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1 Polarimetric direct detection of extra-solar Planets with SPHERE/ZIMPOL “In the spirit of Bernard Lyot” Berkeley, 4.-8. June 2007 Franco Joos ETH Zürich, Switzerland A lot of different approaches to directly detect extra-solar planets. We will do it with
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Polarimetric direct detection ofextra-solar Planets with

SPHERE/ZIMPOL

“In the spirit of Bernard Lyot”Berkeley, 4.-8. June 2007

Franco JoosETH Zürich, Switzerland

● A lot of different approaches to directly detectextra-solar planets. We will do it with

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● A lot of different approaches to directly detectextra-solar planets. We will do it with

SPHERE/ZIMPOL

● SPHERE is a second generation ESO-VLTinstrument with three complementary focalplane instruments aiming to directly detectand analyze giant extra-solar planets

● Two near-IR instruments searching for self-luminous young planets. The third is a high-precision imaging polarimeter ZIMPOLdetecting and analyzing reflected light fromolder planets

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● There will be an overview talk on SPHEREby Jean-Luc Beuzit (PI) tomorrow

● Poster by Anthony Boccaletti: developmentof coronagraphs for SPHERE

● I will concentrate on the polarimetricinstrument ZIMPOL which is the Zürichcontribution to SPHERE

● One of the main problem if trying to directlydetect an extra-solar planets from theground:

The planet is MUCH fainter than the halo ofthe stellar PSF

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● One of the main problem if trying to directlydetect an extra-solar planets from theground:

The planet is MUCH fainter than the halo ofthe stellar PSF

Solution: Use extreme AO and coronagraphyand go for differential technique, searchingfor a signal present at the planet position butnot present in the stellar PSF

● One of the main problem if trying to directlydetect an extra-solar planets from theground:

The planet is MUCH fainter than the halo ofthe stellar PSF

Solution: Use extreme AO and coronagraphyand go for differential technique, searchingfor a signal present at the planet position butnot present in the stellar PSF

imaging polarimetry

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● Light reflected by a planet can highly bepolarized, whereas the starlight can beassumed to be unpolarized

● Light reflected by a planet can highly bepolarized, whereas the starlight can beassumed to be unpolarized

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● A polarimetric measurement is obtained bytaking the difference of the two intensities atorthogonal polarization directions ( I∥ - I⊥).The normalized difference gives thepolarization degree: p = Q/I = (I∥ - I⊥)/(I∥ + I⊥).

● ZIMPOL (Zürich IMaging POLarimeter) is ahigh-precision imaging polarimeter providinga polarimetric precision of better than 10-5

working in the range of 600 to 900nm forSPHERE

synchronization (kHz)

modulator

polarizer

demodulatingCCD detector

S(t) I(t)Spolarization

signalmodulatedpolarization

signal

modulatedintensitysignal

ZIMPOL measuring principle:

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● After thousands of modulation cycles theCCD is read out in less than a second

● ZIMPOL image contains two sub-images ofthe same object at orthogonal polarizationdirections

● Compute the difference and normalize → Q/I

ZIMPOL polarizationmeasurements at 630nmfor Jupiter and Saturn atMc Math Pierce telescope,Kitt Peak

I

Q/I

U/I

Example: Jupiter andSaturn

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Summary of the ZIMPOL technique:

• images of two opposite polarization modes arecreated simultaneously

→ modulation faster than seeingvariations• both images are recorded with same pixel

→ both images are subject to the sameaberrations (chromatic effects)• integration over many modulation cycleswithout readout (low RON)

Precision of 10-5 is routinely achieved in solarapplications

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THE END

Noise CurveNoise Curve

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ZIMPOL camera (1. generation)

limb

total slit

center

Example of “long-slit” spectropolarimetry of Uranus

Joos & Schmid, 2007, A&A

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polarization p(90) vs. reflectivityf(90)

Solar system planets surfaceproperties

p(90) f(90)rockyMercury 5-10% lowMars 5-10% low

cloudy (little Rayleigh scatt.)Venus <5% (–) highSaturn <5% high

cloudy and Rayleigh scatt.Jupiter 5-20% highEarth 5-20% high

strong Rayleigh scatteringUranus >15% med.Neptune >15% med.Titan 50% med.

R-band

● The orientation of theexo-system matters,because thepolarization dependson the phase angle:– always perfect for a

face-on system– twice a year perfect

for an inclined system

star

planet

polarization

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Intensity ratio of exo-Sun and exo-Jupiterat 1'' separation ≈108.

108

logI

1''

Example: Jupiter-Sun system at 5pc

Intensity ratio of exo-Sun and exo-Jupiterat 1'' separation ≈108.

Degradation of the point-like sources duetothe atmosphere→ bright halo of the star→ overlapping of the two intensities→ contrast at the position of the planet≈107

→ too large for an imaging polarimeter

108

logI

107

logI

1''

Example: Jupiter-Sun system at 5pc

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Intensity ratio of exo-Sun and exo-Jupiterat 1'' separation ≈108.

Reducing the contrast by extreme AOand coronagraphy to ≈104. Contrast inthe regime of the most sensitiveimagingpolarimeters.

Degradation of the point-like sources duetothe atmosphere→ bright halo of the star→ overlapping of the two intensities→ contrast at the position of the planet≈107

→ too large for an imaging polarimeter

107

logI

108

logI

104

logI

1''

Example: Jupiter-Sun system at 5pc

Intensity ratio of exo-Sun and exo-Jupiterat 1'' separation ≈108.

Reducing the contrast by extreme AOand coronagraphy to ≈104. Contrast inthe regime of the most sensitiveimagingpolarimeters.

Degradation of the point-like sources duetothe atmosphere→ bright halo of the star→ overlapping of the two intensities→ contrast at the position of the planet≈107

→ too large for an imaging polarimeter

107

logI

108

logI

104

logI

1''

Example: Jupiter-Sun system at 5pc

ZIMPOL


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