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Yale University Observatory

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The Yale University Observatory , also known as the Leitner Family Observatory and Planetarium , is an astronomical observatory owned and operated by Yale University , and maintained for student use. It is located in Farnham Memorial Gardens near the corner of Edwards and Prospect Streets, New Haven , Connecticut .

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60-716: In the 21st century, the Yale Student Observatory, the Leitner observatory also has public outreaches and supports astronomy for students of the college. However, the Yale Observatory traces its history back to being one of the first formal institutions for astronomical observation in the United States, dating to the 1830s. In 1828 Sheldon Clark donated 1200 US dollars to Yale to procure a Dollond refracting telescope. Yale's first observatory ,

120-399: 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

180-492: A 16" RCOS telescope and a refurbished refractor from the Grubb Telescope Company (originally purchased to observe the 1882 transit of Venus). Detectors include an SBIG ST-9E CCD camera and a DSS-7 spectrograph . There is an observing deck between the domes. The observatory also houses a digital planetarium theater, which uses a Spitz SciDomeHD projection system. Observatory An observatory

240-702: A large percentage of clear nights per year, dry air, and are at high elevations. At high elevations, the Earth's atmosphere is thinner, thereby minimizing the effects of atmospheric turbulence and resulting in better astronomical " seeing ". Sites that meet the above criteria for modern observatories include the southwestern United States , Hawaii , Canary Islands , the Andes , and high mountains in Mexico such as Sierra Negra . Major optical observatories include Mauna Kea Observatory and Kitt Peak National Observatory in

300-493: A lot of angular rotating velocity with respect to the rotation around the pivot axis, and as dm 1 is forced closer to the pivot axis of the rotation (by the wheel spinning further), because of the Coriolis effect , with respect to the vertical pivot axis, dm 1 tends to move in the direction of the top-left arrow in the diagram (shown at 45°) in the direction of rotation around the pivot axis. Section dm 2 of

360-454: A particular geographic area ( European Audiovisual Observatory ). Astronomical observatories are mainly divided into four categories: space-based , airborne , ground-based, and underground-based. Historically, ground-based observatories were as simple as containing an astronomical sextant (for measuring the distance between stars ) or Stonehenge (which has some alignments on astronomical phenomena). Ground-based observatories, located on

420-596: A remote 5,640 m (18,500 ft) mountaintop in the Atacama Desert of Chile. The oldest proto-observatories, in the sense of an observation post for astronomy, The oldest true observatories, in the sense of a specialized research institute , include: Space-based observatories are telescopes or other instruments that are located in outer space , many in orbit around the Earth. Space telescopes can be used to observe astronomical objects at wavelengths of

480-477: A small rotation vector ω dt for the short time dt ; e.g.: R new = exp ⁡ ( [ ω ( R old ) ] × d t ) R old {\displaystyle {\boldsymbol {R}}_{\text{new}}=\exp \left(\left[{\boldsymbol {\omega }}\left({\boldsymbol {R}}_{\text{old}}\right)\right]_{\times }dt\right){\boldsymbol {R}}_{\text{old}}} for

540-673: A small rotation vector v perpendicular to both ω and L , noting that E ( exp ⁡ ( [ v ] × ) R ) ≈ E ( R ) + ( ω ( R ) × L ) ⋅ v {\displaystyle E\left(\exp \left(\left[{\boldsymbol {v}}\right]_{\times }\right){\boldsymbol {R}}\right)\approx E\left({\boldsymbol {R}}\right)+\left({\boldsymbol {\omega }}\left({\boldsymbol {R}}\right)\times {\boldsymbol {L}}\right)\cdot {\boldsymbol {v}}} Torque-induced precession ( gyroscopic precession )

600-419: A week at the absolute reference point calibration measurements are performed. Example magnetic observatories include: Example seismic observation projects and observatories include: Example gravitational wave observatories include: A volcano observatory is an institution that conducts the monitoring of a volcano as well as research in order to understand the potential impacts of active volcanism. Among

660-429: Is a change in the orientation of the rotational axis of a rotating body. In an appropriate reference frame it can be defined as a change in the first Euler angle , whereas the third Euler angle defines the rotation itself . In other words, if the axis of rotation of a body is itself rotating about a second axis, that body is said to be precessing about the second axis. A motion in which the second Euler angle changes

