Moist processes and their interaction with storm tracks

潮湿过程及其与风暴路径的相互作用

• 批准号: 2890052
• 金额: --
• 依托单位: University of Reading
• 依托单位国家: 英国
• 项目类别: Studentship
• 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=studentship-2890052
• 关键词: Moist; processes; their; interaction; storm

Atmospheric storm tracks are the regions on earth where midlatitude weather systems predominantly grow, evolve and decay. They are strongly associated with the well-known midlatitude jet streams and are responsible for the majority of extreme weather events away from the tropics. Their longer-term prediction and their behaviour in a future climate is one of the great challenges of atmospheric science. A key uncertainty is the role of latent heating (condensation and evaporation of water) in the setting of the intensity of the storm track, its geographical structure, and its evolution.The dynamics of the storm track involves a complex, non-linear interplay between the jet stream, individual storms, different air masses, cloud fields, and the ocean surface. In this project we will work on capturing and understanding those interplays in terms of a dynamical system, a low-order, non-linear description of the most important physical interactions. As an example, earlier work on this topic has demonstrated that the interplay between the jet stream and storm intensity can be described as a non-linear oscillator, similar to a predator -- prey system known from mathematical biology!In this project we will particularly focus on how latent heating in the storm track can be incorporated in such a dynamical systems approach to the storm track. The project involves novel data analysis tools, applied mathematics, and computer simulations of the storm track, and provides a broad avenue of possible research foci and developments.The aim is to improve our understanding of the dynamics of the storm track and be able to make more confident predictions of their future behaviour.

大气风暴轨迹是地球上中纬度天气系统主要生长、演变和衰退的区域。它们与众所周知的中纬度急流密切相关，是远离热带的大多数极端天气事件的原因。它们在未来气候中的长期预测和行为是大气科学的重大挑战之一。一个关键的不确定性是潜热（水的凝结和蒸发）在风暴轴强度、地理结构和演变中的作用。风暴轴的动力学涉及急流、单个风暴、不同气团、云场和海洋表面之间复杂的非线性相互作用。在这个项目中，我们将致力于捕捉和理解这些相互作用的动力系统，最重要的物理相互作用的低阶，非线性描述。作为一个例子，早期的研究表明，急流和风暴强度之间的相互作用可以被描述为一个非线性振荡器，类似于数学生物学中的捕食者-猎物系统！在这个项目中，我们将特别关注如何潜热加热的风暴路径可以纳入这样一个动力系统的方法风暴路径。该项目涉及新的数据分析工具、应用数学和风暴路径的计算机模拟，并提供了一个可能的研究重点和发展的广阔途径，目的是提高我们对风暴路径动力学的理解，并能够对它们的未来行为做出更有信心的预测。