| http://www.w3.org/ns/prov#value | - Several reasons may have led to this conclusion, including the use of an overaggregated index of ENSO (i.e., mean from October to May of the Southern Oscillation Index [SOI]) that is not the most relevant for North American precipitation anomalies (SST averaged over the so-called NINO3.4 region [5S???5?? N; 170???120?? W] is more relevant for well-documented reasons).42 Additionally, the North Pac
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