A History of Science — Volume 3Williams, Henry Smith
History
A History of Science — Volume 3
Williams, Henry Smith
Science -- History
Meantime, however, it is by no means sure that gravitation does not
enter into the case to the extent of producing an insensible general
oceanic circulation, independent of the Gulf Stream and similar marked
currents, and similar in its larger outlines to the polar-equatorial
circulation of the air. The idea of such oceanic circulation was first
suggested in detail by Professor Lenz, of St. Petersburg, in 1845, but
it was not generally recognized until Dr. Carpenter independently hit
upon the idea more than twenty years later. The plausibility of the
conception is obvious; yet the alleged fact of such circulation has been
hotly disputed, and the question is still sub judice.
But whether or not such general circulation of ocean water takes place,
it is beyond dispute that the recognized currents carry an enormous
quantity of heat from the tropics towards the poles. Dr. Croll, who has
perhaps given more attention to the physics of the subject than almost
any other person, computes that the Gulf Stream conveys to the North
Atlantic one-fourth as much heat as that body receives directly from the
sun, and he argues that were it not for the transportation of heat by
this and similar Pacific currents, only a narrow tropical region of the
globe would be warm enough for habitation by the existing faunas. Dr.
Croll argues that a slight change in the relative values of northern
and southern trade-winds (such as he believes has taken place at various
periods in the past) would suffice to so alter the equatorial current
which now feeds the Gulf Stream that its main bulk would be deflected
southward instead of northward, by the angle of Cape St. Roque. Thus the
Gulf Stream would be nipped in the bud, and, according to Dr. Croll's
estimates, the results would be disastrous for the northern hemisphere.
The anti-trades, which now are warmed by the Gulf Stream, would then
blow as cold winds across the shores of western Europe, and in all
probability a glacial epoch would supervene throughout the northern
hemisphere.
Public-domain text, read in full here on John Shaqi.
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