Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 2 - By Alexander Von Humboldt And Aime Bonpland.
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The Season Of Rains Is That Of Storms; And Yet
A Great Number Of Experiments Made During Three Years, Prove To Me
That It Is Precisely In This Season Of Storms We Find The Smallest
Degree Of Electric Tension In The Lower Regions Of The Atmosphere.
Are
storms the effect of this unequal charge of the different
superincumbent strata of air?
What prevents the electricity from
descending towards the earth, in air which becomes more humid after
the month of March? The electricity at this period, instead of being
diffused throughout the whole atmosphere, appears accumulated on the
exterior envelope, at the surface of the clouds. According to M.
Gay-Lussac it is the formation of the cloud itself that carries the
fluid toward its surface. The storm rises in the plains two hours
after the sun has passed the meridian; consequently a short time after
the moment of the maximum of diurnal heat within the tropics. It is
extremely rare in the islands to hear thunder during the night, or in
the morning. Storms at night are peculiar to certain valleys of
rivers, having a peculiar climate.
What then are the causes of this rupture of the equilibrium in the
electric tension of the air? of this continual condensation of the
vapours into water? of this interruption of the breezes? of this
commencement and duration of the rainy seasons? I doubt whether
electricity has any influence on the formation of vapours. It is
rather the formation of these vapours that augments and modifies the
electrical tension.
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