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Classification of mechanisms, climatic context, areal scaling, and synchronization of floods: the hydroclimatology of floods in the Upper Paraná River basin, Brazil

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Figure

Figure 1. The Paraná River basin (red contour) and streamflowgauges used in this work (black dots)
Figure 2. (a) Number of hits in each neuron (blue hexagons).(b) Connecting neighboring neurons (red lines)
Figure 3. Neuron weights obtained for the SOM. These weights basically represent the rainfall anomalies (in millimeters) over the UpperParaná River basin from day t − 5 (top panels) to day t (bottom panels)
Figure 4. Vertically integrated moisture fluxes (kg (m s)−1, shown by the arrows) and associated divergence field (10−4 kg (m2 s)−1) aver-aged over each neuron class
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