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720-833: Is a facility which precisely measures the total intensity of Earth's magnetic field for field strength and direction at standard intervals. Geomagnetic observatories are most useful when located away from human activities to avoid disturbances of anthropogenic origin, and the observation data is collected at a fixed location continuously for decades. Magnetic observations are aggregated, processed, quality checked and made public through data centers such as INTERMAGNET . The types of measuring equipment at an observatory may include magnetometers (torsion, declination-inclination fluxgate, proton precession, Overhauser-effect), variometer (3-component vector, total-field scalar), dip circle , inclinometer , earth inductor, theodolite , self-recording magnetograph, magnetic declinometer, azimuth compass. Once

780-489: Is a location used for observing terrestrial, marine, or celestial events. Astronomy , climatology / meteorology , geophysics , oceanography and volcanology are examples of disciplines for which observatories have been constructed. The term observatoire has been used in French since at least 1976 to denote any institution that compiles and presents data on a particular subject (such as public health observatory ) or for

840-444: Is a scientific institution whose main task is to make observations in the fields of meteorology, geomagnetism and tides that are important for the navy and civil shipping. An astronomical observatory is usually also attached. Some of these observatories also deal with nautical weather forecasts and storm warnings, astronomical time services, nautical calendars and seismology. Example marine observatories include: A magnetic observatory

900-402: Is added to rotation around a vertical axis. It is important to note that the torque around the gimbal axis arises without any delay; the response is instantaneous. In the discussion above, the setup was kept unchanging by preventing pitching around the gimbal axis. In the case of a spinning toy top, when the spinning top starts tilting, gravity exerts a torque. However, instead of rolling over,

960-563: Is also the mechanism behind gyrocompasses . Precession is the change of angular velocity and angular momentum produced by a torque. The general equation that relates the torque to the rate of change of angular momentum is: τ = d L d t {\displaystyle {\boldsymbol {\tau }}={\frac {\mathrm {d} \mathbf {L} }{\mathrm {d} t}}} where τ {\displaystyle {\boldsymbol {\tau }}} and L {\displaystyle \mathbf {L} } are

1020-431: Is applied to the body. In torque-free precession, the angular momentum is a constant, but the angular velocity vector changes orientation with time. What makes this possible is a time-varying moment of inertia , or more precisely, a time-varying inertia matrix . The inertia matrix is composed of the moments of inertia of a body calculated with respect to separate coordinate axes (e.g. x , y , z ). If an object

1080-925: Is asymmetric about its principal axis of rotation, the moment of inertia with respect to each coordinate direction will change with time, while preserving angular momentum. The result is that the component of the angular velocities of the body about each axis will vary inversely with each axis' moment of inertia. The torque-free precession rate of an object with an axis of symmetry, such as a disk, spinning about an axis not aligned with that axis of symmetry can be calculated as follows: ω p = I s ω s I p cos ⁡ ( α ) {\displaystyle {\boldsymbol {\omega }}_{\mathrm {p} }={\frac {{\boldsymbol {I}}_{\mathrm {s} }{\boldsymbol {\omega }}_{\mathrm {s} }}{{\boldsymbol {I}}_{\mathrm {p} }\cos({\boldsymbol {\alpha }})}}} where ω p

1140-444: Is called nutation . In physics , there are two types of precession: torque -free and torque-induced. In astronomy, precession refers to any of several slow changes in an astronomical body's rotational or orbital parameters. An important example is the steady change in the orientation of the axis of rotation of the Earth , known as the precession of the equinoxes . Torque-free precession implies that no external moment (torque)

1200-428: Is created. Under these circumstances the angular velocity of precession is given by: where I s is the moment of inertia , ω s is the angular velocity of spin about the spin axis, m is the mass, g is the acceleration due to gravity, θ is the angle between the spin axis and the axis of precession and r is the distance between the center of mass and the pivot. The torque vector originates at

1260-463: Is generally accepted to be the earliest known astronomer to recognize and assess the precession of the equinoxes at about 1° per century (which is not far from the actual value for antiquity, 1.38°), although there is some minor dispute about whether he was. In ancient China , the Jin-dynasty scholar-official Yu Xi ( fl. 307–345 AD) made a similar discovery centuries later, noting that

