气候模式中经验正交函数 (EOF) 模式的不确定性与采样大小之间的关系

IF 4.8 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Journal of Climate Pub Date : 2024-03-11 DOI:10.1175/jcli-d-23-0165.1
Tong Shen, Riyu Lu
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引用次数: 0

摘要

摘要 本研究利用耦合模式相互比较项目(CMIP6)第 6 阶段工业化前控制(piControl)实验的模拟结果,以北大西洋涛动(NAO)和厄尔尼诺-南方涛动(ENSO)为例,研究了气候模式中经验正交函数(EOF)模式的不确定性与采样规模之间的关系。结果表明,这种关系可以用一个简明的拟合函数[即 y = a/(x - b)]来量化。这里,y 是一致系数的 5%-95%置信区间,x 是取样规模,a 和 b 是取决于模型或观测数据的两个参数。在拟合函数中,b 对取样规模起调节作用,而参数 a 则对取样规模起缩放作用,因此起着更重要的作用。进一步分析表明,参数 a 或 EOF1 模式的不确定性随着 EOF1 和 EOF2 模式方差分数之差的增加而急剧下降,近似于幂函数形式。确保 EOF 模式可靠的最小取样规模也可通过拟合函数估算出来,并显示出 NAO 和 ENSO 模式之间的巨大差异。这种多样性表明,在对气候变异模式进行模式评估和预测模式的未来变化之前,估计最小采样规模非常重要,特别是当 EOF2 模式解释的方差接近 EOF1 模式时。意义声明 经验正交函数(EOF)分析、主成分分析或特征向量分析已广泛应用于各个研究领域。然而,通过 EOF 方法获得可靠的模式需要多大的取样规模,这仍然是一个未决问题。在本研究中,我们利用足够长的模拟数据,研究了当前气候模式中 EOF 结果的不确定性与采样规模之间的关系,发现这种关系可以用拟合函数 y = a/(x - b) 来描述。这里,y 代表不确定性,x 是采样规模,a 和 b 是参数。参数 a 与第一和第二 EOF 模式的方差分数之差密切相关,在拟合函数中起着更重要的作用。拟合函数还可以估算出获得可靠 EOF 模式所需的最小采样大小,不同模型的最小采样大小差异很大。这些结果为判断 EOF 模式的可靠性提供了依据,特别是当第一和第二 EOF 模式能解释相似的方差分数时。
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Relationship between the Uncertainty of Empirical Orthogonal Function (EOF) Modes and Sampling Sizes in Climate Models
Abstract This study investigates the relationship between the uncertainty of empirical orthogonal function (EOF) modes and sampling size in climate models, using simulated results of preindustrial control (piControl) experiments in phase 6 of the Coupled Model Intercomparison Project (CMIP6), and taking the North Atlantic Oscillation (NAO) and El Niño–Southern Oscillation (ENSO) as examples. The results indicate that this relationship can be quantified by a concise fitting function [i.e., y = a/(x − b)]. Here, y is the 5%–95% confidence interval of congruence coefficient, x is the sampling size, and a and b are two parameters depending on models or observations. As compared with b, which modulates the sampling size in the fitting function, the parameter a scales the sampling size and thus plays a much more important role. Further analysis indicates that the parameter a, or the uncertainty of EOF1 mode, decreases dramatically with the increase of the difference between variance fractions of EOF1 and EOF2 modes, approximately in the form of a power function. The minimum sampling size to ensure a reliable EOF mode can also be estimated by the fitting function and shows a great diversity among models both for the NAO and ENSO. The diversity suggests the importance of estimating the minimum sampling size before model evaluations on climate variability modes and projections on the future change in modes, particularly when the EOF2 mode explains the variance close to EOF1 mode. Significance Statement Empirical orthogonal function (EOF) analysis, principal component analysis, or eigenvector analysis has been widely used in various research fields. However, it remains as an open question as to how large the sampling size is required to be to obtain reliable modes through the EOF method. In this study, we investigate the relationship between the uncertainty of EOF results and sampling size in current climate models, using adequately long simulated data, and we find that this relationship can be depicted by the fitting function y = a/(x − b). Here, y represents the uncertainty, x is the sampling size, and a and b are parameters. The parameter a is closely related to the difference between variance fractions of first and second EOF modes and plays a more important role in the fitting function. The minimum sampling sizes that are required to obtain reliable EOF modes can also be estimated by the fitting function and vary greatly from model to model. The results provide a basis for judging the reliability of EOF modes, particularly when the first and second EOF modes explain similar variance fractions.
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来源期刊
Journal of Climate
Journal of Climate 地学-气象与大气科学
CiteScore
9.30
自引率
14.30%
发文量
490
审稿时长
7.5 months
期刊介绍: The Journal of Climate (JCLI) (ISSN: 0894-8755; eISSN: 1520-0442) publishes research that advances basic understanding of the dynamics and physics of the climate system on large spatial scales, including variability of the atmosphere, oceans, land surface, and cryosphere; past, present, and projected future changes in the climate system; and climate simulation and prediction.
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