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ASTRO 2233 Fall 2010 Adaptive Optics, Interferometry and Planet Detection Lecture 16 Thursday October 21, 2010.

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Presentation on theme: "ASTRO 2233 Fall 2010 Adaptive Optics, Interferometry and Planet Detection Lecture 16 Thursday October 21, 2010."— Presentation transcript:

1 ASTRO 2233 Fall 2010 Adaptive Optics, Interferometry and Planet Detection Lecture 16 Thursday October 21, 2010

2 Projects: Everyone has submitted an outline. After reading the Astro2010 reports and additional class discussions you can change topics if you wish but discuss it with me. Next Tuesday: Phil Muirhead

3 Effects of Atmospheric Turbulence on “Seeing” – i.e. telescope effective resolution SOLUTION – ADAPTIVE OPTICS (AO) Refractive index of atmosphere at 0.5  m n = 1 + 79 x 10 -6 P / T ; P (ressure) in millibars T(emperature) in Kelvin = 1.0003 for P = 1,000 mBar; T = 300K Variations due to small fluctuations in T (and P)

4 Adaptive Optics Ref: Center for Adaptive OpticsWavefront sensor See http://www.ucolick.org/~max/289C/ lecture 6 - Claire Max, Center for Adaptive Opticshttp://www.ucolick.org/~max/289C/

5 Correcting the wavefront using tilt information from the wavefront sensor Claire Max, Center for Adaptive Optics

6 How often do you need to correct wavefront? How fast does the atmosphere change? - depends on wind speed at turbulent layer Time constant for an isoplanetic patch size of 20 cm = 0.31 20/Vavg Vavg is average wind speed For Vavg = 20 m/s (70 km/hr) Time constant = 3 ms - need to correct wavefront every 1 ms In the near infra-red where patch size is ~1 m Time constant ~ 15 ms - need to correct wavefront ~100 times/sec Much easier in the near infra-red - slower correction - fewer actuators due to larger patch size

7 (a) Astronomers using Keck’s adaptive optics have obtained the best pictures yet of the planet Neptune. The images show bands encircling the planet and what appear to be fast-moving storms of haze. (b) The same image without adaptive optics (I. de Pater). Path of laser on Gemini North. The laser is located at the bottom of the yellow/orange beam near the right middle of the image. Note that the laser's light is directed by "relay optics" that direct the light to a "launch telescope" located behind the secondary mirror at the top/center of the telescope. Illustration based on Gemini computer animation. Laser reflects off sodium layer at ~80 km altitude LASER GUIDE “STARS”

8 Measure of Performance – STREHL RATIO Measure of the optical quality of a telescope including “seeing” problems due to atmospheric turbulence Strehl Ratio = Ratio of the amplitude of the point spread function (PSF) – the diffraction pattern - with and without the atmosphere assuming a perfect telescope. Point spread function for no atmosphere – Strehl ratio = 1.0

9 Multi-conjugate adaptive optics – multiple guide stars - allows three dimensional reconstruction of atmospheric turbulence and wider fields of view (European Southern Observatory slide)

10 Extreme adaptive optics – high resolution and high contrast imaging Multiple guide stars Thousands of actuators on deformable mirror Very high precision for setting deformable mirror - a few nm Very high speed in setting deformable mirror – several kHz Center for Adaptive Optics image

11 Angular separation of nulls in diffraction pattern = λ/d INTERFEROMETRY - Very high resolution

12 k = 2 π/λ INTERFEROMETRY

13 VERY LARGE ARRAY Very Large Array, New Mexico

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15 Cygnus A VLA Image at 5 GHz (6 cm wavelength)

16 Atacama Large Millimeter Array Wavelengths 350  m to 1 cm Best resolution ~10 mas

17 RESOLUTION = λ/D VLA (A array) at 3.5 cm: Resolution ~ 0.2 arcsec Atacama mm array: Resolution ~ 0.02 arcsec at 1 mm wavelength

