diffenrences and simailarties between monsoon and mediterranean
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Precipitation and SOI Values. When annual precipitation values were split into the three main different rainfall signals in the Mexican Pacific (winter-spring, summer monsoon, and fall precipitation), a very clear pattern appeared for winter-spring and summer (Fig. 2 a and b). In general, negative SOI values (El Niño conditions, Fig. 2a) produce a marked increase in winter rainfall throughout the Mexican Pacific coast (although the significant points tend to concentrate toward the northwest), whereas La Niña conditions (Fig. 2b) tend to produce an increase in monsoon-type rainfall all along the continental coast of Mexico, including the southern reaches of the Sonoran.
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