The UK Earth system modelling project.

英国地球系统建模项目。

基本信息

批准号：
NE/N01801X/1
负责人：
Paul Holland
金额：
$ 128.56万
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%2FN01801X%2F1
关键词：
UK Earth system modelling project.

项目摘要

Global climate change is one of the leading environmental threats facing mankind. To develop appropriate mitigation and adaptation strategies requires accurate projections of the future state of the Earth's climate. To address this, the research community have developed Global Climate Models (GCMs) that describe the main physical processes in the coupled climate system. These mathematical-computer models are integrated forwards in simulated time, from a pre-industrial period(before ~1850) to present-day, forced by observed estimates of key greenhouse gases (e.g. carbon dioxide, methane, ozone), aerosols and land-use. The models are then continued into the simulated future forced by a range of greenhouse gas, aerosol and land-use scenarios representing plausible future socio-economic development pathways. Each of the time-evolving model future climates are then compared to the pre-industrial and present-day climates from the same model. This analysis results in an ensemble of climate change estimates, linked to each of the applied development pathways, that can be used to assess potential socio-economic and ecological impacts and aid in the development of climate change mitigation and adaptation policies.GCMs have recently been further developed into Earth system models (ESMs). A key difference between ESMs and GCMs is the former include an interactive description of the global carbon cycle. Climate change is primarily driven by human emissions of carbon dioxide which traps a fraction of the Earth's emitted radiation in the atmosphere, warming it and the Earth's surface. This direct warming from increasing carbon dioxide can be amplified or damped by various feedbacks in the climate system (e.g. involving water vapour, clouds or sea-ice). A key determinant of the climate change impact of human-emitted carbon dioxide is how much of the emitted gas actually stays in the atmosphere where it can interact with the Earth's emitted radiation. Presently, around 50% of the carbon dioxide emitted by humans stays in the atmosphere, the remaining 50% being taken up, in roughly equal measures, by the terrestrial biosphere and the world oceans. There is increasing evidence to suggest the efficiency of these natural carbon reservoirs in absorbing human-emitted carbon dioxide may change in the future, being sensitive to both the concentration of carbon dioxide in the Earth system and to the induced climate change. A reduction in the uptake efficiency of Earth's natural carbon reservoirs would result in a larger fraction of emitted carbon dioxide remaining in the atmosphere and thereby a larger climate change (warming) for a given cumulative emission of carbon dioxide.To address the need to simulate both the changing global climate and the carbon cycle response to a changing climate and changing atmospheric composition, we are developing the 1st UK Earth system model, based on the core physical GCM, HadGEM3, developed at the Met Office. This development is a major collaboration between NERC centres and the Met Office, integrating a large body of core research and development into a single, world-leading ESM. This proposal aims to secure the NERC funding to maintain this collaboration. The project will support the final development and community release of the 1st UKESM models, as well as application of these models to a range of collaborative science experiments carried out at the international level to support the IPCC AR6. The project has a major emphasis on evaluating the full range of climate and biogeochemical processes and interactions simulated by UKESM1 models with an aim to increase confidence in future projections made with the models. The project will also generate and analyse a suite of such projections and deliver a set of robust estimates of Earth system change to UK government, business and the public.Finally, the project will initiate long-term development of a 2nd version of the UKESM model, for release ~2023.

全球气候变化是人类面临的主要环境威胁之一。为了制定适当的缓解和适应战略，需要准确预测地球气候的未来状况。为了解决这个问题，研究界开发了全球气候模型（GCM）来描述耦合气候系统中的主要物理过程。这些数学计算机模型在模拟时间中向前整合，从工业化前时期（约 1850 年之前）到现在，受到对关键温室气体（例如二氧化碳、甲烷、臭氧）、气溶胶和陆地排放的观测估计的推动。使用。然后，这些模型将继续进入由一系列温室气体、气溶胶和土地利用情景所驱动的模拟未来，这些情景代表了未来可能的社会经济发展路径。然后将每个时间演变模型的未来气候与同一模型的工业化前和当今气候进行比较。该分析产生了气候变化估计的整体，与每个应用的发展路径相关联，可用于评估潜在的社会经济和生态影响，并帮助制定气候变化减缓和适应政策。GCM 最近已被进一步发展为地球系统模型（ESM）。 ESM 和 GCM 之间的主要区别在于前者包括对全球碳循环的交互式描述。气候变化主要是由人类排放的二氧化碳造成的，二氧化碳将地球排放的一小部分辐射捕获在大气中，导致大气层和地球表面变暖。二氧化碳增加导致的直接变暖可以通过气候系统中的各种反馈（例如涉及水蒸气、云或海冰）来放大或减弱。人类排放的二氧化碳对气候变化影响的一个关键决定因素是，有多少排放的气体实际上留在大气中，在那里它可以与地球排放的辐射相互作用。目前，人类排放的二氧化碳大约有 50% 留在大气中，其余 50% 被陆地生物圈和世界海洋吸收，大致相同。越来越多的证据表明，这些天然碳库吸收人类排放的二氧化碳的效率未来可能会发生变化，对地球系统中二氧化碳的浓度和引起的气候变化都很敏感。地球天然碳库吸收效率的降低将导致更大比例的排放二氧化碳残留在大气中，从而在给定的二氧化碳累积排放量下导致更大的气候变化（变暖）。为了应对不断变化的全球气候以及碳循环对气候变化和大气成分变化的响应，我们正在开发第一个英国地球系统模型，该模型基于英国气象局开发的核心物理 GCM HadGEM3。这项开发是 NERC 中心和英国气象局之间的重大合作，将大量的核心研发整合到一个世界领先的 ESM 中。该提案旨在确保 NERC 提供资金来维持这种合作。该项目将支持第一个 UKESM 模型的最终开发和社区发布，以及将这些模型应用于在国际层面开展的一系列协作科学实验，以支持 IPCC AR6。该项目的重点是评估 UKESM1 模型模拟的全方位气候和生物地球化学过程和相互作用，旨在增强对模型未来预测的信心。该项目还将生成和分析一套此类预测，并向英国政府、企业和公众提供一套对地球系统变化的可靠估计。最后，该项目将启动 UKESM 模型第二版的长期开发，预计于 2023 年发布。