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ASTRO 101

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Title: ASTRO 101


1
ASTRO 101
  • Principles of Astronomy

2
Instructor Jerome A. Orosz
(rhymes with boris)Contact
  • Telephone 594-7118
  • E-mail orosz_at_sciences.sdsu.edu
  • WWW http//mintaka.sdsu.edu/faculty/orosz/web/
  • Office Physics 241, hours T TH 330-500

3
Text Perspectives on Astronomy First
Editionby Michael A. Seeds Dana Milbank.
4
Astronomy Help Room Hours
  • Monday 1200-1300, 1700-1800
  • Tuesday 1700-1800
  • Wednesday 1200-1400, 1700-1800
  • Thursday 1400-1800, 1700-1800
  • Friday 900-1000, 1200-1400
  • Help room is located in PA 215

5
  • Office hours cancelled for October 8 and October
    13

6
Exam 1
  • N48
  • Average 57.2
  • Maximum 91
  • Minimum 24
  • std. dev. 15.6
  • The average corresponds to roughly a C- using the
    guidelines in the syllabus.

7
Coming Up
  • Chapter 5 The Sun
  • Chapter 6 The family of stars
  • Homework due October 15 Question 7, Chapter 6
    (Why does the luminosity of a star depend on both
    its radius and temperature?)

8
Questions for Today
  • How hot is the Sun?
  • How do you take the temperature of a star?

9
The Sun and the Stars
  • In ancient times, there were certain categories
    of objects in the sky
  • The Earth.
  • The Moon.
  • The five planets.
  • The Sun.
  • The fixed stars.

10
The Sun and the Stars
  • In ancient times, there were certain categories
    of objects in the sky
  • The Earth.
  • The Moon.
  • The five planets.
  • The Sun.
  • The fixed stars.

Since the time of Copernicus, we have known these
are the same kinds of objects.
11
The Sun and the Stars
  • In ancient times, there were certain categories
    of objects in the sky
  • The Earth.
  • The Moon.
  • The five planets.
  • The Sun.
  • The fixed stars.

Since the time of Copernicus, we have known these
are the same kinds of objects.
Since the late 1800s, spectroscopy has shown that
the Sun is simply the nearest star.
12
The Sun and the Stars
  • The Sun is the nearest example of a star.
  • Because it is so near, it is the only star whose
    surface we can study in any detail. The other
    stars are so far away that their apparent
    angular diameter is much too tiny to resolve
    with even the largest telescopes.

13
The Angular Size of a Star
  • Because of the huge distances, the angular sizes
    of most stars are about 1000 times or more
    smaller than what you can resolve with even the
    biggest telescopes. (In some cases, the angular
    diameters can be measured using a technique
    called interferometry, but this method does not
    yield an image.)

14
The Sun and the Stars
  • The Sun is the nearest example of a star.
  • Basic questions to ask

15
The Sun and the Stars
  • The Sun is the nearest example of a star.
  • Basic questions to ask
  • What do stars look like on their surfaces? Look
    at the Sun since it is so close.
  • How do stars work on their insides? Look at both
    the Sun and the stars to get many examples.
  • What will happen to the Sun? Look at other stars
    that are in other stages of development.

16
The Sun
  • There are two broad areas of solar research
  • The study of the overall structure of the Sun.
  • The study of its detailed surface features.
  • Think of the distinction of climate and
    weather on Earth
  • Climate refers to global trends.
  • Weather refers to local conditions.

17
The Surface of the Sun
  • The surface of the Sun can be complex.
  • Surprisingly, observing the Sun can be quite
    difficult, owing to the immense heat.
  • The study of the solar surface is usually done
    using many different wavelengths, from the X-rays
    to radio. Different features show up well in
    certain wavelengths.

18
The Solar Surface
  • The Sun has no solid surface. The part we see is
    called the photosphere.
  • A visual light image captures different features
    than an ultraviolet light image.

19
The Solar Surface
  • The Sun has no solid surface. The part we see is
    called the photosphere.
  • High resolution images of the photosphere show
    granulation.