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1320-658: Is that, because of their location above the Earth's atmosphere, their images are free from the effects of atmospheric turbulence that plague ground-based observations. As a result, the angular resolution of space telescopes such as the Hubble Space Telescope is often much smaller than a ground-based telescope with a similar aperture . However, all these advantages do come with a price. Space telescopes are much more expensive to build than ground-based telescopes. Due to their location, space telescopes are also extremely difficult to maintain. The Hubble Space Telescope

1380-613: Is the Mauna Kea Observatory , located near the summit of a 4,205 m (13,796 ft) volcano in Hawaiʻi. The Chacaltaya Astrophysical Observatory in Bolivia, at 5,230 m (17,160 ft), was the world's highest permanent astronomical observatory from the time of its construction during the 1940s until 2009. It has now been surpassed by the new University of Tokyo Atacama Observatory , an optical-infrared telescope on

1440-485: Is the moment of inertia , T s is the period of spin about the spin axis, and τ is the torque . In general, the problem is more complicated than this, however. The special and general theories of relativity give three types of corrections to the Newtonian precession, of a gyroscope near a large mass such as Earth, described above. They are: The Schwarzschild geodesics (sometimes Schwarzschild precession)

1500-442: Is the phenomenon in which the axis of a spinning object (e.g., a gyroscope ) describes a cone in space when an external torque is applied to it. The phenomenon is commonly seen in a spinning toy top , but all rotating objects can undergo precession. If the speed of the rotation and the magnitude of the external torque are constant, the spin axis will move at right angles to the direction that would intuitively result from

1560-446: Is the precession rate, ω s is the spin rate about the axis of symmetry, I s is the moment of inertia about the axis of symmetry, I p is moment of inertia about either of the other two equal perpendicular principal axes, and α is the angle between the moment of inertia direction and the symmetry axis. When an object is not perfectly rigid , inelastic dissipation will tend to damp torque-free precession, and

1620-426: Is used in the prediction of the anomalous perihelion precession of the planets, most notably for the accurate prediction of the apsidal precession of Mercury In astronomy, precession refers to any of several gravity-induced, slow and continuous changes in an astronomical body's rotational axis or orbital path. Precession of the equinoxes, perihelion precession, changes in the tilt of Earth's axis to its orbit, and

1680-605: 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

1740-478: The Stratospheric Observatory for Infrared Astronomy use airplanes to observe in the infrared , which is absorbed by water vapor in the atmosphere. High-altitude balloons for X-ray astronomy have been used in a variety of countries. Example underground, underwater or under ice neutrino observatories include: Example meteorological observatories include: A marine observatory

1800-426: The eccentricity of its orbit over tens of thousands of years are all important parts of the astronomical theory of ice ages . (See Milankovitch cycles .) Axial precession is the movement of the rotational axis of an astronomical body, whereby the axis slowly traces out a cone. In the case of Earth, this type of precession is also known as the precession of the equinoxes , lunisolar precession , or precession of

1860-495: The equatorial bulge into the plane of the ecliptic , but instead causing it to precess. The torque exerted by the planets, particularly Jupiter , also plays a role. The orbits of planets around the Sun do not really follow an identical ellipse each time, but actually trace out a flower-petal shape because the major axis of each planet's elliptical orbit also precesses within its orbital plane, partly in response to perturbations in

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1920-408: 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,

1980-461: The skew-symmetric matrix [ ω ] × . The errors induced by finite time steps tend to increase the rotational kinetic energy: E ( R ) = ω ( R ) ⋅ L 2 {\displaystyle E\left({\boldsymbol {R}}\right)={\boldsymbol {\omega }}\left({\boldsymbol {R}}\right)\cdot {\frac {\boldsymbol {L}}{2}}} this unphysical tendency can be counteracted by repeatedly applying

2040-532: The Atheneum, was founded in 1830, situated in a tower. From 1830 it housed Yale's first refractor , a 5-inch (130 mm) Dollond donated by Sheldon Clark . It was the largest in the United States at the time. With this telescope Olmsted and Elias Loomis made the first American sighting of the return of Halley's Comet on 31 August 1835. (It had been seen in Europe on 6 August, but no news of this had reached

