William Ferrel

 
Scientist:

William Ferrel

American meteorologist (1817–1891)

Born in Fulton County, Pennsylvania, Ferrel moved with his family to farm in West Virginia in 1829. Receiving only the most rudimentary education, his early scientific knowledge was entirely self acquired. Despite this he developed an interest in mathematical physics and, after graduating from Bethany College in West Virginia in 1844, began to study the Principia of Isaac Newton and the Mécanique céleste (Celestial Mechanics) of Pierre Simon de Laplace. He earned his living as a school teacher from 1844 until 1857 when, having established his scientific reputation, he was appointed to the staff of the American Ephemeris and Nautical Almanac. He worked there until 1867 when he joined the US Coast and Geodetic Survey.

In 1856 he published his most significant work, Essay on the Winds and Currents of the Oceans. He showed that all atmospheric motion, as well as ocean currents, are deflected by the Earth's rotation. He went on in 1858 to formulate his law, which states that if a mass of air is moving in any direction there is a force arising from the Earth's rotation that always deflects it to the right in the northern hemisphere and to the left in the southern hemisphere. The air tends to move in a circle whose radius depends upon its velocity and distance from the equator. Ferrel went on to show how this law could be used to explain storms and the pattern of winds and currents. He was in some ways anticipated by Gustave-Gaspard Coriolis whose name is much better known.

Ferrel also did fundamental work on the solar system. He was able to correct Laplace and show that the tidal action of the Sun and Moon on the Earth is slowly retarding the Earth's rotation. In 1864 he provided the first mathematical treatment of tidal friction. His other works included his three-volume Meteorological Researches (1877–82). In 1880 he invented a machine to predict tidal maxima and minima.

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Wikipedia: William Ferrel
This page is about the meteorologist; for the comedian, see Will Ferrell.
William Ferrel
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William Ferrel

William Ferrel (18171891), an American meteorologist, developed theories which explained the mid-latitude atmospheric circulation cell in detail, and it is after him that the Ferrel cell is named.

Ferrel demonstrated that it is the tendency of rising warm air, as it rotates due to the Coriolis effect, to pull in air from more southerly, warmer regions and transport it poleward. It is this rotation which creates the complex curvatures in the frontal systems separating the cooler Arctic air to the north from the warmer continental tropical air to the south.

Ferrel improved upon Hadley's theory by recognizing an until then overlooked mechanism. A quote from his first paper:

The fourth and last force arises from the combination of a relative east or west motion of the atmosphere with the rotatory motion of the earth. In consequence of the atmosphere's revolving on a common axis with that of the earth, each particle is impressed with a centrifugal force, which, being resolved into a vertical and a horizontal force, the latter causes it to assume a spheroidal form conforming to the figure of the earth. But, if the rotatory motion of any part of the atmosphere has a relative eastern motion with regard to the earth's surface, this force is increased, and if it has a relative western motion, it is diminished, and this difference gives rise to a disturbing force which prevents the atmosphere being in a state of equilibrium, with a figure conforming to that of the earth's surface, but causes accumulation of the atmosphere at certain latitudes and a depression at others, and the consequent differences in the pressure of the atmosphere in these latitudes very materially influences its motions. [1]

Hadley's erroneous reasoning had been in terms of a tendency to conserve linear momentum, as air mass travels from north to south or from south to north. Ferrel recognized that in meteorology and oceanography what needs to be taken into account is a tendency of an air mass that is in motion relative to the earth to conserve the angular momentum (of its angular velocity with respect to the earth's axis).

  1. ^ Ferrel, W. 'An essay on the winds and the currents of the Oceans', Nashville journal of medicine and surgery, 1856.
    An essay on the winds and the currents of the Oceans (PDF-file 1.4 MB, scanned images of entire pages.)

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