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Atmospheric Forcing of the Iceland Sea

冰岛海的大气强迫

基本信息

批准号：
NE/N009924/1
负责人：
Thomas Bracegirdle
金额：
$ 33.61万
依托单位：
British Antarctic Survey
依托单位国家：
英国
项目类别：
Research Grant
财政年份：
2016
资助国家：
英国
起止时间：
2016 至无数据
项目状态：
已结题

来源：
https://gtr.ukri.org/projects?ref=NE%2FN009924%2F1
关键词：
Atmospheric Forcing Iceland Sea

项目摘要

The subpolar region of the North Atlantic is crucial for the global climate system. It is where coupled atmosphere-ocean processes, on a variety of spatial scales, require an integrated approach for their improved understanding and prediction. This region has enhanced 'communication' between the atmosphere and ocean. Here large surface fluxes of heat and moisture make the surface waters colder, saltier and denser resulting in a convective overturning that contributes to the lower limb of the Atlantic Meridional Overturning Circulation (AMOC). The AMOC is an ocean circulation that carries warm water from the tropics northward with a return flow of cold water southwards at depth; it is instrumental in keeping Europe's climate relatively mild. The Iceland Sea - to the north and east of Iceland - is arguably the least studied of the North Atlantic's subpolar seas. However new discoveries are forcing a redesign of our conceptual model of the North Atlantic's ocean circulation which places the Iceland Sea at the heart of this system and suggests that it requires urgent scientific focus. The recently discovered North Icelandic Jet is thought to be one of two pathways for dense water to pass through the Denmark Strait - the stretch of ocean between Iceland and Greenland - which is the main route for dense waters from the north to enter the Atlantic. Its discovery suggests a new paradigm for where dense water entering the North Atlantic originates. However at present the source of the North Icelandic Jet remains unknown. It is hypothesized that relatively warm Atlantic-origin water is modified into denser water in the Iceland Sea, although it is unclear precisely where, when or how this happens. We will test this hypothesis and investigate this new ocean circulation paradigm. We will examine wintertime atmosphere-ocean processes in the Iceland Sea by characterising its atmospheric forcing, i.e. observing the spatial structure and variability of surface heat, moisture and momentum fluxes in the region and the weather systems that dictate these fluxes. We will make in situ observations of air-sea interaction processes from several platforms (an aircraft; and via project partners an unmanned airborne vehicle, a meteorological buoy and a research vessel) and use these to evaluate meteorological analyses and reanalyses from operational weather forecasting centres. These meteorological analyses and reanalyses are a blend of observations and model output and represent the atmosphere as best we know it. We will carry out numerical modelling experiments to investigate the dynamics of selected weather systems which strongly influence the region, but appear not to be well represented; for example, the boundary layers that develop over transitions between sea ice and the open ocean during cold-air outbreaks; or the jets and wakes that occur downstream of Iceland. We will use our unique observations to improve model representation of these systems.We will also carry out new high-resolution climate simulations. A series of experiments will cover recent past and likely future situations; as well as some idealised situations such as no wintertime sea ice in the Iceland Sea region. We will use a state-of-the-art atmospheric model with high resolution over the Iceland Sea to investigate changes in the atmospheric circulation and surface fluxes. Finally, in collaboration with our international partners, we will analyse new ocean observations and establish which weather systems are important for changing ocean properties in this region. We will use a range of ocean and atmospheric models to establish how current and future ocean circulation pathways function. In short, we will determine the role that atmosphere-ocean processes in the Iceland Sea play in creating the dense waters that flow through Denmark Strait and feed into the lower limb of the AMOC.

北大西洋的副极地区域对全球气候系统至关重要。在这方面，各种空间尺度上的大气-海洋耦合过程需要采取综合办法，以改进对这些过程的理解和预测。这一区域加强了大气和海洋之间的“交流”。在这里，大量的热量和水分的表面通量使表面沃茨更冷、更咸和更密集，导致对流翻转，这有助于大西洋经向翻转环流（AMOC）的下肢。AMOC是一种海洋环流，它将温暖的水从热带地区向北输送，并将冷水向南回流;它有助于保持欧洲的气候相对温和。冰岛海-冰岛的北部和东部-可以说是北大西洋副极地海洋中研究最少的。然而，新的发现正在迫使我们重新设计北大西洋海洋环流的概念模型，该模型将冰岛海置于该系统的中心，并表明它需要紧急的科学关注。最近发现的北冰岛急流被认为是密集水通过丹麦海峡的两条途径之一-丹麦海峡是冰岛和格陵兰岛之间的海洋延伸-这是密集沃茨从北方进入大西洋的主要途径。它的发现为进入北大西洋的稠密水的起源提供了一个新的范例。然而，目前北冰岛喷气机的来源仍然不明。据推测，相对温暖的南极起源的水在冰岛海被改变成密度更大的水，尽管尚不清楚这种情况在何时何地以及如何发生。我们将测试这一假设，并调查这一新的海洋环流模式。我们将研究冬季大气海洋过程中的冰岛海的特点，其大气强迫，即观察的空间结构和变化的表面热量，水分和动量通量在该地区和天气系统，决定这些通量。我们将从几个平台（一架飞机;并通过项目伙伴，一架无人驾驶航空器、一个气象浮标和一艘研究船）对海气相互作用过程进行现场观测，并利用这些观测结果对业务天气预报中心的气象分析和再分析进行评价。这些气象分析和再分析是观测和模式输出的混合，代表我们所知的最佳大气层，我们将进行数值模拟实验，研究对该区域有强烈影响但似乎没有得到充分代表的选定天气系统的动态;例如，在冷空气爆发期间，海冰和开阔海洋之间的过渡区形成的边界层;或冰岛下游的喷射流和尾流。我们将利用我们独特的观测结果来改进这些系统的模型表示。我们还将进行新的高分辨率气候模拟。一系列实验将涵盖最近的过去和可能的未来情况;以及一些理想化的情况，如冰岛海地区没有冬季海冰。我们将使用一个国家的最先进的高分辨率的大气模式在冰岛海调查大气环流和地表通量的变化。最后，我们将与我们的国际合作伙伴合作，分析新的海洋观测结果，并确定哪些天气系统对改变该地区的海洋特性至关重要。我们将使用一系列海洋和大气模型来确定当前和未来海洋环流路径的功能。简而言之，我们将确定冰岛海的大气-海洋过程在形成流经丹麦海峡并流入AMOC下肢的稠密沃茨中所起的作用。