20
Granulation
  • From the measurement of Doppler shifts, we know
    that the granules are blobs of gas that are
    rising and falling.
  • The granules are similar to what one sees in
    boiling water on Earth.
  • Energy from the interior is being transported
    outwards by motions in the gas. This type of
    energy transport is called convection.

21
Solar Oscillations
  • By detailed analysis of the Doppler shifts of
    different parts of the photosphere, we know that
    the photosphere oscillates (i.e. it vibrates much
    like a bell).

22
Solar Oscillations
  • By detailed analysis of the Doppler shifts of
    different parts of the photosphere, we know that
    the photosphere oscillates (i.e. it vibrates much
    like a bell).
  • These vibrations are somewhat similar to sound
    waves in the air on Earth.

23
Solar Oscillations
  • By detailed analysis of the Doppler shifts of
    different parts of the photosphere, we know that
    the photosphere oscillates (i.e. it vibrates much
    like a bell).
  • These vibrations are somewhat similar to sound
    waves in the air on Earth.
  • Since the speed of sound in a gas depends on the
    temperature and density of the gas, the study of
    solar oscillations can reveal details about the
    solar interior.

24
Sunspots
  • Sunspots are darker regions on the Suns surface.
  • They can be observed in the optical, and were
    first discovered by Galileo in 1610.

25
Sunspots
  • Note the complex structure in the spot and its
    surroundings.

26
The Solar Cycle
  • In the mid 1800s, a Swiss astronomer made
    detailed observations of sunspots in order to
    search for transits of a possible planet interior
    to Mercury.

27
The Solar Cycle
  • No planets were found, but it was discovered that
    the number of sunspots varies with an 11 year
    cycle.
  • This is not fully understood.

28
Sunspots
  • Galileo used sunspots to track the rotation of
    the Suns surface

29
Sunspots
  • Galileo was the first to sunspots to track the
    rotation of the Suns surface.

30
Sunspots
  • Galileo was the first to sunspots to track the
    rotation of the Suns surface.
  • The Sun does not rotate as a solid body. The
    equator rotates once every 25 days. At 45o
    latitude, it takes 27.8 days.

31
The Sun and Space Weather
  • Violent activity can occur in regions near
    sunspots.
  • A solar flare is a giant eruption of particles
    and radiation.
  • The radiation and particles can interact with the
    Earths upper atmosphere, disrupting satellite
    communications and power grids.

32
The Sun and Space Weather
  • Violent activity can occur in regions near
    sunspots.
  • A solar flare is a giant eruption of particles
    and radiation.
  • The cause of these giant flares is not
    understood, although magnetic fields are thought
    to play a role.

33
Next
  • Other Stars

34
Stellar Properties
  • The Sun and the stars are similar objects.
  • In order to understand them, we want to try and
    measure as many properties about them as we can
  • Temperature at the surface
  • Power output (luminosity)
  • Radius
  • Mass
  • Chemical composition

35
Observing Other Stars
  • Recall there is basically no hope of spatially
    resolving the disk of any star (apart from the
    Sun). The stars are very far away, so their
    angular size as seen from Earth is extremely
    small.

36
Observing Other Stars
  • Recall there is basically no hope of spatially
    resolving the disk of any star (apart from the
    Sun). The stars are very far away, so their
    angular size as seen from Earth is extremely
    small.
  • Recently using interferometry, it has been
    possible to measure the angular diameters of the
    nearest stars. This is not really the same as
    imaging their surfaces.

37
Observing Other Stars
  • Recall there is basically no hope of spatially
    resolving the disk of any star (apart from the
    Sun). The stars are very far away, so their
    angular size as seen from Earth is extremely
    small.
  • The light we receive from a star comes from the
    entire hemisphere that is facing us.

38
Observing Other Stars
  • Recall there is basically no hope of spatially
    resolving the disk of any star (apart from the
    Sun). The stars are very far away, so their
    angular size as seen from Earth is extremely
    small.
  • The light we receive from a star comes from the
    entire hemisphere that is facing us. That is, we
    see the disk-integrated light.

39
Measuring Photons
  • There are 4 fundamental properties one can
    measure for a photon
  • Its energy/wavelength/frequency.
  • Its direction.
  • Its time of arrival.
  • Its polarization, which a measure of the
    direction of the electric and magnetic fields.
  • The first three properties are the most commonly
    measured ones in astronomy.

