Equinoctial rains: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">Rainy seasons that occur regularly in many places within a few degrees of the [[equator]] at or shortly after the [[equinoxes]].</div><br/> <div class="paragraph">This characteristic of two distinct annual [[precipitation]] maxima is found chiefly within a [[tropical rain forest climate]]. The main regions are the Congo Valley, the greater Amazon Valley, and the East Indies. In most places, the spring maximum is the greater. <br/>''Compare'' [[zenithal rains]].</div><br/> </div> | <div class="definition"><div class="short_definition">Rainy seasons that occur regularly in many places within a few degrees of the [[equator]] at or shortly after the [[equinox|equinoxes]].</div><br/> <div class="paragraph">This characteristic of two distinct annual [[precipitation]] maxima is found chiefly within a [[tropical rain forest climate]]. The main regions are the Congo Valley, the greater Amazon Valley, and the East Indies. In most places, the spring maximum is the greater. <br/>''Compare'' [[zenithal rains]].</div><br/> </div> | ||
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Latest revision as of 15:55, 25 April 2012
equinoctial rains
Rainy seasons that occur regularly in many places within a few degrees of the equator at or shortly after the equinoxes.
This characteristic of two distinct annual precipitation maxima is found chiefly within a tropical rain forest climate. The main regions are the Congo Valley, the greater Amazon Valley, and the East Indies. In most places, the spring maximum is the greater.
Compare zenithal rains.
Compare zenithal rains.