Philips Atlas of the Universe

(Marvins-Underground-K-12) #1
Reflector: A telescope in which the light is collected
by means of a mirror.

Refraction: The change in direction of a ray of light
when passing from one transparent substance into
another.

Refractor: A telescope which collects its light by
means of a lens. The light passes through this lens
(object-glass)and is brought to focus; the image
is then magnified by an eyepiece.

Resolving power: The ability of a telescope to
separate objects which are close together; the larger
the telescope the greater its resolving power. Radio
telescopes (see radio astronomy)have poor
resolving power compared with optical telescopes.

Retardation: The difference in the time of moonrise
between one night and the next. It may exceed one
hour, or it may be as little as a quarter of an hour.

Retrograde motion: In the Solar System, movement
in a sense opposite to that of the Earth in its orbit;
some comets, notably Halley’s, have retrograde
motion. The term is also used with regard to the
apparent movements of planets in the sky; when
the apparent motion is from east to west, relative
to the fixed stars, the direction is retrograde. The
term may be applied to the rotations of planets. Since
Uranus has an axial inclination of more than a right
angle, its rotation is technically retrograde; Venus
also has retrograde axial rotation.

Reversing layer: The gaseous layer above the bright
surface or photosphere of the Sun. Shining on its
own, the gases would yield bright spectral lines; but
as the photosphere makes up the background, the
lines are reversed, and appear as dark absorption or
Fraunhofer lines. Strictly speaking, the whole of the
Sun’s chromosphere is a reversing layer.

Right ascension: The right ascension of a celestial
body is the time which elapses between the
culmination of the First Point of Ariesand the
culmination of the body concerned. For example,
Aldebaran in Taurus culminates 4h 33m after the
First Point of Aries has done so; therefore the right
ascension of Aldebaran is 4h 33m. The right ascensions
of bodies in theSolar System change quickly.
However, the right ascensions of stars do not change,
apart from the slow cumulative effect of precession.

Roche limit: The distance from the centre of a planet,
or other body, within which a second body would be
broken up by gravitational distortion. This applies only
to an orbiting body which has no appreciable structural
cohesion, so that strong, solid objects, such as artificial
satellites, may move safely well within the Roche limit
for the Earth. The Roche limit lies at 2.44 times the
radius of the planet from the centre of the globe, so
that for the Earth it is about 9170 kilometres above
ground-level. Saturn’s ring system lies within the
Roche limit for Saturn.

RR Lyrae variables: Regular variable stars whose
periods are very short (between about 1^1 / 4 hours and
about 30 hours). They seem to be fairly uniform in

luminosity; each is around 100 times as luminous
as the Sun. They can therefore be used for distance
measures, in the same way as Cepheids. Many of
them are found in star clusters, and they were formerly
known as cluster-Cepheids. No RR Lyrae variable
appears bright enough to be seen with the naked eye.

S
Saros:A period of 18 years 11.3 days, after which
the Earth, Moon and Sun return to almost the same
relative positions. Therefore, an eclipse of the Sun
or Moon is liable to be followed by a similar eclipse
18 years 11.3 days later. The period is not exact, but
is good enough for predictions to be made – as was
done in ancient times by Greek philosophers.

Satellite:A secondary body orbiting a primary. The
Earth has one satellite (the Moon); Jupiter has 53,
Saturn 30, Uranus 23, Neptune 11 and Pluto one,
while Mercury and Venus are unattended.

Schmidt telescope (or Schmidt camera): A type
of telescope which uses a spherical mirror and a
special glass correcting plate. With it, relatively wide
areas of the sky may be photographed with a single
exposure; definition is good all over the plate. In its
original form, the Schmidt telescope can be used only
photographically. The largest Schmidt in use is the
122-centimetre instrument at Palomar.

Scintillation: Twinkling of stars. It is due entirely
to the effects of the Earth’s atmosphere; a star will
scintillate most violently when it is low over the
horizon, so that its light is passing through a thick layer
of atmosphere. A planet, which shows up as a small
disk rather than a point, will generally twinkle much
less than a star.

Seasons: Effects on the climate due to the inclination
of the Earth’s axis. The fact that the Earth’s distance
from the Sun is not constant has only a minor effect
upon our seasons.

Second of arc:One 360th of a degree. See arc
minute, arc second.

Secular acceleration: Because of friction produced
by the tides, the Earth’s rotation is gradually slowing
down; the ‘day’ is becoming longer. The average daily
lengthening is only 0.00000002 seconds, but over a
sufficiently long period the effect becomes detectable.
The lengthening of terrestrial time periods gives
rise to an apparent speeding-up of the periods of the
Sun, Moon and planets. Another result of these tidal
phenomena is that the Moon is receding from the
Earth slowly.

Seeing: The quality of the steadiness and clarity
of a star’s image. It depends upon conditions in the
Earth’s atmosphere. From the Moon, or from space,
the ‘seeing’ is always perfect.

Seismometer:An earthquake recorder. Very sensitive
seismometers were taken to the Moon by the Apollo
astronauts, and provided interesting information about
seismic conditions there.

Selenography: The study of the Moon’s surface.

Sextant:An instrument used for measuring the
altitude of a celestial body above the horizon.

Seyfert galaxies: Galaxies with small, bright nuclei.
Many of them are radio sources, and show evidence
of violent disturbances in their nuclei.

Shooting-star:The luminous appearance caused by
a meteor falling through the Earth’s atmosphere.

Sidereal period:The time taken for a planet or other
body to make one journey around the Sun (365.2 days
in the case of the Earth). The term is also used for
a satellite in orbit around a planet. Also known as
periodic time.

Sidereal time:The local time reckoned according
to the apparent rotation of the celestial sphere. It is
zero hours when the First Point of Aries crosses the
observer’s meridian. The sidereal time for any observer
is equal to the right ascension of an object which lies
on the meridian at that time. Greenwich sidereal time
is used as the world standard (this is, of course, merely
the local sidereal time at Greenwich Observatory).

Solar apex:The point on the celestial sphere towards
which the Sun is apparently travelling. It lies in the
constellation Hercules; the Sun’s velocity towards the
apex is 19 kilometres per second. The point directly
opposite in the sky to the solar apex is termed the
solar antapex. This motion is distinct from the Sun’s
rotation around the centre of the Galaxy, which
amounts to about 320 kilometres per second.

Solar constant:The unit for measuring the amount
of energy received on the Earth’s surface by solar
radiation. It is equal to 1.94 calories per minute per
square centimetre. (A calorie is the amount of heat
needed to raise the temperature of 1 gram of water
by 1 degree C.)

Solar flares:See flares, solar.

Solar parallax: The trigonometrical parallax of the
Sun. It is equal to 8.79 seconds of arc.

Solar System: The system made up of the Sun, the
planets, satellites, comets, asteroids, meteoroids and
interplanetary dust and gas.

Solar time, apparent: The local time reckoned
according to the Sun. Noon occurs when the Sun
crosses the observer’s meridian, and is therefore
at its highest in the sky.

Solar wind: A steady flow of atomic particles
streaming out from the Sun in all directions. It was
detected by means of space probes, many of which
carry instruments to study it. Its velocity in the
neighbourhood of the Earth exceeds 965 kilometres
per second. The intensity of solar wind is enhanced
during solar storms.

Solstices:Times when the Sun is at its northernmost
point in the sky (declination 23^1 / 2 °N, around 22 June),
or at its southernmost point (23^1 / 2 °S, around 22
December). The dates of the solstices vary somewhat,
because of the calendar irregularities due to leap years.

GLOSSARY


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