identify whether marine heatwaves and ocean acidifying events are likely to reinforce each other.In conclusion, we will provide a new view of how anthropogenic heat and carbon anomalies are controlled, identifying their asymmetries, the ocean and atmospheric drivers, and implications for the global climate response and marine hazards.This work is directly relevant to two Grand Challenges of the World Climate Research programme on "Clouds, circulation and climate sensitivity" and "Carbon feedbacks in the Climate system".

我们需要了解海洋的未来，因为更多的热量和碳供应给气候系统。我们知道，海洋吸收了90%以上提供给气候系统的额外热量，通常25%的额外碳排放到气候系统。我们知道，海洋在决定全球平均表面变暖与排放到大气中的碳累积量成比例方面发挥着核心作用。然而，这种变暖对碳排放的线性依赖性存在很大的不确定性。减少这种不确定性是气候科学的一项紧迫任务，以便可靠地估计特定变暖目标（如巴黎协定）的剩余碳预算。我们的工作表明，地表变暖与碳排放之间的模式间不确定性取决于气候反馈的不确定性，包括云，海洋热量吸收和海洋碳吸收。为了加深理解和减少不确定性，我们需要确定区域对气候反馈、海洋热量和碳吸收的贡献，这些是气候系统的全球反应，区域海洋如何吸收供应给气候系统的额外热量和碳，对影响海洋灾害发生的可能性也很重要，如海洋热浪和海洋酸化事件。因此，我们需要知道为什么某些海洋区域比地球仪上的其他区域更快地获得额外的热量或碳。我们需要了解这一区域海洋热量和碳吸收的驱动因素。这些驱动程序的范围从1。提供给海洋的额外热量和碳是由全球海洋上空的稳定环流携带的，这表明额外热量和碳增量的模式在符号上彼此相似;2.海洋通过随时间变化的环流来驱动热量和碳增量的变化，这表明额外热量和碳增量的模式可能彼此具有相反的迹象;3.大气通过海气交换的差异驱动热量和碳的变化，云的反馈作用加强了副热带的暖异常，削弱了南大洋的暖异常。我们需要了解这些海洋热量和碳异常的驱动因素，因为海洋环境的变化会影响海洋灾害的可能性。例如，海洋热浪是温度升高的时期，持续数周至数月，其可能性受到海洋如何吸收供应给气候系统的额外热量的区域模式的影响。温度和碳变化的结合可能会改变海洋的pH值，导致海洋酸化事件。我们需要确定海洋热浪和海洋酸化事件是否可能相互加强。总之，我们将提供一个关于人为热量和碳异常如何控制的新观点，确定其不对称性，海洋和大气驱动因素，以及对全球气候响应和海洋灾害的影响。这项工作与世界气候研究计划的两个重大挑战直接相关，即“云，循环和气候敏感性”和“气候系统中的碳反馈”。

项目成果

期刊论文数量（10）

专著数量（0）

科研奖励数量（0）

会议论文数量（0）

专利数量（0）

Energy budget diagnosis of changing climate feedback.

DOI：
10.1126/sciadv.adf9302
发表时间：
2023-04-21
期刊：
SCIENCE ADVANCES
影响因子：
13.6
作者：
Cael, B. B.;Bloch-Johnson, Jonah;Ceppi, Paulo;Fredriksen, Hege-Beate;Goodwin, Philip;Gregory, Jonathan M.;Smith, Christopher J.;Williams, Richard G.
通讯作者：
Williams, Richard G.

The impacts of cloud-radiative changes on poleward atmospheric and oceanic energy transport in a warmer climate