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The Science of Astronomy

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Presentation on theme: "The Science of Astronomy"— Presentation transcript:

1 The Science of Astronomy
Astronomy – understanding what happens in the sky Astrophysics – understanding what happens in space

2 The Lovely Sky

3 The Southern View

4 Using the Belt Stars

5 One of the Course Themes: What you see depends on how you look.

6 88 Official Constellations

7 Sky Maps: Constellations mark patches of the sky and tell stories.

8 Constellations tell stories

9 Constellations of the North and South

10 Panoramic View of the MW

11 Galactic Coordinates: A different perspective

12 Sky Coordinates Horizon Coordinates:
Horizon - the "sky line", i.e. where the sky apparently meets the land Azimuth (Az) - angular coordinate measure around the horizon, starting from the North point and moving Eastward Altitude (Alt) - angular measure above the horizon along a great circle passing through the zenith North Point - the point that is on the horizon and directly North Zenith - the point directly above Nadir - the point directly below Meridian - the great circle that passes from the North point through the zenith to the South Point

13 Perspective: The Horizon Horizon is where “the sky meets the ground”

14 Azimuth and Altitude in the Horizon system

15 Perspective: Star Trails star trails are an effect of Earth’s rotation

16

17 Share Question In order to see the greatest number of stars possible throughout the period of one year, a person should be located at latitude a) 90 degrees b) 45 degrees c) 0 degrees d) anywhere, since latitude makes no difference.

18 Sky Coordinates Celestial Coordinates:
Right Ascension (RA) - similar to Earth longitude but for the sky; RA is measured Eastward starting from the Vernal Equinox Declination (Dec) - similar to Earth latitude but for the sky; Dec is positive in the North Celestial Sphere and negative in the South Celestial Poles - projection of North and South Poles onto the sky Celestial Equator (CE) - projection of equator onto the sky Ecliptic - apparent path of the Sun over the course of one year

19 Longitude

20 Latitude

21 Celestial Sphere: A projection of latitude and longitude onto the sky.

22 The Celestial Sphere is a directional system for a “sky globe”

23 Diurnal Motion diurnal motion refers to motions that repeat daily

24 Share Question The celestial equator is
a) the path of the Sun in the sky. b) the path of the Moon in the sky. c) always directly overhead at the Earth's equator. d) always along the horizon for people on Earth's equator.

25 Perspective: The ecliptic is Earth’s orbital plane around the Sun.

26 Perspective: The Zodiac constellations are seasonal owing to annual motion

27 Earth’s Orbit is NOT a Circle
The orbit of the Earth around the Sun is slightly elliptical and not perfectly circular. Perihelion – closest Aphelion – furthest However, the change in distance does NOT account for our seasons!

28 Seasons and the Sky Vernal Equinox - first day of spring; the Sun lies exactly over the equator and is passing into the N. hemisphere Autumnal Equinox - first day of autumn; the Sun lies exactly over the equator and is passing into the S. hemisphere Summer Solstice - first day of summer; the Sun is highest in the sky for N. observers (lowest for S. observers) Winter Solstice - first day of winter; the Sun is lowest in the sky for N. observers (highest for S. observers)

29 Perspective: The Analemma
Illustrates how the sun is at different altitudes in the sky throughout the year

30 Earth’s Tilt The Earth’s equator and the ecliptic are not in the same plane. The tilt of the Earth’s axis (or the inclination between these two planes) is about 23.5 degrees. It is this tilt that causes us to have annual seasons.

31 The Cause of Seasons The climate on Earth depends on latitude. This is because the Earth is round. By contrast if the Earth were flat, all places would have the same climate. Sunlight is absorbed by the curved Earth A bundle of light falls obliquely across land at the poles; the same light (and energy) falls more directly on land at the equator. Whether Earth is tilted toward or away from the Sun affects how a bundle of light is concentrated on land at a given latitude over the course of a year.

32 Planetary Configurations
Inferior Planets – Mercury, Venus Superior Planets – Mars, Jupiter, Saturn, Uranus, Neptune

33 Synodic Period Sidereal period is how often something repeats with respect to distant stars. Synodic is repetition with respect to something besides a star.

34 Ancient Astronomy Mesopotamia – (~6000 yrs ago) first to keep long term astronomical records; introduced zodiac and 360 degrees in a circle Babylonia – (~500 BC) determined synodic periods of planets Egypt – little known (influence on Greeks?) China – long timeline of records (eclipses, other events) Mesoamerica – complex calendars (e.g., Aztecs and Mayans) Greeks - Moved astronomy from a level of prediction to one of explanation (or attempts to do so)

35 Ancient Astronomical Tools
Aztec Mayan Chinese Stonehenge

36

37 The Cosmos of Pythagoras
(~540 BC) quasi-scientific models for the Solar System; bodies are spheres and move on circular paths (including the Earth!)

38 The Universe of Aristotle
For the ancients, circles and uniform motion were paramount. Such a priori emphasis represents a bias (a presumption without demonstration, proof, or evidence).

39 Cosmology of Dante’s Divine Comedy
An illustration of an Earth-centered view (or model) of the universe. The view was championed by Aristotle and held sway for centuries. Note the continued prominence of circles and spheres,

40 Aristotle: Shape of the Earth
(~350 BC) Supported the idea that Earth is a sphere with “proofs”: Falling objects move toward Earth’s center Shadow of Earth against Moon is always circular Some stars can be seen in certain places, but not in others

41 Interlude: Review of Angular Measure

42 Arc Length, and the key rule of Angular Size
Physical Size = Angular Size X Distance Special Case: circumference of a circle is Radians!

43 Eratothenes: Earth Circumference
An application of geometry in conjunction with a measurement to infer the size of our planet. Note the use of “controls” in the experiment, namely the timing (implying also a fixed longitude).

44 Aristarchus (~270 BC) Applied geometry to astronomical considerations:
Size of Moon relative to Earth Distance of Moon Distance of Sun relative to Moon Size of Sun Earth rotates about an axis Earth revolves about the Sun

45 Aristarchus and the Size of the Moon

46 Aristarchus and the Distance to the Sun

47 Objections to Aristarchus
Greeks disregarded ideas of Earth rotation and revolution for “reasonable” reasons: no “rushing” winds stones fall straight down there is no parallax or change in brightness of the stars over a year

48 Hipparchus and Precession of the Earth’s Rotation Axis
(~130 BC) discovered the precession of the Earth’s rotation axis with a period of 26,000 years

49 Ptolemy’s Geocentric Model
(~140 AD) Summarized and extended a detailed geocentric model for the motions of celestial objects (description published in the Almagest)


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