A megathermal climate is one with persistent high temperatures and abundant rainfall, with potential annual evaporation in excess of.
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Megathermal climates are sometimes split into two temperature-based subsets & mdash; "'equatorial "'and "'tropical "'( the latter used here in the sense of " outer tropical " ) & mdash; with " equatorial " denoting little or no variation in temperature throughout the year and " tropical " denoting significant seasonal variation, even though no month has an average temperature of below 18�C . In addition, what temperature fluctuations do exist in an equatorial climate will typically bear no relationship to the astronomical seasons for the applicable side of the equator, while in the ( outer ) tropical subtype the temperature will move in concert with the seasons, the time of higher sun and longer days being warmest and the time of lower sun and shorter days coolest.
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