Wavelet correlations to reveal multiscale coupling in geophysical systems

TL;DR

This paper demonstrates that wavelet cross-correlation is an effective statistical method for identifying and analyzing multiscale interactions and feedbacks in geophysical systems, especially between soil moisture and temperature.

Contribution

It introduces and validates the wavelet cross-correlation method for revealing multiscale coupling in climate data, highlighting its ability to resolve dynamics across different temporal scales.

Findings

Successfully captures soil moisture-temperature coupling across days to months

Identifies the magnitude and directionality of multiscale interactions

Applicable to various climatic regimes from wet to dry

Abstract

The interactions between climate and the environment are highly complex. Due to this complexity, process-based models are often preferred to estimate the net magnitude and directionality of interactions in the Earth System. However, these models are based on simplifications of our understanding of nature, thus are unavoidably imperfect. Conversely, observation-based data of climatic and environmental variables are becoming increasingly accessible over large scales due to the progress of space-borne sensing technologies and data-assimilation techniques. Albeit uncertain, these data enable the possibility to start unraveling complex multivariable, multiscale relationships if the appropriate statistical methods are applied. Here, we investigate the potential of the wavelet cross-correlation method as a tool for identifying multiscale interactions, feedback and regime shifts in geophysical systems. The ability of wavelet cross-correlation to resolve the fast and slow components of coupled systems is tested on synthetic data of known directionality, and then applied to observations to study one of the most critical interactions between land and atmosphere: the coupling between soil moisture and near-ground air temperature. Results show that our method is not only able to capture the dynamics of the soil moisture-temperature coupling over a wide range of temporal scales (from days to several months) and climatic regimes (from wet to dry), but also to consistently identify the magnitude and directionality of the coupling. Consequently, wavelet cross-correlations are presented as a promising tool for the study of multiscale interactions, with the potential of being extended to the analysis of causal relationships in the Earth system.