The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
History
The story of the universe. Volume 2 (of 4) : $b The earth : land and sea
Astronomy; Earth (Planet); Natural history
In order to facilitate our reasoning I have assumed that the moon
is the only tide-producing agent; this is, however, not the case.
No doubt the ebb and the flow around our coasts is generated mainly
by the attraction of the moon. It must not, however, be forgotten
that a portion of the tide is originated by the attraction of the
sun. These solar tides will still continue to ebb and flow quite
independently of the lunar tides, so that even if the accommodation
between the earth and the moon had been completed some further tidal
disturbance would not be wanting. The effect of the solar tides will
be to abate still further the velocity with which the earth turns
round on its axis, and consequently a time must ultimately arrive
when the length of the day will be longer than the time which the
moon takes to revolve around our earth.
THE GULF STREAM
--LORD KELVIN
I mean by the Gulf Stream that mass of heated water which pours from
the Strait of Florida across the North Atlantic, and likewise a wider
but less definite warm current, evidently forming part of the same
great movement of water, which curves northward to the eastward of
the West Indian Islands. I am myself inclined, without hesitation,
to regard this stream as simply the reflux of the equatorial
current, added to no doubt during its northeasterly course by the
surface-drift of the anti-trades which follows in the main the same
direction.
The scope and limit of the Gulf Stream will be better understood if
we inquire in the first place into its origin and cause. As is well
known--in two bands, one to the north and the other to the south
of the equator--the northeast and southeast trade-winds, reduced
to meridional directions by the eastward frictional impulse of the
earth’s rotation, drive before them a magnificent surface current of
hot water 4,000 miles long by 450 miles broad at an average rate of
thirty miles a day. Off the coast of Africa, near its starting-point
to the south of the Islands of St. Thomas and Anna Bon this
“equatorial current” has a speed of forty miles in the twenty-four
hours, and a temperature of 23° C.
Public-domain text, read in full here on John Shaqi.
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