Southern Ocean carbon indices and metrics (SARDINE)

南大洋提供了一个主要窗口，大气通过这个窗口影响内陆海洋的性质，进而影响深海对大气的影响。在这里形成的地表水在全球海洋上深度转移，深水返回海面。全球海洋在碳循环中的作用受到这种双重活动的强烈控制：离开南大洋的表层水吸收大气中的二氧化碳，而深水富含二氧化碳，因此当深水返回海面时，二氧化碳被排放到大气中。南大洋模式水域的体积持续变化，预计将随着不同的排放方案以非线性方式变化，以及与南极洲上空大气变化相关的颠覆环流的变化。尚不清楚的是南大洋海洋碳吸收的相关变化，以及对全球碳和气候指标的更广泛影响。例如，如果南大洋的层结加强而通风减弱，那么对碳和气候系统会产生什么影响？我们需要知道南大洋是如何隔离热量和碳的，以及这种吸收可能会如何随着气候变化而改变。通过利用通风和主要物理程序(管弦乐队)的诊断方法，我们将确定不同水团中有多少碳被吸收，并确定不同物理、生物和化学过程对应的碳库的变化。我们需要知道南大洋如何改变气候系统中的全球碳反馈。通过在地球系统模型中确定二氧化碳年上升1%的海洋碳储量的变化，我们将揭示南大洋对全球碳循环反馈的影响，以及它们的组成部分如何随着物理、化学和生物过程的变化而变化。同样，我们需要知道南大洋如何影响全球气候指标，包括给定累计碳排放预计地表增温多少，为避免超过增温目标可能排放多少碳，以及在排放停止后延迟峰值增温的程度。通过典型浓度路径下的地球系统模式的综合热诊断和碳诊断，我们将确定南大洋对全球表面变暖对碳排放的响应的影响，避免变暖目标所允许的最大碳排放量，以及排放停止后全球表面变暖的程度。这项工作对于我们理解南大洋环流和通风变化如何影响全球变暖的全球碳和气候指标是至关重要的。南大洋主导着全球海洋热量和碳吸收，但在全球气候模型中的表现很差。目前的地球系统模型在对最近过去的海洋物理和生物地球化学表示方面存在广泛的差异，在气候强迫下对未来的预测方面，模型之间往往存在巨大差异。这项研究将使我们能够首次确定南大洋的物理、生物和化学过程对各种关键的全球气候指标的贡献。通过综合这些气候指标以及正在进行的项目管弦乐队和玫瑰揭示的对南大洋物理和生物地球化学性质的新理解，我们将能够对预测的气候未来的扩散做出新的解释，并确定南大洋对不确定性的影响。

The Southern Ocean provides the primary window by which the atmosphere affects the properties of the interior ocean and, in turn, how the deep ocean affects the atmosphere. Surface waters formed here are transferred at depth over the global ocean and deep waters are returned to the sea surface. The role of the global ocean in the carbon cycle is strongly controlled by this dual activity: surface waters leaving the Southern Ocean act to drawdown atmospheric carbon dioxide, while deep waters are carbon rich and so when deep waters return to the sea surface carbon dioxide is outgassed to the atmosphere.There are ongoing changes in the volume of Southern Ocean mode waters, which are projected to vary in a nonlinear manner with different emission scenarios, together with changes in the overturning circulation associated with atmospheric changes over Antarctica. What is unclear are the associated changes in ocean carbon uptake in the Southern Ocean together with the wider effects on global carbon and climate metrics. For example, if the stratification strengthens and ventilation weakens in the Southern Ocean, what then are the resulting effects for the carbon and climate system?We need to know how the Southern Ocean is sequestering heat and carbon, and how that uptake is likely to alter with climate change. By drawing upon ventilation and overturning diagnostics from a mainly physical programme (ORCHESTRA), we will identify how much carbon is taken up in different water masses and identify the changes in carbon pools corresponding to different physical, biological and chemical processes.We need to know how the Southern Ocean alters global carbon feedbacks in the climate system. By identifying the changes in ocean carbon inventories in Earth system model projections for 1% annual rise in CO2, we will reveal the effect of the Southern Ocean on global carbon-cycle feedbacks, as well as identify how their components alter with changes in physical, chemical and biological processes.Similarly, we need to know how the Southern Ocean affects global climate metrics, including how much surface warming is expected for a given cumulative carbon emission, how much carbon may be emitted to avoid exceeding warming targets and the extent of delayed peak warming after emissions cease. Through combined heat and carbon diagnostics of Earth system models following Representative Concentration Pathways, we will identify the effect of the Southern Ocean on the global surface warming response to carbon emissions, the maximum permitted carbon emission to avoid warming targets and how much global surface warming might occur after emissions cease.This work is crucial if we are to understand how Southern Ocean circulation and ventilation changes affect global carbon and climate metrics in a warming world. The Southern Ocean dominates global ocean heat and carbon uptake, but is poorly represented in global climate models. There is a wide spread across current Earth system models in their ocean physical and biogeochemical representation of the recent past, and often dramatic differences between models in their projections for the future under climate forcing. This study will allow us to attribute for the first time the contribution of the physical, biological and chemical processes in the Southern Ocean to various critical global climate metrics. Through a synthesis of these climate metrics with new understanding of the physical and biogeochemical properties of the Southern Ocean revealed by ongoing projects ORCHESTRA and RoSES, we will be able to produce new interpretations of the spread in projected climate futures and identify the effect of the Southern Ocean on the uncertainty.