40
Measuring Photons
  • Recall the 4 fundamental properties one can
    measure for a photon
  • Its energy/wavelength/frequency.
  • Depending on the detection system, there is a
    limit to the spectral resolution, which is the
    ability to tell one wavelength from another. At
    some point, the energy difference between two
    photons becomes too small to measure with your
    device.

41
Observing Other Stars
  • To get an understanding of how a star works, the
    most useful thing to do is to measure the
    spectral energy distribution, which is a plot of
    the intensity of the photons vs. their
    wavelengths (or frequencies or energies).

42
Observing Other Stars
  • To get an understanding of how a star works, the
    most useful thing to do is to measure the
    spectral energy distribution, which is a plot of
    the intensity of the photons vs. their
    wavelengths (or frequencies or energies).
  • There are two ways to do this
  • Broad band, by taking images with a camera and
    a colored filter.

43
Observing Other Stars
  • To get an understanding of how a star works, the
    most useful thing to do is to measure the
    spectral energy distribution, which is a plot of
    the intensity of the photons vs. their
    wavelengths (or frequencies or energies).
  • There are two ways to do this
  • Broad band, by taking images with a camera and
    a colored filter.
  • High resolution, by using special optics to
    disperse the light and record it.

44
Broad Band Photometry
  • There are several standard filters in use in
    astronomy.
  • The filter lets only light within a certain
    wavelength region through (that is why they have
    those particular colors).

45
Color Photography
  • The separate images are digitally processed to
    obtain the final color image.

46
Color Photography
47
Color Photography
48
Broad Band Photometry
  • Broad band photometry has the advantage in that
    it is easy (just need a camera and some filters
    on the back of your telescope), and it is
    efficient (relatively few photons are lost in the
    optics).

49
Broad Band Photometry
  • Broad band photometry has the advantage in that
    it is easy (just need a camera and some filters
    on the back of your telescope), and it is
    efficient (relatively few photons are lost in the
    optics).
  • The disadvantage is that the spectral resolution
    is poor, so subtle differences in photon energies
    are impossible to detect.

50
Broad Band Photometry
  • Despite the disadvantages, broad band photometry
    is useful.
  • For example, it is immediately evident that
    different stars have different colors (the
    image on the left is a composite of three images
    taken in different filters.

51
Magnitudes
  • Historically (e.g. Hipparcos in the First
    Century), the brightness of stars as seen by the
    eye have been measured on a magnitude scale
  • The brightest stars were first magnitude.
  • The faintest stars were sixth magnitude.
  • Brighter objects have smaller magnitudes.

52
Magnitudes
  • In modern times, it was discovered that the human
    eye has a nonlinear response to light if one
    source of light has twice the photons as a second
    source, then the first source would not appear by
    eye to be twice as bright.
  • The response of the eye is logarithmic, so that
    differences of magnitudes correspond to ratios of
    flux.

53
The Magnitude Scale
  • The modern of the magnitude scale is set up so
    that a difference of 5 magnitudes corresponds to
    a ratio of brightnesses of 100.
  • Bright objects can have negative apparent
    magnitudes.

54
High Resolution Spectroscopy
  • To obtain a high resolution spectrum, light from
    a star is passed through a prism (or reflected
    off a grating), and focused and detected using
    some complicated optics.

55
High Resolution Spectroscopy
  • Using a good high resolution spectrum, you can
    get a much better measurement of the spectral
    energy distribution.

56
High Resolution Spectroscopy
  • Using a good high resolution spectrum, you can
    get a much better measurement of the spectral
    energy distribution.
  • The disadvantage is that the efficiency is lower
    (more photons are lost in the complex optics).
    Also, it is difficult to measure more than one
    star at a time (in contrast to the direct imaging
    where several stars can be on the same image).

57
Stellar Properties
  • The Sun and the stars are similar objects.
  • In order to understand them, we want to try and
    measure as many properties about them as we can
  • Temperature at the surface
  • Power output (luminosity)
  • Radius
  • Mass
  • Chemical composition

58
Spectral Classification
  • In the early 1800s, Joseph Fraunhofer observed
    the solar spectrum. He saw dark regions, known
    as spectral lines (these tell us what elements
    are there).

