Astrofysik, VT2007 5A1440. Freedman & Kaufmann, Universe, 7th ed (Freeman & Co, New York)

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Presentation transcript:

Astrofysik, VT2007 5A1440

Freedman & Kaufmann, Universe, 7th ed (Freeman & Co, New York)

Anglular sizes

Astronomers use angles to denote the positions and apparent sizes of objects in the sky The basic unit of angular measure is the degree (°). Astronomers use angular measure to describe the apparent size of a celestial object—what fraction of the sky that object seems to cover The angular diameter (or angular size) of the Moon is ½° or the Moon subtends an angle of ½°.

If you draw lines from your eye to each of two stars, the angle between these lines is the angular distance between these two stars

The adult human hand held at arm’s length provides a means of estimating angles

Angular Measurements Subdivide one degree into 60 arcminutes –minutes of arc –abbreviated as 60 arcmin or 60´ Subdivide one arcminute into 60 arcseconds –seconds of arc –abbreviated as 60 arcsec or 60” 1° = 60 arcmin = 60´ 1´ = 60 arcsec = 60”

The Small Angle Formula D = linear size of object a = angular size of object (in arcsec) d = distance to the object

Small Angle Formula Example On July 26, 2003, Jupiter was 943 million kilometers from Earth and had an angular diameter of 31.2”. Using the small-angle formula, determine Jupiter’s actual diameter.

Distances

Powers-of-ten notation is a useful shorthand system for writing numbers

Astronomical distances are often measured in astronomical units, parsecs, or light-years Astronomical Unit (AU) –One AU is the average distance between Earth and the Sun –1.496 X 10 8 km Light Year (ly) –One ly is the distance light can travel in one year at a speed of 3 x 10 5 km/s –9.46 X km or 63,240 AU Parsec (pc) –the distance at which 1 AU subtends an angle of 1 arcsec or the distance from which Earth would appear to be one arcsecond from the Sun –1 pc = 3.09 × km = 3.26 ly

Naked-eye astronomy had an important place in ancient civilizations Positional astronomy –the study of the positions of objects in the sky and how these positions change Naked-eye astronomy Extends far back in time –British Isles Stonehenge –Native American Medicine Wheel –Aztec, Mayan and Incan temples –Egyptian pyramids

Mayan observatory in the Yukatan (A.D. 1000)

Eighty-eight constellations cover the entire sky Ancient peoples looked at the stars and imagined groupings made pictures in the sky We still refer to many of these groupings Astronomers call them constellations (from the Latin for “group of stars”)

Modern Constellations On modern star charts, the entire sky is divided into 88 regions Each is a constellation Most stars in a constellation are nowhere near one another They only appear to be close together because they are in nearly the same direction as seen from Earth

Annual Motion The stars also appear to slowly shift in position throughout the year This is due to the orbit of the earth around the sun If you follow a particular star on successive evenings, you will find that it rises approximately 4 minutes earlier each night, or 2 hours earlier each month

Winter triangle

Coordinate Systems

It is convenient to imagine that the stars are located on a celestial sphere The celestial sphere is an imaginary object that has no basis in physical reality However it is still a model that remains a useful tool of positional astronomy Landmarks on the celestial sphere are projections of those on the Earth

At any time, an observer can see only half of the celestial sphere The other half is below the horizon, hidden by the body of the Earth Circumpolar stars

Celestial equator divides the sky into northern and southern hemispheres Celestial poles are where the Earth’s axis of rotation would intersect the celestial sphere Polaris is less than 1° away from the north celestial pole, which is why it is called the North Star or the Pole Star. Point in the sky directly overhead an observer anywhere on Earth is called that observer’s zenith.

The Sun appears to trace out a circular path called the ecliptic on the celestial sphere tilted at 23 ½ degrees to the equator The ecliptic and the celestial equator intersect at only two points Each point is called an equinox The point on the ecliptic farthest north of the celestial equator that marks the location of the Sun at the beginning of summer in the northern hemisphere is called the summer solstice At the beginning of the northern hemisphere’s winter the Sun is farthest south of the celestial equator at a point called the winter solstice June 21 March 31 Dec 21 Sept 21

Rektascension deklination vårdagsjämningspunkten

The Moon helps to cause precession, a slow, conical motion of Earth’s axis of rotation

Precession causes the gradual change of the star that marks the North Celestial Pole

FIN

The Nature of Light

Light is electromagnetic radiation and is characterized by its wavelength ( )

The Nature of Light In the 1860s, the Scottish mathematician and physicist James Clerk Maxwell succeeded in describing all the basic properties of electricity and magnetism in four equations This mathematical achievement demonstrated that electric and magnetic forces are really two aspects of the same phenomenon, which we now call electromagnetism

Photons Planck’s law relates the energy of a photon to its frequency or wavelength E = energy of a photon h = Planck’s constant c = speed of light = wavelength of light The value of the constant h in this equation, called Planck’s constant, has been shown in laboratory experiments to be h = x 10 –34 J s

Because of its electric and magnetic properties, light is also called electromagnetic radiation Visible light falls in the 400 to 700 nm range Stars, galaxies and other objects emit light in all wavelengths

An opaque object emits electromagnetic radiation according to its temperature

Wien’s law and the Stefan-Boltzmann law are useful tools for analyzing glowing objects like stars A blackbody is a hypothetical object that is a perfect absorber of electromagnetic radiation at all wavelengths Stars closely approximate the behavior of blackbodies, as do other hot, dense objects The intensities of radiation emitted at various wavelengths by a blackbody at a given temperature are shown by a blackbody curve

Wien’s Law Wien’s law states that the dominant wavelength at which a blackbody emits electromagnetic radiation is inversely proportional to the Kelvin temperature of the object

Stefan-Boltzmann Law The Stefan-Boltzmann law states that a blackbody radiates electromagnetic waves with a total energy flux F directly proportional to the fourth power of the Kelvin temperature T of the object: F =  T 4

FIN