Hostname: page-component-77c89778f8-9q27g Total loading time: 0 Render date: 2024-07-18T06:38:17.115Z Has data issue: false hasContentIssue false

VII. Observations of the Places of the Georgian Planet, made at Edinburgh with an Equatoreal Instrument

Published online by Cambridge University Press:  17 January 2013

John Robison
Affiliation:
Professor of Natural Philosophy in theUniversity of Edinburgh

Extract

Hence it may be deduced, (by following the method described in a paper formerly read to this Society) that the planet was in opposition January 13a. 04b. 56′ M. T. Greenwich, in longitude, 3a. 23°. 32′. 24″ from the mean equinox, with −°. 30′. 38″ north heliocentric latitude.

The error of the theory in longitude is nearly +5″, and in latitude nearly −18″.

I attribute this error in latitude to the different manner in which I observed the declinations. I formerly obferved the difference of declination between the planet and fixed star by means of a common micrometer. But I was obliged to substitute Dr Bradley's rhombus for my micrometer, which had received an injury which I could not get repaired in time. If this be allowed, the error in longitude will be diminished nearly 2″.

Type
Papers Read Before the Society
Copyright
Copyright © Royal Society of Edinburgh 1790

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

* Transactions of the Royal Society of Edin. Vol. I. N° XI. Phys. Cl.