Platzer Paul, Chapron Bertrand, Messori Gabriele
Laboratoire d'Océanographie Physique et Spatiale, Univ. Brest/Ifremer/CNRS/IRD, Plouzané, F-29280 France.
Odyssey, Inria/IMT/CNRS, Plouzané, F-29280 France.
NPJ Clim Atmos Sci. 2025;8(1):203. doi: 10.1038/s41612-025-01086-w. Epub 2025 May 28.
Large-scale atmospheric variability can be summarized by recurring patterns called weather regimes. Their properties, including predictability, have been studied using the local dimension, a geometrical estimate of degrees of freedom from multifractal theory. Local dimension estimates vary across regimes, decrease when a single regime dominates, and increase during transitions, supporting their dynamical significance. However, these variations stem not only from geometry but also from sampling density. We develop a null-hypothesis test using stochastic twins-Gaussian mixture-based surrogates matching atmospheric sampling density but with constant geometry-applied to ERA5 500 hPa fields. Density effects alone explain over 25% of local dimension variance and reproduce the dimension drop near regime peaks, indicating this behavior is density-driven, not geometric. The remaining variability is plausibly geometry-driven. This approach, applicable to any observed system with known sampling distribution, offers a new framework for interpreting local dimension estimates in atmospheric and oceanic data.
大规模大气变率可以通过称为天气型的反复出现的模式来概括。其属性,包括可预测性,已使用局部维数进行研究,局部维数是多重分形理论中自由度的几何估计。局部维数估计在不同天气型之间变化,当单一天气型占主导时减小,在转变期间增加,这支持了它们的动力学意义。然而,这些变化不仅源于几何结构,还源于采样密度。我们使用随机孪生——基于高斯混合的替代物开发了一种零假设检验,该替代物匹配大气采样密度但具有恒定的几何结构,并应用于ERA5 500百帕场。仅密度效应就解释了超过25%的局部维数方差,并重现了天气型峰值附近的维数下降,表明这种行为是由密度驱动的,而非几何结构驱动的。其余的变率可能是由几何结构驱动的。这种方法适用于任何具有已知采样分布的观测系统,为解释大气和海洋数据中的局部维数估计提供了一个新框架。