2100-529: The Solar System have a much smaller eccentricity and precess at a much slower rate, making them nearly circular and nearly stationary. Discrepancies between the observed perihelion precession rate of the planet Mercury and that predicted by classical mechanics were prominent among the forms of experimental evidence leading to the acceptance of Einstein 's Theory of Relativity (in particular, his General Theory of Relativity ), which accurately predicted

2160-631: The US, Roque de los Muchachos Observatory in Spain, and Paranal Observatory and Cerro Tololo Inter-American Observatory in Chile . Specific research study performed in 2009 shows that the best possible location for ground-based observatory on Earth is Ridge A  — a place in the central part of Eastern Antarctica. This location provides the least atmospheric disturbances and best visibility. Beginning in 1933, radio telescopes have been built for use in

2220-405: The United States.) 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. In the same year a 9-inch Alvan Clark refractor was mounted in the observatory. The building was demolished in 1893 and the telescope is now at

2280-515: 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 . The observatory was renamed as the Leitner Family Observatory and Planetarium in 2008. The observatory now uses a refurbished 8-inch Reed refractor for visual observations of planets and stars. It also includes two Ash domes housing

2340-723: The best known are the Hawaiian Volcano Observatory and the Vesuvius Observatory . Mobile volcano observatories exist with the USGS VDAP (Volcano Disaster Assistance Program), to be deployed on demand. Each volcano observatory has a geographic area of responsibility it is assigned to whereby the observatory is tasked with spreading activity forecasts, analyzing potential volcanic activity threats and cooperating with communities in preparation for volcanic eruption . Precession Precession

2400-631: The center of mass. Using ω = ⁠ 2π / T ⁠ , we find that the period of precession is given by: T p = 4 π 2 I s   m g r T s = 4 π 2 I s sin ⁡ ( θ )   τ T s {\displaystyle T_{\mathrm {p} }={\frac {4\pi ^{2}I_{\mathrm {s} }}{\ mgrT_{\mathrm {s} }}}={\frac {4\pi ^{2}I_{\mathrm {s} }\sin(\theta )}{\ \tau T_{\mathrm {s} }}}} Where I s

2460-463: The electromagnetic spectrum that cannot penetrate the Earth's atmosphere and are thus impossible to observe using ground-based telescopes. The Earth's atmosphere is opaque to ultraviolet radiation, X-rays , and gamma rays and is partially opaque to infrared radiation so observations in these portions of the electromagnetic spectrum are best carried out from a location above the atmosphere of our planet. Another advantage of space-based telescopes

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2520-406: The entire upper portion of the telescope dome can be rotated to allow the instrument to observe different sections of the night sky. Radio telescopes usually do not have domes. For optical telescopes, most ground-based observatories are located far from major centers of population, to avoid the effects of light pollution . The ideal locations for modern observatories are sites that have dark skies,

2580-482: The equator . Earth goes through one such complete precessional cycle in a period of approximately 26,000 years or 1° every 72 years, during which the positions of stars will slowly change in both equatorial coordinates and ecliptic longitude . Over this cycle, Earth's north axial pole moves from where it is now, within 1° of Polaris , in a circle around the ecliptic pole , with an angular radius of about 23.5°. The ancient Greek astronomer Hipparchus (c. 190–120 BC)

2640-402: The external torque. In the case of a toy top, its weight is acting downwards from its center of mass and the normal force (reaction) of the ground is pushing up on it at the point of contact with the support. These two opposite forces produce a torque which causes the top to precess. The device depicted on the right is gimbal mounted. From inside to outside there are three axes of rotation:

2700-670: The field of radio astronomy to observe the Universe in the radio portion of the electromagnetic spectrum. Such an instrument, or collection of instruments, with supporting facilities such as control centres, visitor housing, data reduction centers, and/or maintenance facilities are called radio observatories . Radio observatories are similarly located far from major population centers to avoid electromagnetic interference (EMI) from radio , TV , radar , and other EMI emitting devices, but unlike optical observatories, radio observatories can be placed in valleys for further EMI shielding. Some of

2760-455: The form of the changing gravitational forces exerted by other planets. This is called perihelion precession or apsidal precession . In the adjunct image, Earth's apsidal precession is illustrated. As the Earth travels around the Sun, its elliptical orbit rotates gradually over time. The eccentricity of its ellipse and the precession rate of its orbit are exaggerated for visualization. Most orbits in

