1b11 foundations of astronomy astronomical co-ordinates liz puchnarewicz [email protected]

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1B11 Foundations of Astronomy Astronomical co- ordinates Liz Puchnarewicz emp @mssl.ucl.ac. uk www.ucl.ac.uk/webct www.mssl.ucl.ac.uk/

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Page 1: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Foundations of AstronomyAstronomical co-ordinates

Liz [email protected]/webctwww.mssl.ucl.ac.uk/

Page 2: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Positions of astronomical sources

Constellations and star names

The most important parameter you can know about any astronomical source is its position on the sky.

Why?

1. Isolate, identify and re-visit the source

2. Check for transient sources, supernovae etc.

3. Associate sources at different wavelengths

By grouping stars into constellations, our ancestors developed the first system for unambiguously identifying celestial sources. Now, we use co-ordinate systems based on angular distance scales.

Page 3: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Equatorial System

More co-ordinate systems

NCP =90O

Celestial horizon,=0O

SCP =-90O

The Equatorial system is the one most generally

used. It is based on a projection of the Earth’s

equator and poles onto the celestial sphere.

NCP = North Celestial Pole

SCP = South Celestial Pole

-90O < < 90O

0h < < 24h

Page 4: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 RA and Dec

Right Ascension, RA or , is measured in hours and a full circle (360O) = 24 hours. There are 60 minutes of time in one hour, and 60 seconds of time in one minute (h,m,s).

Declination, Dec or , is measured in degrees from –90O at the SCP to +90O at the NCP. There are 60 arcminutes in one degree and 60 arcseconds in one arcminute (O,’,’’).

The zero-point for Dec is on the celestial horizon which is a projection of the Earth’s equator on the sky.

The zero point for RA is defined as the position of the Sun in the sky at the Vernal Equinox (~21 March), the point at which the Sun crosses the equator from South to North. It is also known as the “First Point of Aries” (although it is now in Pisces) and it is measured eastwards.

Page 5: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Astronomical co-ordinates

star

Celestial equator

SCP

NCP

Earth

Celestial sphere

Vernal equinox

East 1” is the angular

diameter of 1p at 4km!

Page 6: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Star maps and catalogues

The positions (RA, Dec) of stars can now be mapped and catalogued.

+10O

0O

-10O

0h1h2h RADec

1h 28m 40s +6O 50’ 10”

Page 7: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Precession

The Earth’s rotation axis precesses in space due to the gravitational pull of the Sun and the Moon.

23.5O

rotation axis

equatorial bulge

Sun

MoonEarth Orbital plane (ecliptic)

Precession (once every 26,000 years). 1.4O westwards per century.

Page 8: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Precession and Nutation

• Precession occurs due to the gravitational pull of the Sun and the Moon (mostly the Moon).

• Over 26,000 years, the positions of the celestial poles and the equinoxes change with respect to the stars.

• Thus it is always necessary to specify a date for equatorial co-ordinates (currently using 2000.0 co-ordinates).

• Nutation is an additional wobble in the position of the Earth’s poles.

• It is mainly due to the precession of the Moon’s orbit, which has a period of 18.6 years.

Page 9: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

NCP

SCP

1B11 Some key points on the observer’s sky

Zenith

observer

meridian

stars

Earth rotates

90-

= latitude

N S

W

E

horizon

star

Page 10: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

NCP

SCP

1B11 Some key points on the observer’s sky

Zenith

meridian

N S

W

E

horizon

star

Stars rise in the East, transit the meridian and

set in the West

celestial equator

hour angle

Page 11: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1 sidereal day

1B11 Time systems

Solar day = time between successive transits of the Sun = 24 hours

Sidereal day = time between successive transits of the Vernal Equinox = 23 hours 56min 04sec

4min extra rotation

Page 12: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Solar vs sidereal

• Sidereal day is about 4mins shorter than the solar day.

• Relative to the (mean) solar time, the stars rise 4mins earlier each night (about 2 hours each month).

• We define 0h Local Sidereal Time (LST) as the time when the Vernal Equinox lies on the observer’s meridian.

LST = Hour angle of the Vernal Equinox

For the Greenwich Meridian:

GST = H. A. of the Vernal Equinox at Greenwich

LST = GST + longitude east of Greenwich

Page 13: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Key relations – LST, RA and HA

key points on the sky

Local Sidereal Time = Right Ascension on the meridian

So, for example, if LST = 11:30, stars with RA=11h30m are on the meridian

HA = LST - RA

ie if a star is on the meridian, RA = LST and HA = 0.

If LST is 11:30, a star with RA = 10h30m has HA = 1h;ie it is one hour past the meridian.

Page 14: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Solar time

Apparent solar time is the time with respect to the Sun in the sky (ie the time told by a sundial).

The apparent solar day is not constant over the year due to:

1. Eccentricity of the Earth’s orbit

2. Inclination of the ecliptic to the equator

Mean solar time: define a point on the Equator (the “mean sun”) which moves eastwards at the average rate of the real Sun, such that the mean solar day is 1/365.2564 of a sidereal year.

(local) mean solar time = HA of mean sun + 12 hours

GMT = HA mean sun at Greenwich + 12 hours

Page 15: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Equation of time

The difference between apparent solar time and mean solar time is called the equation of time and ranges from between –14m15s to +16m15s.

May21 Jan21Nov21Sep21Jul21 Mar21

+15m

+10m

+5m

0m

-5m

-10m

-15m

Page 16: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Universal Time

Universal Time (UT1) = Greenwich Mean Time (GMT)

But UT1 uses the Earth’s rotation as its “clock” so has some irregularities including general slowing of rotation.

