2011
DOI: 10.1016/j.jhydrol.2011.04.034
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River regimes and recent hydrological changes in the Duero basin (Spain)

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Cited by 64 publications
(46 citation statements)
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“…In this research we used principal component analysis (PCA) in S mode to define regions where the temporal variation of the hydrological variables (standardized stramflow index evolution at the 187 gauging stations) had the same pattern (the observation stations were the variables, and the time observations the cases). The PCA technique is widely used by hydrologists to analyze the spatiotemporal variability of hydrological variables (Preisendorfer, 1988;Kalayci and Kahya, 2006; Kahya et al, 2008;Morán-Tejeda et al, 2011;Peterson et al, 2011); it allows for retention of common features of the samples and identification of local peculiarities. Using this approach we obtained an additional non-correlated set of variables that were the linear combinations of the originals.…”
Section: Regionalizationmentioning
confidence: 99%
“…In this research we used principal component analysis (PCA) in S mode to define regions where the temporal variation of the hydrological variables (standardized stramflow index evolution at the 187 gauging stations) had the same pattern (the observation stations were the variables, and the time observations the cases). The PCA technique is widely used by hydrologists to analyze the spatiotemporal variability of hydrological variables (Preisendorfer, 1988;Kalayci and Kahya, 2006; Kahya et al, 2008;Morán-Tejeda et al, 2011;Peterson et al, 2011); it allows for retention of common features of the samples and identification of local peculiarities. Using this approach we obtained an additional non-correlated set of variables that were the linear combinations of the originals.…”
Section: Regionalizationmentioning
confidence: 99%
“…Recent studies have demonstrated a negative trend in the occurrence of snow days in the northwest of the Iberian Peninsula (Pons et al 2009), and a substantial decrease in the duration and depth of the snowpack, which is causing a decrease and shift in spring peak flows (López-Moreno 2005, López-Moreno et al 2008. Snowmelt is a general component of river regimes in the headwaters of the Duero basin (Morán-Tejeda et al 2011b), and the decrease of spring high flows is likely to be related to the reduction in snowpack given the increasing temperatures documented in the region in recent decades. (Esteban-Parra et al 1995, Morales et al 2005.…”
Section: Discussionmentioning
confidence: 99%
“…Precipitation shows a marked seasonality. It peaks roughly in autumn and winter and decreases in spring to its lowest amounts in summer [Moran-Tejeda et al, 2011c]. Precipitation from October to December generates soil water reserves and runoff.…”
Section: The Duero Basinmentioning
confidence: 99%
“…Precipitation from October to December generates soil water reserves and runoff. The dry period coincides with warm temperatures in summer [Moran-Tejeda et al, 2011c]. Summer drought conditions affect 90% of the surface of the Duero river basin [Moratiel et al, 2011].…”
Section: The Duero Basinmentioning
confidence: 99%