Yale University Observatory

Yale University's Observatory, the Atheneum, was founded in 1830. The observatory was renamed to the Leitner Family Observatory and Planetarium in 2008. Beginning in 1830, it housed a 5-inch refractor which was the largest in Americas at the time. A number of telescopes have been mounted in the observatory including a 9-inch Alvan Clark refractor in 1870, a heliometer in 1880 and an 8-inch (200 mm) telescope in 1882. The observatory was credited with the first American viewing of the return of Halley's Comet in 1835, photographing the Sun during the Transit of Venus, pioneering work in the study of meteors and to monitoring the motion of the axis of the earth. The observatory now uses a refurbished 8-inch Reed refractor for visual observations of planets and stars.

History

Yale's first observatory, the Atheneum, was situated in a tower, which from 1830 housed Yale's first and America's largest refractor, a 5-inch (130 mm) Dollond donated by Sheldon Clark. With this telescope Olmsted and Elias Loomis made the first American sighting of the return of Halley's Comet in 1835. (August 31; seen in Europe August 6, but no news of this had reached America). The telescope was mounted on casters and moved from window to window, but it could not reach altitudes much over 30 deg above the horizon.

In 1870, a cylindrical turret was added above the tower, so that all altitudes could be reached. The building was demolished in 1893 and the telescope is now at the Smithsonian Institution in Washington, D.C.

The observatory, in the turret (modelled after the gun turret of the ironclad ship USS Monitor), housed a 9-inch (230 mm) Alvan Clark refractor donated by Joseph E. Sheffield. The telescope was later housed in the dome on Bingham Hall (the dome later converted to a small planetarium, and now used as an experimental aquarium).

An 8-inch (200 mm) telescope financed by E.M. Reed of New Haven was first used for photographing the Sun during the Transit of Venus on December 6, 1882.

The observatory also possessed an heliometer, ordered from Repsold and Sons by H. A. Newton in 1880, delivered in time for measurements of the Transit of Venus on December 6, 1882 for determination of solar parallax. This is the same type of instrument that Friedrich Bessel used in 1838 for the first significant determination of a stellar parallax (of the star 61 Cygni). Under the direction of W. L. Elkin from 1883 to 1910 the heliometer yielded (according to Frank Schlesinger) the most (238) and the best parallaxes obtained before the advent of photographic astrometry.

In the late 1890s, W. L. Elkin built two batteries of cameras equipped with rotating shutters for obtaining the velocities as well as the heights of meteors, pioneering work in the study of meteors.[1]

The Loomis Tower on Canner Street, erected in 1923 in memory of Elias Loomis (1811–1889), was at the time the largest polar telescope in America. The installation was originally designed for the comfort of the observer who sat at the eyepiece in a warm room at the top of the tower. The tube (beneath the stairs) was parallel to the polar axis of the Earth. The building at the base of the tower had a sliding roof and housed a 30-inch (760 mm) optical flat coelostat mirror driven equatorially and reflecting light from any unobscured part of the sky through both a 15-inch (380 mm) photographic and a 10-inch (250 mm) visual guide telescope, both of the same focal length, 600 inches.

In 1945, the telescope was reversed, with the 15-inch (380 mm) objective at the top, the plate holder at the foot of the tube. The telescope was thus rigidly mounted for photographing the polar region only, for the purpose of investigating the wobbling of the axis of rotation of the earth and redetermining the constants of precession and nutation.

The Loomis Telescope was moved to Bethany, Connecticut in 1957, to continue monitoring the apparent motion of the axis of the earth. Carol Williams analyzed plates for her Ph.D. thesis, 1967. She found apparent motions largely correlated with tidal disturbances of the earth's crust.

See also

References

  1. ↑

External links

Coordinates: 41°19′03″N 72°55′17″W / 41.3174°N 72.9215°W / 41.3174; -72.9215

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