Tropical nature, and other essaysWallace, Alfred Russel
History
Tropical nature, and other essays
Wallace, Alfred Russel
Ecology -- Tropics; Natural history -- Tropics; Tropics
Old Opinions on Continental Changes--Theory of Oceanic
Islands--Present and Past Distribution of Land and
Sea--Zoological Regions--The Palæarctic Region--The Ethiopian
Region--The Oriental Region--Past changes of the Great Eastern
Continent--Regions of the New World--Past History of the American
Continents--The Australian Region--Summary and Conclusion
_pages 304-347_
TROPICAL NATURE,
AND OTHER ESSAYS.
I.
THE CLIMATE AND PHYSICAL ASPECTS OF THE EQUATORIAL ZONE.
The three Climatal Zones of the Earth--Temperature of the
Equatorial Zone--Causes of the Uniform High Temperature near
the Equator--Influence of the Heat of the Soil--Influence of
the Aqueous Vapour of the Atmosphere--Influence of Winds on
the Temperature of the Equator--Heat due to the Condensation
of Atmospheric Vapour--General features of the Equatorial
Climate--Uniformity of the Equatorial Climate in all parts of the
globe--Effects of Vegetation on Climate--Short Twilight of the
Equatorial Zone--The aspect of the Equatorial Heavens--Intensity
of meteorological phenomena at the Equator--Concluding Remarks.
It is difficult for an inhabitant of our temperate land to realize
either the sudden and violent contrasts of the arctic seasons or the
wonderful uniformity of the equatorial climate. The lengthening or
the shortening days, the ever-changing tints of spring, summer, and
autumn, succeeded by the leafless boughs of winter, are constantly
recurring phenomena which represent to us the established course
of nature. At the equator none of these changes occur; there is
a perpetual equinox and a perpetual summer, and were it not for
variations in the quantity of rain, in the direction and strength
of the winds, and in the amount of sunshine, accompanied by
corresponding slight changes in the development of vegetable and
animal life, the monotony of nature would be extreme.
In the present chapter it is proposed to describe the chief
peculiarities which distinguish the equatorial from the temperate
climate, and to explain the causes of the difference between
them,--causes which are by no means of so simple a nature as are
usually imagined.
Public-domain text, read in full here on John Shaqi.
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