2820-454: The heights of meteors , pioneering work in the study of meteors. 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

2880-399: The hub of the wheel, the gimbal axis, and the vertical pivot. To distinguish between the two horizontal axes, rotation around the wheel hub will be called spinning , and rotation around the gimbal axis will be called pitching . Rotation around the vertical pivot axis is called rotation . First, imagine that the entire device is rotating around the (vertical) pivot axis. Then, spinning of

2940-405: The instantaneous angular velocity is ω ( R ) = R I 0 − 1 R T L {\displaystyle {\boldsymbol {\omega }}\left({\boldsymbol {R}}\right)={\boldsymbol {R}}{\boldsymbol {I}}_{0}^{-1}{\boldsymbol {R}}^{T}{\boldsymbol {L}}} Precession occurs by repeatedly recalculating ω and applying

3000-477: The position of the Sun during the winter solstice had drifted roughly one degree over the course of fifty years relative to the position of the stars. The precession of Earth's axis was later explained by Newtonian physics . Being an oblate spheroid , Earth has a non-spherical shape, bulging outward at the equator. The gravitational tidal forces of the Moon and Sun apply torque to the equator, attempting to pull

3060-429: The rotation axis will align itself with one of the inertia axes of the body. For a generic solid object without any axis of symmetry, the evolution of the object's orientation, represented (for example) by a rotation matrix R that transforms internal to external coordinates, may be numerically simulated. Given the object's fixed internal moment of inertia tensor I 0 and fixed external angular momentum L ,

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3120-477: The spinning top just pitches a little. This pitching motion reorients the spinning top with respect to the torque that is being exerted. The result is that the torque exerted by gravity – via the pitching motion – elicits gyroscopic precession (which in turn yields a counter torque against the gravity torque) rather than causing the spinning top to fall to its side. Precession or gyroscopic considerations have an effect on bicycle performance at high speed. Precession

3180-414: The surface of Earth, are used to make observations in the radio and visible light portions of the electromagnetic spectrum . Most optical telescopes are housed within a dome or similar structure, to protect the delicate instruments from the elements. Telescope domes have a slit or other opening in the roof that can be opened during observing, and closed when the telescope is not in use. In most cases,

3240-440: 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

3300-405: The torque and angular momentum vectors respectively. Due to the way the torque vectors are defined, it is a vector that is perpendicular to the plane of the forces that create it. Thus it may be seen that the angular momentum vector will change perpendicular to those forces. Depending on how the forces are created, they will often rotate with the angular momentum vector, and then circular precession

3360-441: The wheel (around the wheelhub) is added. Imagine the gimbal axis to be locked, so that the wheel cannot pitch. The gimbal axis has sensors, that measure whether there is a torque around the gimbal axis. In the picture, a section of the wheel has been named dm 1 . At the depicted moment in time, section dm 1 is at the perimeter of the rotating motion around the (vertical) pivot axis. Section dm 1 , therefore, has

3420-430: The wheel is moving away from the pivot axis, and so a force (again, a Coriolis force) acts in the same direction as in the case of dm 1 . Note that both arrows point in the same direction. The same reasoning applies for the bottom half of the wheel, but there the arrows point in the opposite direction to that of the top arrows. Combined over the entire wheel, there is a torque around the gimbal axis when some spinning

3480-795: The world's major radio observatories include the Very Large Array in New Mexico , United States, Jodrell Bank in the UK , Arecibo in Puerto Rico , Parkes in New South Wales , Australia, and Chajnantor in Chile . A related discipline is Very-long-baseline interferometry (VLBI). Since the mid-20th century, a number of astronomical observatories have been constructed at very high altitudes , above 4,000–5,000 m (13,000–16,000 ft). The largest and most notable of these

3540-483: Was able to be serviced by the Space Shuttles while many other space telescopes cannot be serviced at all. Airborne observatories have the advantage of height over ground installations, putting them above most of the Earth's atmosphere. They also have an advantage over space telescopes: The instruments can be deployed, repaired and updated much more quickly and inexpensively. The Kuiper Airborne Observatory and

3600-489: Was first used for photographing the Sun during the Transit of Venus on December 6, 1882. The observatory also possessed a 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

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