Geosci. Model Dev., 10, 1945–1960, 2017 www.geosci-model-dev.net/10/1945/2017/ doi:10.5194/gmd-10-1945-2017 © Author(s) 2017. CC Attribution 3.0 License. A non-linear Granger-causality framework to investigate climate–vegetation dynamics Christina Papagiannopoulou1, Diego G. Miralles2,3, Stijn Decubber1, Matthias Demuzere2, Niko E. C. Verhoest2, Wouter A. Dorigo4, and Willem Waegeman1 1Depart. of Mathematical Modelling, Statistics and Bioinformatics, Ghent University, Ghent, Belgium 2Laboratory of Hydrology and Water Management, Ghent University, Ghent, Belgium 3Depart. of Earth Sciences, VU University Amsterdam, Amsterdam, the Netherlands 4Depart. of Geodesy and Geo-Information, Vienna University of Technology, Vienna, Austria Correspondence to: Christina Papagiannopoulou (
[email protected]) Received: 11 October 2016 – Discussion started: 16 November 2016 Revised: 20 March 2017 – Accepted: 29 March 2017 – Published: 17 May 2017 Abstract. Satellite Earth observation has led to the creation in the global climate system. Plant life alters the characteris- of global climate data records of many important environ- tics of the atmosphere through the transfer of water vapour, mental and climatic variables. These come in the form of exchange of carbon dioxide, partition of surface net radia- multivariate time series with different spatial and temporal tion (e.g. albedo), and impacts on wind speed and direction resolutions. Data of this kind provide new means to fur- (Nemani et al., 2003; McPherson et al., 2007; Bonan, 2008; ther unravel the influence of climate on vegetation dynamics. Seddon et al., 2016; Papagiannopoulou et al., 2017). Because However, as advocated in this article, commonly used statis- of the strong two-way relationship between terrestrial vegeta- tical methods are often too simplistic to represent complex tion and climate variability, predictions of future climate can climate–vegetation relationships due to linearity assump- be improved through a better understanding of the vegetation tions.