Earth current

Definition and stakes

Michael August Friedrich Prestel,  Popular Science Monthly (1877)

“ The terrestrial atmospheric currents, in their passage over the same portion of the earth's surface (whether this passage be periodic or not periodic) , never take the same route, or have the same limits, and consequently the localities over which they pass on their return will happen to be at one time in the centre of the current, at another time more or less near to its northern or its southern edge. ”
Source: Wikisource

Portrait of Matthew Fontaine Maury Matthew Fontaine Maury,  Physical Geography of the Sea and its Meteorology (1864)

“ The production of currents without wind.—For the sake of further illustration, let us suppose a globe of the earth's size, and with a solid nucleus, to be covered all over with water two hundred fathoms deep, and that every source of heat and cause of radiation be removed, so that its fluid temperature becomes constant and uniform throughout. On such a globe, the equilibrium remaining undisturbed, there would be neither wind nor current. Let us now suppose that all the water within the tropics, to the depth of one hundred fathoms, suddenly becomes oil. ”
Source: Wikisource

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