“…In an effort to explore the relations between the water dynamics and ecosystem processes, several studies (Anyamba, Tucker, & Mahoney, 2002;Armanios & Fisher, 2014;Chen, De Jeu, Liu, Van der Werf, & Dolman, 2014;Davenport & Nicholson, 1993;Deshmukh, 1984;Eklundh, 1998;Nicholson, Davenport, & Malo, 1990;Richard & Poccard, 1998;Shinoda, 1995) have investigated the response of vegetation to P/SM patterns, by examining the spatiotemporal patterns and inter-relations of P/SM and the Normalized Difference Vegetation Index (NDVI) in EA and other sensitive regions of the globe. While spectral vegetation indices, such as NDVI, have been extensively used to analyze spatiotemporal variations in vegetation distribution, their use to quantify vegetation status or behavior is plagued by several shortcomings, such as its high sensitivity to atmospheric influences (cloud, aerosols), constraints due to seasonal decreases in solar illumination, its limitation in monitoring only the top of the canopy (Liu, de Jeu, McCabe, Evans, & van Dijk, 2011), its proneness to saturation in dense canopies (Liu, van Dijk, McCabe, Evans, & Jeu, 2012), and its weak and indirect link with water content (Pettorelli, 2013).…”