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EAGER: Generalizing Monin-Obukhov Similarity Theory (MOST)-based Surface Layer Parameterizations for Turbulence Resolving Earth System Models (ESMs)

EAGER: Generalizing Monin-Obukhov Similarity Theory (MOST)-based Surface Layer Parameterizations for Turbulence Resolving Earth System Models (ESMs)
EAGER:将基于 Monin-Obukhov 相似理论 (MOST) 的表面层参数化推广到湍流解析地球系统模型 (ESM)
批准号:
2414424
负责人:
Marc Calaf
金额:
$23.64万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2024
资助国家:
美国
项目状态:
未结题
起止时间:
2024-02-15 至 2026-01-31

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中文摘要
翻译
今天,天气预报是我们日常生活中不可或缺的一部分,也是世界经济和安全的支柱,例如,通过及时预报能源生产、农业规划和应对严重风暴等。由于几个重要因素,如更强大的计算机的可用性,以及在运行期间不断获取实验数据,模型输出的准确性随着时间的推移而逐渐提高。尽管如此,在表示某些特有的物理过程方面仍然存在重大缺陷。其中之一是陆地-大气相互作用的表示,它捕捉到了空气与地球表面交换热量、水分和阻力的方式。传统上,这些过程是使用最初为规范流动和表面条件开发的公式来表示的,并且已知在现实的表面配置(例如,山区地形、森林上空、非均匀表面等)下表现不佳。尽管如此,由于缺乏更好的替代方案,它仍然是所有数值天气预报和气候模型的主力。在这一研究项目中,将开发一种新的方法,以促进现有的陆地-大气相互作用公式的扩展,使其适用于所有现实的流动和地面配置。这项工作的结果将代表近地表过程在数值天气预报和气候模式中表示方式的范例变化,导致天气和气候预测精度的下一次飞跃。这项研究有可能影响每个人,从美国农村的当地农民,到计划下一个海上风电场的投资者,以及刚刚查看天气预报为即将到来的周末做计划的普通家庭。具体地说,这个项目将利用广义Monin-Obukhov相似性理论(MOST),该理论包括湍流各向异性的度量作为额外的无量纲项。作为第一步,将在湍流分辨地球系统模型中实施拉格朗日平均方案,以便可以实时计算湍流各向异性,目标是瞬时修正大多数标度关系。作为第二步,将通过对不同现实复杂流动形态进行不同的大涡模拟,并将结果与现有的实验数据进行比较,来测试该新框架的稳健性。此外,还将测试这一新框架对空间分辨率的依赖性。这里的目标是了解空间分辨率如何影响湍流各向异性的计算,以及它在校正地表附近的动量、质量和能量交换方面的相应效果。这个项目是非常必要的第一步,在基于各向异性的广义Monin-Obukhov相似理论(MOST)可以在非分辨率湍流地球系统模型中实施之前。这个奖项反映了NSF的法定使命,并通过使用基金会的智力优势和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
Today, weather forecasts are an integral part of our daily lives and a pillar of the world’s economy and safety through, for example, timely forecasts for energy production, agricultural planning, and severe storm readiness, to name a few. The accuracy of the model outputs has progressively increased with time as a result of several important factors, such as the availability of more powerful computers, and the continuous ingestion of experimental data during runtime. Nonetheless, there remain significant weaknesses in the representation of some of the characteristic physical processes. One of these is the representation of land-atmosphere interactions, which capture the way the air exchanges heat, moisture, and drag with the Earth’s surface. Traditionally, these processes have been represented using a formulation that was originally developed for canonical flow and surface conditions, and which is known to not perform well under realistic surface configurations (e.g. mountainous terrain, over forests, heterogeneous surfaces, etc.). Nonetheless it remains the workhorse in all numerical weather prediction and climate models given the lack of better alternatives. In this research project a new approach will be developed that facilitate the extension of the existing land-atmosphere interaction formulation to be applicable to all realistic flow and surface configurations. Results from this work will represent a paradigm change in the way near surface processes are represented in numerical weather prediction and climate models, leading to the next leap forward in weather and climate prediction accuracy. This research has the potential to impact everyone, from the local farmer in rural U.S.A, to investors planning for the next offshore wind farm, as well as the regular family that is just checking the weather forecast to plan for the upcoming weekend.Specifically, this project will leverage the generalized Monin-Obukhov Similarity Theory (MOST) that includes the metric of turbulence anisotropy as an additional non-dimensional term. As the first step, a Lagrangian averaging scheme will be implemented in a turbulence resolving Earth System Model such that it is possible to compute turbulence anisotropy on the fly, with the goal of instantaneously correcting MOST scaling relations. As the second step, the robustness of this new framework will be tested by running different Large-Eddy Simulations of different realistic complex flow configurations and comparing the results with existing experimental datasets. In addition, this new framework will also be tested with respect to its dependence with spatial resolution. The goal here is to understand how spatial resolution affects the computation of turbulence anisotropy and its corresponding effect in correcting the momentum, mass, and energy exchanges near the surface. This project represents a very much needed first step, before the anisotropy-based generalized Monin-Obukhov Similarity Theory (MOST) can be implemented in non-resolving turbulence Earth System Models.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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Collaborative Research: Transport and mixing processes in turbulent boundary layers over ground-elevated surface roughness
  • 批准号:
    2235750
  • 项目类别:
    Standard Grant
  • 资助金额:
    $26.84万
  • 财政年份:
    2023
  • 负责人:
    Marc Calaf
  • 依托单位:
Collaborative Research: GCR: Developing Integrated Agroecological Renewable Energy Systems through Convergent Research
  • 批准号:
    2317985
  • 项目类别:
    Continuing Grant
  • 资助金额:
    $63.76万
  • 财政年份:
    2023
  • 负责人:
    Marc Calaf
  • 依托单位:
Collaborative Research: Unfolding the Link between Forest Canopy Structure and Flow Morphology: A Physics-based Representation for Numerical Weather Prediction Simulations
  • 批准号:
    1712538
  • 项目类别:
    Standard Grant
  • 资助金额:
    $22.85万
  • 财政年份:
    2017
  • 负责人:
    Marc Calaf
  • 依托单位:
海外基金