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chapter - Atmospheric and Oceanic Science

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La Plata basin climatology<br />

FIG. 2.9. Littoral Region a) Location. Rainfall regime at characteristic sites: b) Center-North c) South<br />

region d) Eastern Region.<br />

Here the influence of the circulation of the West is especially important in<br />

winter. In this season, the cyclogenesis over either Uruguayan or the Argentine<br />

Mesopotamia has a maximum in frequency (Gan <strong>and</strong> Rao 1991; Vigliarolo 1998).<br />

The further displacement toward the Southeast of these recently generated low<br />

pressures centres causes a maximum of precipitation by the end of winter, on the<br />

southeaster border of the continent, practically entirely outside La Plata basin.<br />

Spite of the relative proximity to the Atlantic Ocean, the region presents features<br />

of continental climate as in Winter there is frequent frosts, while in Summer,<br />

the daily maximum temperatures usually exceed the 36ºC (except near the coast),<br />

especially during the second half of December <strong>and</strong> January.<br />

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