18 Keck 10-m optical telescopes, Hawaii. Experimental interferometer.

19 LARGE BINOCULAR TELESCOPE Mt Graham, Arizona Two 8.4 m mirrors spaced 14.4 m apart 8.4 m => ~14 mas resolution (no atmosphere) 14.4 m => 8 mas fringe spacing as interferometer

20 European Southern Observatory (ESO) Very Large Telescope(S) - 4 x 8M

21 VLT Interferometry

22 Space Interferometry Mission - SIM What: Interferometer – 10m baseline Positional Accuracy – 4 μarcsec (1 μarcsec relative over 1 deg field) Distance measurements: 1% accuracy to several thousand parsecs 10% over whole galaxy CALIBRATE CEPHEID and RR LYRA VARIABLE STARS Planet search – astrometric search nulling interferometer tests dynamic range of 10 4

23 Detection of Angular Motion of the Parent Star about the Center-of-Mass of System No periodic motion means no planet – or planet to small/distant from star 1.Astrometry – measuring the positional motion of the star Remember for two bodies in a circular orbit about each other – i.e. about the CM: m 1 r 1 = m 2 r 2 For a planet about a star a ☼ = m p a p / m ☼ - what is this telling us about the radius of the orbit of a planet that would make it easiest to detect where a ☼ = radius of star orbit via periodic positional changes of the star? a p = radius of planet orbit – large is good => bigger star orbit radius The angular shift in the star’s position is : θ = a ☼ / R radians where R is the distance to the star from Earth = {m p a p / m ☼ } / R arc sec if a p is in AU and R is in parsecs

24 Sun’s trajectory about the center-of- mass of the solar system. As viewed from 10 parsecs (32 light years) away. ASTROMETRY – measuring angular deflection of the parent star about center of mass of system

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26 Example: for circular orbits, planet-star pair, * = velocity of star For Circular Orbit Maximum velocity for elliptical orbits r 1 = radius of star orbit about center-of-mass = a m 2 /(m 1 + m 2 ) a = star-planet distance Basis for discovering extra- solar planets http://upload.wikimedia.org/wikipedia/commons/5/59/Orbit3.gif 2. Velocity of the Star measurements via Doppler Shift from Keppler’s 3 rd law, a 3  p 2 p is the orbit period

27 For a star in a circular orbit and assuming that m p << m ☼ then: The measured maximum velocity is given by v max = 28.4 p -1/3 {m p Sin i / M J } m ☼ -2/3 m sec -1 Where p is the orbit period in years, Sin i is the sine of the orbit inclination relative to the line-of-sight from Earth, M J is the mass of Jupiter and m ☼ is the mass of the star in solar masses. For an elliptical orbit: v max = {2  G / p} 1/3 {m p Sin i / (m p + m ☼ ) 2/3 } {1 / (1 – e 2 ) 1/2 } m sec -1 Jupiter orbiting the Sun: v max = 12.5 m sec -1, where p = 11.9 years For Earth orbiting the Sun v max = 0.1 m sec -1 - very difficult to measure

28 The measured maximum velocity is given by v max = 28.4 p -1/3 {m p Sin i / M J } m ☼ -2/3 m sec -1 Where p is the orbit period in years, Sin i is the sine of the orbit inclination relative to the line-of-sight from Earth, M J is the mass of Jupiter and m ☼ is the mass of the star in solar masses. Gliese 281 g: m ☼ = 0.3 solar masses P = 36.5 days = 0.1 years Sin i = 1 m p = 3 Earth masses = 0.01 mass of Jupiter Velocity = 1.36 m/sec

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30 Astrometry: Advantages: Direct measurement of mass of the planet – assumes we know star’s mass from stellar type – i.e. spectral class Sensitive to large planets a long way from the star Disadvantages: θ  1 / Distance to the star => nearby stars only [θ max for Sun – Jupiter from 10 light years  1.6 milli arc sec] Velocity measurements: Advantages: Sensitive to large planets close to the star Not directly dependent on distance to the star – just need sensitivity Disadvantages: m p Sin i - lower limit on the mass Not sensitive to planets at large distances from the star

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