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The
circulation of the atmosphere, Plate III
Southeast
trade-wind region the larger
The
offices of the atmosphere
It
is a powerful machine
Whence
come the rains that feed the great rivers
How
vapor passes from one hemisphere to the other
Evaporation
greatest about latitude 17o-20o
The
rainy seasons
Rainless
regions
Why
mountains have a dry and a rainy side
The
immense fall of rain upon the Western Ghauts in India: how caused
Vapor
for the Patagonia rains comes from the North Pacific
The
mean annual fall of rain
Evaporation
from the Indian Ocean
Evidences
of design
Adaptation
Table
of Contents
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