DIMSUM: Drivers and impacts of North Atlantic heat and freshwater fluxes unsettling modern-day climate

DIMSUM：北大西洋热量和淡水通量扰乱现代气候的驱动因素和影响

• 批准号: NE/Y005082/1
• 负责人: Yueng-Djern Lenn
• 金额: $ 37.02万
• 依托单位: Bangor University
• 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: https://gtr.ukri.org/projects?ref=NE%2FY005082%2F1
• 关键词: DIMSUM; Drivers; impacts; North; Atlantic

Among the most fatal, societal risks of the changing climate is the crossing of climate tipping points, leading to an abrupt and potentially irreversible climate change. Observations from paleoclimate records, established theory, and models suggest that changes in North Atlantic ocean circulation, driven by freshwater discharges from melting glaciers and sea ice, may trigger this risk. Already, recent research has shown that excess freshwater in the North Atlantic is linked to stormier weather in the high northern latitudes in winter and drier, warmer European summers. The ice melt and the associated freshwater fluxes are, in turn, highly sensitive to the distribution of heat by the ocean and atmospheric circulations of the Arctic and North Atlantic. Thus, predicting changes in the distribution of heat and freshwater in the Arctic and the North Atlantic requires a detailed understanding of the feedbacks between the ice, the ocean, and the atmosphere. Unfortunately, many current climate models do not adequately capture these feedbacks and may hence, potentially, underestimate the risk of rapid climate change. Considering the rate at which the Arctic is currently warming and losing ice, there is an urgent need to assess the resulting ocean changes in the North Atlantic and their large-scale climatic consequences. DIMSUM approaches the gap in our knowledge around ice-ocean-atmosphere feedbacks in the Arctic and North Atlantic region with a unique combination of observations, new model products, and tools. Taking advantage of the long-term field observations from the OSNAP and RAPID mooring arrays across the North Atlantic, high resolution simulations produced within the NC CANARI project and the state-of-the-art Arctic Subpolar gyre sTate Estimate (ASTE), we will first characterise heat and freshwater changes in the Arctic and North Atlantic regions. We will further use the special adjoint capability of the ASTE model to carry out sensitivity and attributions studies. These studies will help us assess mechanisms that drive changes in the heat and freshwater distribution. In addition, we will evaluate climate feedbacks and impacts by applying statistical techniques to ASTE, remote sensing observations, atmospheric reanalysis data, and the new, large ensemble, high resolution CANARI simulations. By finally integrating the results into a new, conceptual model analysis, we will provide improved threshold estimates for climate tipping points in the North Atlantic sector.

气候变化的最致命的社会风险是气候转化点的穿越，导致突然且可能不可逆的气候变化。从古气候记录，既定理论和模型中的观察结果表明，北大西洋循环的变化是由熔融冰川和海冰的淡水排放驱动的，可能会触发这种风险。最近的研究已经表明，北大西洋的多余淡水与冬季高北纬度地区的暴风雨和更干燥，更温暖的欧洲夏天有关。反过来，冰融化和相关的淡水通量对北极和北大西洋的海洋和大气循环的热量非常敏感。因此，预测北极和北大西洋中热量和淡水的分布变化需要详细了解冰，海洋和大气之间的反馈。不幸的是，许多当前的气候模型没有充分捕获这些反馈，因此可能会低估气候变化的风险。考虑到北极目前正在变暖和失去冰的速度，迫切需要评估北大西洋的海洋变化及其大规模的气候后果。 Dimsum围绕着北极和北大西洋地区的冰山 - 大气反馈的知识差距，并具有独特的观测，新模型产品和工具的独特组合。利用OSNAP的长期现场观察和北大西洋上的快速系泊阵列，NC Canari项目中产生的高分辨率模拟以及最先进的北极亚极圆形Gyre州估算（ASTE），我们将首先是北极和北大西洋地区的热量和淡水变化。我们将进一步使用ASTE模型的特殊伴随能力来进行灵敏度和归因研究。这些研究将帮助我们评估驱动热量和淡水分布变化的机制。此外，我们将通过将统计技术应用于ASTE，遥感观测，大气重新分析数据以及新的大型集合，高分辨率Canari模拟来评估气候反馈和影响。通过最终将结果整合到一个新的概念模型分析中，我们将为北大西洋部门的气候转化点提供改进的阈值估计。