UMBRELLA - UM Boundary Layer Representation including land-atmosphere interactions

UMBRELLA - UM 边界层表示，包括陆地-大气相互作用

• 批准号: NE/X018555/1
• 负责人: Andrew Ross
• 金额: $ 97.91万
• 依托单位: University of Leeds
• 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%2FX018555%2F1
• 关键词: UMBRELLA; UM; Boundary; Layer; Representation

The atmospheric boundary layer (BL) is the layer of the atmosphere near the Earth's surface which is directly influenced by the surface. The BL plays a key role in the atmosphere - controlling the exchange of heat, moisture and other atmospheric constituents (both natural and anthropogenic) between the surface and the free troposphere. The boundary layer is also crucial in the initiation of convection and so impacts on the location and timing of convective rainfall. Turbulence is a key characteristic of the BL but is generally too small scale to be resolved in weather and climate models and so needs to be parametrised. With increased computational resources it is now feasible to run operation weather forecasts at km scales where convection can be resolved explicitly (though not necessarily well resolved). As we move towards sub-km scale the models will also begin to resolve large scale boundary structures. This regime where we partly resolve these key processes is known as the grey zone. Modelling the boundary layer in the grey zone requires re-evaluation and modification of the boundary layer parametrisation schemes and their coupling to convection (parametrised or explicit). This project will firstly evaluate the currently available boundary layer schemes and their coupling to convection in the Met Office Unified Model (MetUM) at different resolutions across the grey zone as well as testing any new developments produced as part of this programme. Secondly it will study the coupling between surface heterogeneity, boundary layer structures and convection to understand the key role of heterogeneity. Previous studies largely focus on homogeneous case studies, despite the fact that most land is actually not flat and covers a variety of land use and surface conditions. Including surface heterogeneity will allow a more thorough evaluation of the current boundary layer schemes as well as providing a physical underpinning for more realistic parametrisations which are aware of the underlying variability in the surface characteristics. The project will make use of the latest field observations from the upcoming Wescon field campaign as well as data from long term observational sites in the UK and US. We will also utilise the latest Meteosat third generation satellite observations to evaluate the model in the tropics. We will combine these observations with idealised large eddy simulations and more realistic simulations with the MetUM to study the behaviour of the boundary layer over the diurnal cycle at homogeneous sites and for heterogeneous regions (e.g. regions with variable surface temperature and moisture, or gentle topography).

大气边界层（英语：Atmospheric boundary layer，BL）是地球表面附近的大气层，直接受地球表面的影响。BL在大气中起着关键作用-控制地表和自由对流层之间的热量，水分和其他大气成分（自然和人为）的交换。边界层在对流的形成过程中也起着至关重要的作用，因此对对流降雨的位置和时间也有影响。湍流是BL的一个关键特征，但通常尺度太小，无法在天气和气候模式中解决，因此需要参数化。随着计算资源的增加，现在可以在km尺度上运行天气预报，其中对流可以明确解决（尽管不一定很好地解决）。当我们向亚千米尺度发展时，模型也将开始解析大尺度边界结构。我们部分解决这些关键过程的机制被称为灰色地带。在灰色区域模拟边界层需要重新评估和修改边界层参数化方案及其与对流的耦合（参数化或显式）。该项目将首先评估目前可用的边界层方案及其在灰色区域不同分辨率下与气象局统一模型（MetUM）中对流的耦合，并测试作为该计划一部分产生的任何新发展。其次，将研究地面非均匀性、边界层结构和对流之间的耦合，以了解非均匀性的关键作用。以前的研究主要集中在同质的案例研究，尽管事实上，大多数土地实际上是不平坦的，涵盖了各种土地利用和表面条件。包括表面的异质性将允许更彻底的评价目前的边界层方案，以及提供一个物理基础，更现实的参数化，这是知道在表面特性的潜在变化。该项目将利用来自即将到来的Wescon现场活动的最新现场观测以及来自英国和美国长期观测站点的数据。我们还将利用最新的气象卫星第三代卫星观测来评估热带地区的模型。我们将结合联合收割机这些观测结果与理想化的大涡模拟和更现实的模拟与MetUM研究的行为边界层的昼夜循环在均匀的网站和异质区域（例如，可变的表面温度和湿度的区域，或平缓的地形）。