The Common Nature of Epidemics, and their relation to climate and civilization — John Shaqi
The Common Nature of Epidemics, and their relation to climate and civilizationSmith, Southwood
History
The Common Nature of Epidemics, and their relation to climate and civilization
Smith, Southwood
Communicable diseases; Epidemics; Quarantine
Overcrowding, for example, we can prevent; the accumulation of filth in
towns and houses we can prevent; the supply of light, air, and water,
together with the several other appliances included in the
all-comprehensive word CLEANLINESS, we can secure. To the extent to
which it is in our power to do this, it is in our power to prevent
epidemics.
The human family have now lived together in communities more than six
thousand years, yet they have not learnt to make their habitations
clean. At last we are beginning to learn the lesson. When we shall have
mastered it, we shall have conquered epidemics. Our duties, then, and
our hopes in this respect, I shall proceed to show.
* * * * *
The principal constituents of the atmosphere maintain their equilibrium
steadily over the whole surface of the globe. There is scarcely any
difference in the relative proportion of its oxygen and nitrogen in the
torrid zone and in the arctic regions. Whatever influence the atmosphere
may have on climate must consequently depend on something adventitious
to it and not in anything forming a part of it. Possibly therefore that
something may be, in some degree, under human control.
The main constituents of climate are temperature and moisture, and these
are the climatic conditions that exercise the greatest influence on
epidemics.
Minor but still important conditions are the nature of the soil, the
proportion of land that is cleared and under cultivation, the extent of
forests, lakes, and rivers, the prevailing winds, the electrical state
of the atmosphere, and so on.
The temperature is highest where the sun’s rays are vertical, or nearly
so; where the sky is cloudless; where the day is longest; and where
there is the smallest difference between the fervid noon-tide heat and
the temperature of the short night.
The moisture is greatest where in addition to all the other sources of
humidity there are periodical rains. In the countries subject to these
rains, the entire extent of the level and low land is often covered a
foot deeper with water than before the rain set in.
Elevated temperature and excessive moisture are combined in tropical
countries; and they are concentrated in those parts of the tropics in
which there are extensive forests having an undergrowth of luxuriant
vegetation; in which the tides of the ocean penetrate deeply into the
interior of the land, and mix with the waters of the rivers; and in
which the rivers constantly overflow their banks and form marshes and
swamps.
In tropical countries there are tracts such as these that extend in
unbroken continuity hundreds of leagues. The western coast of Africa
(the Bight of Benin) presents an unbroken area of upwards of 100,000
square miles, consisting of one vast alluvial and densely-wooded forest,
irrigated by Atlantic tides, and intersected by numerous rivers and
creeks, whose muddy banks are constantly overflowed.
Public-domain text, read in full here on John Shaqi.
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