Future intensity of precipitation extremes over eastern Canada using very high-resolution modelling

使用超高分辨率模型计算加拿大东部未来极端降水强度

• 批准号: RGPIN-2020-05631
• 负责人: DiLuca, Alejandro
• 金额: $ 2.19万
• 依托单位: Université du Québec à Montréal
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2022
• 资助国家: 加拿大
• 起止时间: 2022-01-01 至 2023-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=765313
• 关键词: Future; intensity; precipitation; extremes; over

Precipitation extremes are among the most damaging and costly weather phenomena to impact eastern Canada. During the cold season, snowfall events can produce massive disruptions in ground and air transportation. In summer and shoulder seasons, rainfall extremes can lead to flooding causing extensive economic and environmental damage. Precipitation extremes are expected to change in the future due to various processes often competing with each other. On the one hand, precipitation extremes are expected to increase due to the increase in atmospheric moisture content in response to the warming of the atmosphere. On the other hand, large-scale circulation changes associated with responses to changes in temperature distributions (i.e., baroclinicity and stability) are expected to lead to less extratropical storms and decreases in precipitation extremes. In addition, there are large uncertainties about the role to be played by some fine-scale processes and feedbacks including the extra latent heat being released and microphysical effects due to changes in hydrometeors. Assessing future changes in extreme precipitation thus requires considering several complex processes at spatial and temporal scales that current climate models, either global or standard regional models, are unable to reproduce due to their coarse resolution and somewhat simplistic parameterization of some processes. The overarching aim of my Discovery research is to determine the causes of future changes in the intensity of extreme precipitation events over eastern Canada. The proposed research program is structured according to two primary questions that combine advanced modelling with state-of-the-art observations: 1. How well do the newly developed convection-permitting models represents observed precipitation extremes? 2. What are the projected changes in the intensity of extreme precipitation and how these changes depend on the amount of moisture (thermodynamics) and the type of precipitation (microphysics)? This research will make use of a very high-resolution climate model that explicitly simulates convective processes (convection permitting) and includes a sophisticated representation of cloud and precipitation microphysical processes. To limit the required computational resources, the model is run over a limited area using the dynamical downscaling technique, and for a limited number of events where heavy precipitation has been previously identified. Simulations of future climate will use a hierarchy of future environments where different changes are introduced in a stepwise manner to help isolate key sources of future changes. That is, for the first time, the evolution of damaging storms will be explored at kilometre-scale resolutions using boundary forcings that emulate present and plausible future conditions. Outcomes will support the development of adaptation strategies to mitigate the future impact of extreme precipitation on runoff, freshwater resources and flooding.

极端降水是影响加拿大东部的最具破坏力和昂贵的天气现象之一。在寒冷的季节，降雪事件可能会在地面和空中运输中造成巨大的干扰。在夏季和肩膀季节，极端降雨会导致洪水造成广泛的经济和环境破坏。由于各种过程经常相互竞争，预计未来的降水极端会发生变化。一方面，由于大气变暖，大气水分含量的增加，预计极端降水会增加。另一方面，与对温度分布变化的反应有关（即斜压力和稳定性）的大规模循环变化预计会导致少量的热带风暴和极端降水的降低。此外，关于一些精细的过程和反馈，包括释放的额外潜热以及由于水学位变化而导致的微物理效应，还有很大的不确定性。因此，评估极端降水的未来变化需要考虑在空间和时间尺度上进行几个复杂的过程，因为当前气候模型（全球或标准区域模型）由于其粗分辨率和某些过程的某种简单的参数化而无法复制。 我发现研究的总体目的是确定加拿大东部极端降水事件强度变化的原因。拟议的研究计划是根据将高级建模与最先进的观察结合的两个主要问题结构结构的：1。新开发的对流渗透模型的良好表明观察到的极端降水？ 2.极端降水强度的预计变化是什么，这些变化如何取决于水分的量（热力学）和降水类型（微物理学）？这项研究将利用非常高分辨率的气候模型，该模型明确模拟对流过程（对流允许），并包括云和降水微物理过程的复杂表示。为了限制所需的计算资源，该模型是使用动态降压技术在有限区域上运行的，并且对于以前已经确定了大量降水量的有限事件。对未来气候的模拟将使用未来环境的层次结构，在这些环境中，以逐步引入不同的变化，以帮助隔离未来变化的关键来源。也就是说，首次使用模拟当前和合理的未来条件的边界强迫，将在公里尺度的决议中探索破坏性风暴的演变。结果将支持制定适应策略，以减轻极端降水对径流，淡水资源和洪水的未来影响。