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found for the Atlantic basins of North America, the basins of central Europe, and some basins of South America and Africa. On the contrary, poor correlations were found in the Asian basins, mainly those that drain to the Arctic Ocean. Nevertheless, in the latter basins, when monthly correlations were analyzed separately, noticeable seasonal impacts were observed since correlations were much higher in July ( Figure 4c ) than in January ( Figure 4b ). In addition, in these zones it is clearly observed
found for the Atlantic basins of North America, the basins of central Europe, and some basins of South America and Africa. On the contrary, poor correlations were found in the Asian basins, mainly those that drain to the Arctic Ocean. Nevertheless, in the latter basins, when monthly correlations were analyzed separately, noticeable seasonal impacts were observed since correlations were much higher in July ( Figure 4c ) than in January ( Figure 4b ). In addition, in these zones it is clearly observed
