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南大洋碳和热量对气候的影响。

Southern ocean carbon and heat impact on climate.

机构信息

Laboratoire d'Océanographie et du Climat Expérimentations et Approches Numériques (LOCEAN), Sorbonne Université, CNRS/IRD/MNHN, Paris, France.

British Antarctic Survey, Cambridge, UK.

出版信息

Philos Trans A Math Phys Eng Sci. 2023 Jun 26;381(2249):20220056. doi: 10.1098/rsta.2022.0056. Epub 2023 May 8.

Abstract

The Southern Ocean greatly contributes to the regulation of the global climate by controlling important heat and carbon exchanges between the atmosphere and the ocean. Rates of climate change on decadal timescales are therefore impacted by oceanic processes taking place in the Southern Ocean, yet too little is known about these processes. Limitations come both from the lack of observations in this extreme environment and its inherent sensitivity to intermittent processes at scales that are not well captured in current Earth system models. The Southern Ocean Carbon and Heat Impact on Climate programme was launched to address this knowledge gap, with the overall objective to understand and quantify variability of heat and carbon budgets in the Southern Ocean through an investigation of the key physical processes controlling exchanges between the atmosphere, ocean and sea ice using a combination of observational and modelling approaches. Here, we provide a brief overview of the programme, as well as a summary of some of the scientific progress achieved during its first half. Advances range from new evidence of the importance of specific processes in Southern Ocean ventilation rate (e.g. storm-induced turbulence, sea-ice meltwater fronts, wind-induced gyre circulation, dense shelf water formation and abyssal mixing) to refined descriptions of the physical changes currently ongoing in the Southern Ocean and of their link with global climate. This article is part of a discussion meeting issue 'Heat and carbon uptake in the Southern Ocean: the state of the art and future priorities'.

摘要

南大洋通过控制大气和海洋之间的重要热和碳交换,对全球气候调节做出了巨大贡献。因此,气候变化的速度在数十年的时间尺度上受到南大洋海洋过程的影响,但人们对这些过程知之甚少。限制因素既来自于在这个极端环境中缺乏观测,也来自于该大洋对间歇性过程的固有敏感性,而这些间歇性过程在当前的地球系统模型中无法很好地捕捉到。启动“南大洋碳和热对气候的影响计划”就是为了填补这一知识空白,其总体目标是通过调查控制大气、海洋和海冰之间交换的关键物理过程,了解并量化南大洋热和碳收支的变化,为此采用了观测和建模相结合的方法。在这里,我们简要概述了该计划,并总结了其前半段时间内取得的一些科学进展。这些进展的范围从对南大洋通风率的特定过程(例如风暴引起的湍流、海冰融水前缘、风引起的回旋流、密集的陆架水形成和深海混合)的重要性的新证据,到对当前南大洋正在发生的物理变化及其与全球气候的联系的更精细描述。本文是“南大洋热和碳吸收:现状和未来重点”讨论会议的一部分。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7866/10164461/5946a44f325d/rsta20220056f01.jpg

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