The Energy System of Matter: A Deduction from Terrestrial Energy PhenomenaWeir, James, active 1883-1912
Science
The Energy System of Matter: A Deduction from Terrestrial Energy Phenomena
Weir, James, active 1883-1912
Force and energy
atmospheric mass was indicated by its elevation or its energy of
position. In the descent this energy is thus entirely transformed, and
reverts once more to its original form of energy of rotation.
The continual transformation of axial energy by the aqueous vapour, and
the conversion of that energy by the upward movement of the air masses
into energy of position, naturally tends to produce a retardative effect
on the motion of revolution of the earth. But this retardative effect is
in turn completely neutralised or balanced by the corresponding
accelerative effect due to the equally continuous return as the energy
of the air masses reverts in the continuous polar movement to its
original axial form. Speaking generally, the equatorial regions, or the
regions of high velocity, are the location of the most powerful
transformation or abstraction of axial energy by the aqueous vapour.
Conversely, the polar or regions of low velocity are the location of the
greatest return of energy by the air. As no energy return is possible
unless by the transference of the atmospheric material from regions of
high to regions of low velocity, the configuration of the planet in
rotation must conform to this condition. The spheroidal form of the
earth is thus exquisitely adapted to the working of the atmospheric
machine. As already pointed out, however, the energising and raising of
atmospheric masses is by no means confined to equatorial regions, but
takes place more or less over the whole planetary surface. The same
applies to the energy return. The complete cycle may be carried out in
temperate zones; gaseous masses, also, leaving equatorial regions at
high altitudes do not necessarily reach the polar regions, but may
attain their lowest levels at intermediate points. Neither do such
masses necessarily proceed to the regions of low velocity by purely
linear paths. On the contrary, they may and do move both towards the
poles and downwards by circuitous and even vortical paths. In fact, as
will be readily apparent, their precise path is of absolutely no moment
in the consideration of energy return.
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