International Atomic Time (TAI) uses atomic clocks which are more accurate so a modified version of UT is used,

Co-ordinated Universal Time (UTC)

Zero point for TAI was defined as UT1 on 1958 January 1.

UTC = TAI + an integral number of seconds

and is maintained to be within 0.9s of UT1 using leap seconds.

Page 17: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Topocentric (horizon) co-ordinates

Co-ordinates relative to an observer’s horizon.

Zenith

observer

meridian

N S

W

E

horizon

A

h

A = azimuthh = altitude

Page 18: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Topocentric co-ordinates (cont.)

Altitude = h = angular distance above the horizon.

Zenith distance = ZD = 90 - h

Azimuth = A = angular bearing of an object from the north, measured eastwards.

eg. 0O = due north and 90O = due east

Page 19: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Ecliptic co-ordinates

Useful when studying the movements of the planets and when describing the Solar System.

NCP

equator

K (= ecliptic north pole)

ecliptic

= ecliptic latitude measured in degrees, 0O-90O, north or south

= ecliptic longitude measured in degrees, 0O-360O, eastwards from the First Point of Aries

Page 20: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Galactic co-ordinatesUseful when considering the positions and motions of bodies relative to our stellar system and our position in the Galaxy.

b

NGP; b=90O

SGP

Galactic equator

GC

ll = 0O

l = 90O

l = 180O

l = 270O

Page 21: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Galactic co-ordinates (cont.)

l = Galactic longitude

Measured with respect to the direction to the Galactic Centre (GC). The Galaxy is rotating towards l = 90O.

b = Galactic latitude

The North Galactic Pole (NGP) lies in the northern hemisphere.

The subscripts I and II are used to differentiate between the

older Ohlsson system and the new IAU system of Galactic co-ordinates, ie lII, bII are IAU co-ordinates.

Page 22: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Celestial position corrections

The position for any celestial object is not necessarily its true position – a number of factors must be taken into account:

1. Atmospheric refraction

2. Aberration of starlight

3. Parallax

4. Proper motion

Page 23: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Atmospheric refraction

Starlight is refracted on entering the Earth’s atmosphere due to the change in refractive index.

Zenith(no refraction)

Sun at sunset

35’

apparent position

real positionhorizon

Page 24: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Atmospheric refraction (cont.)

Atmospheric refraction always increases the altitude of an object (ie it always reduces the zenith distance).

The constant of refraction can be measured by using the transits of a circumpolar star.

Refraction depends on the wavelength of the light observed.

For ZD < 45O, the correction to ZD, R, is given by:

where is the apparent zenith distance.

At ZD > 45O, the curvature of the Earth must be taken into account. Near ZD = 90O, special empirical tables are used.

tankR

Page 25: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Aberration of starlight

James Bradley was trying to measure stellar parallax, when he discovered the effects of stellar aberration.

1. Light has a finite velocity

2. The Earth moves relative to the star

3. The combination of velocities “moves” the star position by up to 20”.49.

v =

c =

3x1

05 k

m/s

v = 29.8 km/s

5103

8.29tan

49".20

Page 26: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Aberration of starlight (cont.)

Ecliptic co-ordinates

This was a very important discovery.

It was the first experimental confirmation of the Earth’s motion about the Sun.

It confirmed the speed of light, first estimated only 50 years before.

It showed that sources trace an ellipse around the sky in the course of a year with a semi-major axis of 20”.49 and semi-minor axis of 20”.49sin(where is the ecliptic latitude).

The effect is the same one that makes raindrops appear to be coming towards you when you’re driving through the rain.

Page 27: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Parallax

When things close to you move faster than those further away.

Page 28: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Calculating parallax

Note that the parallactic angles

M

T

L

A B

L

T

M

LTM

In one year, the Earth moves around an ellipse with semi-major axis of 149,600,000 km.

1 Astronomical Unit (AU)= 149,600,000 km

Use this to measure the distances to nearby stars.

Page 29: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Parallax in Astronomy

is the parallax angle

D

1AU

distant stars

nearby star

D

AU1tan

Page 30: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Parallax (cont.)

Stellar aberration

In one year, a nearby star will trace out an ellipse on the sky due to parallax.

Semi-major axis =

Semi-minor axis = sin ( = ecliptic latitude)

Note the similarity with aberration – however the magnitude of aberration is constant for every object in the sky. Parallax depends on the distance to the object.

Also, parallax is on a much smaller scale than aberration.

Page 31: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Stellar distance

Measuring provides the only direct way of calculating stellar distances.

An object with = 1 arcsec would lie 1 parsec away

D (parsecs) = 1/

1 parsec = 3.086x1016m

= 206,265 AU = 3.26 light years

Parallax was first measured by Bessel in 1838 who measured =0”.314 for 61 Cygni. In 1839, Henderson

measured =0”.74 for Centauri.

Our closest star is Proxima Centauri: = 0”.764, D = 1.31pc

Page 32: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Proper motion

Each star, including our Sun, has its own intrinsic space motion.

The component of this motion, combined with that of the Sun, projected on the sky, is known as Proper Motion, .

Page 33: 1B11 Foundations of Astronomy Astronomical co-ordinates Liz Puchnarewicz emp@mssl.ucl.ac.uk

1B11 Proper motion (cont.)

Proper motion seen by Hipparcos

is measured in arcseconds per year.

It has components in RA and Dec: , .

Largest proper motion known is for Barnard’s Star, where = 10.34 arcsec/year.

space velocity

vt

d

Vt = tangential speed

d=distance

dv t (SI units; in radians/sec)

dv t 74.4For vt in km/s, in

arcsec/year and d in parsecs.