Influences of Coherent Structures on Validity of the Constant Flux Layer Assumptions in the Unstable Atmospheric Surface Layer

不稳定大气表层相干结构对恒定通量层假设有效性的影响

• 批准号: 2325687
• 负责人: Heping Liu
• 金额: $ 44.08万
• 依托单位: Washington State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2023
• 资助国家: 美国
• 起止时间: 2023-08-01 至 2026-07-31
• 项目状态: 未结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=2325687&HistoricalAwards=false
• 关键词: Influences; Coherent; Structures; Validity; Constant

In many applications such as weather and climate modeling, it is assumed that the transfer rate for scalars (i.e., scalar fluxes), including heat, water vapor, CO2, and other greenhouse gases, is constant with respect to height in the atmospheric surface layer, the lowest layer of the atmosphere. This so-called constant flux layer assumption is also widely used in land-surface flux measurements to quantify scalar fluxes to and from land surfaces. However, the reported failure of this assumption implies that scalar fluxes measured and modeled in the atmospheric surface layer are not equivalent to the fluxes across the surface-atmosphere interface, leading to uncertainty in measured and modeled fluxes in these applications. Despite the abundant studies on the roles of large turbulent eddies (i.e., coherent structures) in contributing to scalar fluxes, it is not well understood as to how large turbulent eddies contribute to changes in fluxes with height in the atmospheric surface layer. The objective of this project is to study what physical mechanisms regulate the attributes of large eddies across height that lead to varying contributions to fluxes with height, contributing to the failure of the constant flux layer assumption across a wide range of atmospheric conditions. By leveraging the existing facilities and as guided by flux budget equations, a field experiment will be conducted over the large water body of Ross Barnett Reservoir in Ridgeland, Mississippi, with a flux tower equipped with five levels of eddy covariance systems and other instruments. The field experiment will provide a unique dataset that minimizes the influence of advective terms and enables more precise examination of the attributes of large turbulent eddies. A combined approach of several analysis methods, such as fast Fourier transform, wavelet transform, and ensemble empirical decomposition mode, will be used to characterize the attributes of large turbulent eddies and their variations with height across instability ranges. Quadrant analysis will be used to quantify asymmetric flux contributions from sweeps and ejections of large turbulent eddies, enabling an analysis of the underlying mechanisms that modulate changes in fluxes with height. Further, such analyses will allow the study of mechanisms that lead to different behaviors of height-varying fluxes for different scalars. The field experiment will generate a unique dataset valuable for studying a wide range of topics in micrometeorology, hydrometeorology, boundary-layer turbulence, lake evaporation, water-atmosphere interactions, carbon emissions from inland waters, water budget for freshwater management, and aquatic ecosystems. An involved Ph.D. student will gain first-hand experience in designing, preparing, and conducting micrometeorological experiments and learn eddy covariance techniques, data analysis theories and tools, and many other research skills. Mini-research projects using the datasets collected in this project will be developed and incorporated into the curriculum of one undergraduate course and two graduate courses being taught by the PI for students’ term projects. Short films and presentations about the field experiment and research findings will be disseminated in scientific conferences and seminars as well as the PI’s department websites for diverse audiences.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.

在诸如天气和气候建模的许多应用中，假设标量的传输速率（即，标量通量），包括热、水蒸气、CO2和其它温室气体，相对于大气表面层（大气的最低层）的高度是恒定的。这种所谓的恒定通量层假设也广泛用于地表通量测量，以量化进出地表的标量通量。然而，报告失败的这一假设意味着，标量通量测量和模拟在大气表面层的通量不等于整个表面-大气界面，导致在这些应用中的测量和模拟通量的不确定性。尽管对大湍流涡旋的作用进行了大量的研究（即，相干结构）对标量通量的贡献，但对于大的湍流涡旋如何对大气表面层中通量随高度的变化做出贡献还没有很好的理解。该项目的目的是研究什么物理机制调节跨高度的大涡旋的属性，导致不同的贡献通量与高度，有助于失败的恒定通量层假设在广泛的大气条件。通过利用现有设施，并根据通量平衡方程，将在密西西比里奇兰的罗斯巴内特水库的大型水体上进行实地试验，试验中将使用一个配有五级涡度相关系统和其他仪器的通量塔。现场实验将提供一个独特的数据集，最大限度地减少平流项的影响，并能够更精确地检查大型湍流涡旋的属性。采用快速傅立叶变换、小波变换和集合经验分解模式等多种分析方法相结合的方法，将用来表征大湍流涡旋的属性及其在不稳定范围内随高度的变化。象限分析将用于量化大湍流涡旋的扫掠和喷射的不对称通量贡献，从而能够分析调节通量随高度变化的基本机制。此外，这样的分析将允许的机制，导致不同的行为的高度变化的通量为不同的标量的研究。实地实验将产生一个独特的数据集，对研究微气象学、水文气象学、边界层湍流、湖泊蒸发、水-大气相互作用、内陆沃茨的碳排放、淡水管理的水预算和水生生态系统等广泛专题很有价值。一个复杂的博士学生将获得设计，准备和进行微气象实验第一手经验，并学习涡度相关技术，数据分析理论和工具，以及许多其他研究技能。使用本项目收集的数据集的小型研究项目将被开发并纳入PI为学生学期项目教授的一门本科课程和两门研究生课程的课程中。关于现场实验和研究结果的短片和演示将在科学会议和研讨会以及PI的部门网站上传播给不同的观众。该奖项反映了NSF的法定使命，并通过使用基金会的知识价值和更广泛的影响审查标准进行评估，被认为值得支持。