Sept. 9th/11th - The paths of stars; diurnal cycle Flashcards

1
Q

How do we locate objects on the celestial sphere?

A

Celestial coordinates: describe the precise position of a star on the celestial sphere, similar to how we use longitude + latitude to locate a city on earth

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2
Q

2 celestial coordinates:

A
  • Declination
  • Right Ascension
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3
Q

Declination (2 celestial coordinates)

A
  • Similar to latitude:
  • Similar to how latitude is parallel to Earth’s equator, lines of declination are parallel to the celestial equator
  • Earth’s equator has lat = 0 deg, celestial equator has dec. 0 deg
  • Latitude is labelled east or west relative to the equator??????, while declination is labelled positive or negative
    - EX: North pole = 0 deg. N, North Celestial Pole has dec. = +90 deg.
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4
Q

Right Ascension (2 celestial coordinates)

A
  • Similar to longitude:
  • Both span vertically, north to south
  • As there is no starting point for longitude, there is no starting point for right ascension
    - By international treaty, longitude 0 (prime meridian) runs through Greenwich, and by convention, right ascension 0 is the line of right ascension that runs through the March equinox
  • Longitude is measured in degrees east or west of Greenwich, while right ascension in measured in hours east of the March equinox
    - A full 360° circle around the celestial equator goes through 24 hours of right ascension, so each hour of right ascension represents an angle of 360°÷24=15°
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5
Q

How do we locate stars using declination/right ascension?

A
  • DEC: + = above equator, - = below equator
  • RA: each hour = 15 degrees, units of time = how long after the March equinox the object crosses the meridian
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6
Q

Celestial coordinates aren’t always accurate:

A

Move slowly relative to distant stars because they’re tied to the celestial equator - which moves gradually relative to the constellations; require continuous updating

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7
Q

Celestial Coordinates of the Sun:

A
  • It takes a year for the Sun to make a full circuit of the ecliptic, which means it moves through all 24 hours of right ascension over the course of the year.
  • Unlike stars, which remain essentially fixed in the patterns of the constellations on the celestial sphere, the Sun moves gradually along the ecliptic.
  • The Sun therefore moves approximately one-twelfth of the way around the ecliptic each month, meaning that its right ascension changes by about 24÷12=2 hours per month.
  • While RA advances steadily through the year, the Sun’s declination changes much more slowly around the solstices than around the equinoxes
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8
Q

Equinoxes & Solstices:

A
  • Special moments that occur each year when earth is at particular positions in its orbit
  • Correspond to the locations of the sun along the ecliptic
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9
Q

“Equinox” has a dual meaning:

A

it’s the moment in March when the sun’s path crosses the celestial equator, and the point on the ecliptic at which the sun appears to be located at that moment

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10
Q

How do stars move through local sky?

A

The path of any star through your local sky depends only on

  • (1) your latitude and
  • (2) the declination of the star.
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11
Q

The sky at the north pole - where the daily paths of stars are easiest to understand

A
  • The daily circles of the stars keep them at constant altitudes above or below the North Polar horizon
  • The altitude of any star is equal to its declination
  • As a result, all stars north of the celestial equator are circumpolar at the North Pole, meaning that they never fall below the horizon.
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12
Q

The Sky at the Equator:

A

As the equatorial sky appears to turn, all star paths rise straight out of the eastern horizon and set straight into the western horizon, with the following features:

  • Stars with dec=0° lie on the celestial equator and therefore rise due east, cross the meridian at the zenith, and set due west.
  • Stars with dec>0° rise north of due east, reach their highest point on the meridian in the north, and set north of due west. Their rise, set, and highest point depend on their declination.
  • Stars with dec<0° rise south of due east, reach their highest point on the meridian in the south, and set south of due west. For example, a star with dec=−50° rises 50° south of due east, crosses the meridian 50° to the south of the zenith—that is, at an altitude of 90°−50°=40° in the south—and sets 50° south of due west.
  • Because exactly half of any star’s daily circle lies above the horizon, every star at the equator is above the horizon for exactly half of each sidereal day, or just under 12 hours (and below the horizon for the other half of the sidereal day).
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13
Q

The celestial equator always extends from due east on your horizon to due west on your horizon, crossing the meridian at an altitude of…

A

90° minus your latitude.

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14
Q

How Does The Sun Move Through Local Sky?

A

The Sun’s path on any particular day depends only on its declination and your latitude - because the Sun’s declination changes over the course of the year, the Sun’s path also changes

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15
Q

During Equinoxes - How Does The Sun Move Through Local Sky?

A

the Sun is on the celestial equator (dec=0°) and therefore follows the celestial equator’s path: It rises due east, crosses the meridian at altitude 50° in the south, and sets due west; above the horizon for 12 hours

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16
Q

During June Solstice - How Does The Sun Move Through Local Sky?

A

the Sun rises well north of due east, reaches an altitude of 50°+2312°=7312° when it crosses the meridian in the south, and sets well north of due west.

The daylight hours are long because much more than half the Sun’s path is above the horizon.

17
Q

On December Solstice - - How Does The Sun Move Through Local Sky?

A

the Sun rises well south of due east, reaches an altitude of only 50°−2312°=2612° when it crosses the meridian in the south, and sets well south of due west

The daylight hours are short because much less than half the Sun’s path is above the horizon.

18
Q

At North Poles - How Does The Sun Move Through Local Sky?

A

Because the Sun appears on the celestial equator on the day of the March equinox, the Sun circles the North Polar sky on the horizon on March 21, completing a full circle in 24 hours (1 solar day)

Over the next 3 months, the Sun continues to circle the horizon each day, circling at gradually higher altitudes as its declination increases

It reaches its highest point on the June solstice, when its declination of +2312° means that it circles the North Polar sky at an altitude of 2312° After the June solstice, the daily circles gradually fall lower over the next 3 months, reaching the horizon on the September equinox

Then, because the Sun’s declination is negative for the next 6 months (until the following March equinox), the Sun remains below the North Polar horizon

19
Q

At South Pole - How Does The Sun Move Through Local Sky?

A

The Sun’s daily circle first reaches the horizon on the September equinox. The daily circles then rise gradually higher, reaching a maximum altitude of 2312° on the December solstice (when it is summer in the Antarctic), and then slowly fall back to the horizon on the March equinox

The South Pole has the Sun above the horizon during the 6 months it is below the North Polar horizon.

IMPORTANT NOTE: First, the atmosphere bends light enough so that when the Sun is near the horizon, it appears to be about 1° higher than it really is, which means we can see the Sun even when it is slightly below the horizon. Second, the Sun’s angular size of about 12° means that it does not fall below the horizon at a single moment but instead sets gradually. Together, these effects mean that the Sun appears above each polar horizon for several days longer than 6 months each year.

20
Q

At The Equator - How Does The Sun Move Through Local Sky?

A

The celestial equator extends from the horizon due east, through the zenith, to the horizon due west

The Sun therefore follows this path on each equinox, reaching the zenith at local noon

21
Q

At the Tropics - How Does The Sun Move Through Local Sky?

A

The circles of latitude 23.5°N and 23.5°S are called the tropic of Cancer and the tropic of Capricorn

The region between these two circles, generally called the tropics, represents the parts of Earth where the Sun can sometimes reach the zenith at noon

22
Q

At the Arctic/Antarctic Circles

A

At latitudes progressively farther from the equator, the daily time that the Sun is above the horizon varies progressively more with the seasons

The special latitudes at which the Sun remains continuously above the horizon for a full day each year are the polar circles: - the Arctic Circle at latitude 66.5°N and
- the Antarctic Circle at latitude 66.5°S