Ménard Richard, Deshaies-Jacques Martin, Gasset Nicolas
a Modeling and Integration Section, Air Quality Research Division , Environment and Climate Change Canada , Dorval , Quebec , Canada.
J Air Waste Manag Assoc. 2016 Sep;66(9):874-95. doi: 10.1080/10962247.2016.1177620.
An objective analysis is one of the main components of data assimilation. By combining observations with the output of a predictive model we combine the best features of each source of information: the complete spatial and temporal coverage provided by models, with a close representation of the truth provided by observations. The process of combining observations with a model output is called an analysis. To produce an analysis requires the knowledge of observation and model errors, as well as its spatial correlation. This paper is devoted to the development of methods of estimation of these error variances and the characteristic length-scale of the model error correlation for its operational use in the Canadian objective analysis system. We first argue in favor of using compact support correlation functions, and then introduce three estimation methods: the Hollingsworth-Lönnberg (HL) method in local and global form, the maximum likelihood method (ML), and the [Formula: see text] diagnostic method. We perform one-dimensional (1D) simulation studies where the error variance and true correlation length are known, and perform an estimation of both error variances and correlation length where both are non-uniform. We show that a local version of the HL method can capture accurately the error variances and correlation length at each observation site, provided that spatial variability is not too strong. However, the operational objective analysis requires only a single and globally valid correlation length. We examine whether any statistics of the local HL correlation lengths could be a useful estimate, or whether other global estimation methods such as by the global HL, ML, or [Formula: see text] should be used. We found in both 1D simulation and using real data that the ML method is able to capture physically significant aspects of the correlation length, while most other estimates give unphysical and larger length-scale values.
This paper describes a proposed improvement of the objective analysis of surface pollutants at Environment and Climate Change Canada (formerly known as Environment Canada). Objective analyses are essentially surface maps of air pollutants that are obtained by combining observations with an air quality model output, and are thought to provide a complete and more accurate representation of the air quality. The highlight of this study is an analysis of methods to estimate the model (or background) error correlation length-scale. The error statistics are an important and critical component to the analysis scheme.
客观分析是数据同化的主要组成部分之一。通过将观测值与预测模型的输出相结合,我们整合了每个信息源的最佳特征:模型提供的完整时空覆盖范围,以及观测值提供的与真实情况的紧密表征。将观测值与模型输出相结合的过程称为分析。要进行分析,需要了解观测误差和模型误差及其空间相关性。本文致力于开发估计这些误差方差以及模型误差相关性特征长度尺度的方法,以便在加拿大客观分析系统中实际应用。我们首先主张使用具有紧致支集的相关函数,然后介绍三种估计方法:局部和全局形式的霍林斯沃思 - 隆贝格(HL)方法、最大似然方法(ML)以及[公式:见原文]诊断方法。我们进行一维(1D)模拟研究,其中误差方差和真实相关长度是已知的,并在两者均不均匀的情况下对误差方差和相关长度进行估计。我们表明,HL方法的局部版本能够准确捕获每个观测站点的误差方差和相关长度,前提是空间变异性不太强。然而,实际的客观分析仅需要一个全局有效的单一相关长度。我们研究局部HL相关长度的任何统计量是否可以作为有用的估计,或者是否应使用其他全局估计方法,例如全局HL、ML或[公式:见原文]方法。我们在一维模拟和使用实际数据中都发现,ML方法能够捕获相关长度的物理显著方面,而大多数其他估计给出的是不符合物理实际且更大的长度尺度值。
本文描述了加拿大环境与气候变化部(前身为加拿大环境部)对地表污染物客观分析的一项拟议改进。客观分析本质上是通过将观测值与空气质量模型输出相结合而获得的空气污染物表面图,并且被认为能提供空气质量的完整且更准确的表征。本研究的亮点是对估计模型(或背景)误差相关长度尺度的方法进行分析。