Abstract
Equatorial and tropical air masses largely control the humid tropical group of climates found at low latitudes. Every month of the year has an average temperature above 18°C, and no winter season. In these tropical systems, the primary periodic energy flux is diurnal: the temperature variation from day to night is greater than from season to season (see Figure 4.2, p. 35). Average annual rainfall is heavy and exceeds annual evaporation, but varies in amount, season, and distribution.
Preview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1998 Springer-Verlag Berlin Heidelberg
About this chapter
Cite this chapter
Bailey, R.G. (1998). The Humid Tropical and Mountain Ecoregions. In: Ecoregions. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-2200-2_8
Download citation
DOI: https://doi.org/10.1007/978-1-4612-2200-2_8
Publisher Name: Springer, New York, NY
Print ISBN: 978-0-387-98311-0
Online ISBN: 978-1-4612-2200-2
eBook Packages: Springer Book Archive