59
Spectral Classification
  • In the early 1800s, Joseph Fraunhofer observed
    the solar spectrum. He saw dark regions, known
    as spectral lines (these tell us what elements
    are there).
  • Starting in the late 1800s, it became possible to
    take the spectra of stars with similar detail.

60
Spectral Classification
  • By the early 1900s, astronomers at Harvard
    College Observatory had collected the spectra of
    hundreds of thousands of stars (one at a time!).

61
Spectral Classification
  • By the early 1900s, astronomers at Harvard
    College Observatory had collected the spectra of
    hundreds of thousands of stars (one at a time!).
  • What does one do with them?

62
Spectral Classification
  • By the early 1900s, astronomers at Harvard
    College Observatory had collected the spectra of
    hundreds of thousands of stars (one at a time!).
  • What does one do with them? You classify them,
    based on certain characteristics, and hope you
    can make sense out of all of them.

63
Spectral Classification
  • By the early 1900s, astronomers at Harvard
    College Observatory had collected the spectra of
    hundreds of thousands of stars (one at a time!).
  • What does one do with them? You classify them,
    based on certain characteristics, and hope you
    can make sense out of all of them.
  • Most of the early classification work was done by
    women (since they were paid less than men there
    could be more of them on the staff).

64
Spectral Classification
  • At first, there was no physical understanding.
  • The earliest classification scheme was based on
    the strength of the hydrogen lines, with classes
    of A, B, C, D, E, F, G, H, I, J, K, L, M, N, O.
  • Class A had the strongest hydrogen lines, class O
    the weakest.

65
Spectral Classification
  • At first, there was no physical understanding.
  • The earliest classification scheme was based on
    the strength of the hydrogen lines, with classes
    of A, B, C, D, E, F, G, H, I, J, K, L, M, N, O.
  • Class A had the strongest hydrogen lines, class O
    the weakest.
  • Later on, only a few of these classes were kept.

66
Spectral Classification
  • At first, there was no physical understanding.
  • The earliest classification scheme was based on
    the strength of the hydrogen lines, with classes
    of A, B, C, D, E, F, G, H, I, J, K, L, M, N, O.
  • Class A had the strongest hydrogen lines, class O
    the weakest.
  • Later on, only a few of these classes were kept.
    Then, subclasses were added (e.g. G2), based on
    other elements.

67
Spectral Classification
  • At first, there was no physical understanding.
  • The earliest classification scheme was based on
    the strength of the hydrogen lines, with classes
    of A, B, F, G, K, M, O.
  • Eventually, physical understanding came. It was
    discovered that the spectral type was a
    temperature indicator. As a result, a more
    natural ordering of the spectral types became O,
    B, A, F, G, K, M (the old classes were retained).

68
Spectral Classification
  • Here are digital plots of representative stars in
    the spectral sequence.
  • Note the variation in the strength of the
    hydrogen lines.

69
Spectral Classification
  • This is a computer simulation of the different
    types.

70
Spectral Classification
  • Why do the spectral classes look different from
    one another?
  • The temperature. The electrons in the atoms are
    responsible for the spectral lines, and the
    energies of the electrons are change with
    changing temperature. Example an O-star is so
    hot that the hydrogen atoms have lost their
    electrons, so no lines of hydrogen are seen.

71
Spectral Classification
  • http//www.astronomynotes.com

72
Spectral Classification
  • This is a computer simulation of the different
    types.

73
Spectral Classification
  • A measurement of the spectral type gives the
    surface temperature of the star.

74
Spectral Classification
  • A measurement of the spectral type gives the
    surface temperature of the star.
  • O-stars are the hottest, with surface
    temperatures of up to 60,000 K.
  • M-stars are the coolest, with temperatures of
    only 3000 K.
  • The temperature of the Sun (a G2 star) is 5770 K.

75
Stellar Properties
  • The Sun and the stars are similar objects.
  • In order to understand them, we want to try and
    measure as many properties about them as we can
  • Temperature at the surface Use the spectral
    type
  • Power output (luminosity)
  • Radius
  • Mass
  • Chemical composition

76
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