Miscellanea Curiosa, Vol. 1: Containing a collection of some of the principal phaenomena in nature, accounted for by the greatest philosophers of this age
History
Miscellanea Curiosa, Vol. 1: Containing a collection of some of the principal phaenomena in nature, accounted for by the greatest philosophers of this age
Natural history; Science -- Early works to 1800; Voyages and travels -- Early works to 1800
In the foregoing History are contained several Problems, that merit well
the Consideration of our acutest Naturalists, both by reason of the
constancy of the Effect, and of the immense Extent thereof; near half
the Surface of the Globe being concerned. The chief of these Problems
are, 1. Why these Winds are perpetually from the East in the _Atlantic_
and _Æthiopick_; as likewise in the _Pacifick_ Ocean, between the
Latitudes of 30 North and South? 2. Why the said Winds extend no farther
with constancy than to the Latitude of 30 Degrees? 3. Why there should
be a constant South-Westerly Wind upon and near the Coast of _Guinea_?
4. Why in the North part of the _Indian_ Ocean, the Winds, which for one
half Year do agree with those of the other two Oceans, should change in
other half Year, and blow from the opposite Points; whilst the Southern
part of that Ocean follows the General Rule, and has perpetual Winds
about S. E? 5. Why in these General Trade-Winds it should be always
true, that to the Northward of the _Æquator_ it is inclin'd to the
Northwards of the East; and in South Latitudes, to the Southward
thereof? 6. Why in these Seas of _China_ there should be so great an
Inclination from the East to the North, more than elsewhere? with many
more, which it would be much easier to propose than answer.
But lest I should seem to propose to others, Difficulties which I have
not thought worth my own Time and Pains, take here the result of an
earnest Endeavour after the true reason of the aforesaid _Phænomena_;
wherein if I am not able to account for all Particulars, yet 'tis hoped
the Thoughts I have spent thereon, will not be judged wholly lost, by
the Curious in Natural Enquiries.
Wind is most properly defined to be the Stream or Current of the Air,
and where such a Current is perpetual and fixt in its Course, 'tis
necessary that it proceed from a permanent un-intermitting Cause.
Wherefore some have been inclin'd to propose the diurnal _Rotation_ of
the Earth upon its _Axis_, by which, as the _Globe_ turns Eastwards, the
loose and _fluid_ Particles of the Air, being so exceeding light as they
be, are left behind, so that in respect of the Earths _Surface_ they
move Westwards, and become a constant Easterly Wind. This Opinion seems
confirm'd, for that these Winds are found only near the _Æquinoctial_,
in those Parallels of Latitude where the diurnal Motion is swiftest; and
I should readily assent to it, if the constant Calms in the _Atlantick_
Sea, near the _Æquator_, the Westerly Winds near the Coast of _Guinea_;
and the _Periodical_ Westerly _Monsoons_ under the _Æquator_ in the
_Indian_ Seas, did not declare the insufficency of that _Hypothesis_.
Besides the Air being kept to the Earth by the Principle of _Gravity_,
would acquire the same degree of _Velocity_ that the Earths _Surface_
moves with, as well in respect of the diurnal _Rotation_, as of the
Annual about the Sun, which is about thirty times swifter.
Public-domain text, read in full here on John Shaqi.
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