_Without Ocean-currents the Globe would not be habitable._—All these
foregoing considerations show to what an extent the climatic condition
of our globe is due to the thermal influences of ocean-currents.
As regards the northern hemisphere, we have two immense oceans, the
Pacific and the Atlantic, extending from the equator to near the north
pole, or perhaps to the pole altogether. Between these two oceans lie
two great continents, the eastern and the western. Owing to the earth’s
spherical form, far too much heat is received at the equator and far
too little at high latitudes to make the earth a suitable habitation
for sentient beings. The function of these two great oceans is to
remove the heat from the equator and carry it to temperate and polar
regions. Aërial currents could not do this. They might remove the heat
from the equator, but they could not, as we have already seen, carry
it to the temperate and polar regions; for the greater portion of the
heat which aërial currents remove from the equator is dissipated into
stellar space: the ocean alone can convey the heat to distant shores.
But aërial currents have a most important function; for of what avail
would it be, though ocean-currents should carry heat to high latitudes,
if there were no means of distributing the heat thus conveyed over the
land? The function of aërial currents is to do this. Upon this twofold
arrangement depends the thermal condition of the globe. Exclude the
waters of the Pacific and the Atlantic from temperate and polar regions
and place them at the equator, and nothing now existing on the globe
could live in high latitudes.
Were these two great oceans placed beside each other on one side of the
globe, and the two great continents placed beside each other on the
other side, the northern hemisphere would not then be suitable for the
present order of things: the land on the central and on the eastern
side of the united continent would be far too cold.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account