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Day 2: Polarisation of the CMB

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Day 2:

Polarisation of the CMB

Eiichiro Komatsu

[Max Planck Institute for Astrophysics]

University of Amsterdam March 5, 2020

Lecture notes:

https://wwwmpa.mpa-garching.mpg.de/~komatsu/lectures--reviews.html

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How do we measure

gravitational waves?

(3)

Measuring GW

d`

2

= dx

2

= X

ij

ij

dx

i

dx

j

d`

2

= X

ij

(

ij

+ h

ij

)dx

i

dx

j

GW changes distances between two points

(4)

Laser Interferometer

Mirror

Mirror

detector No signal

(5)

Laser Interferometer

Mirror

Mirror

Signal!

detector

(6)

LIGO detected GW from a binary

blackholes, with a frequency of ~100 Hz

= the wavelength of thousands of kilometres

But, the primordial GW affecting the

CMB has a frequency of 10 –18 Hz = the wavelength of billions of light-years!!

How do we find it?

(7)

Detecting GW by CMB

Isotropic electro-magnetic fields

(8)

Detecting GW by CMB

GW propagating in isotropic electro-magnetic fields

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hot

hot

cold

cold

cold cold

hot hot

Detecting GW by CMB

Space is stretched => Wavelength of light is also stretched

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hot

hot

cold

cold

cold cold

hot hot

Detecting GW by CMB Polarisation

electron electron

Space is stretched => Wavelength of light is also stretched

h + ij

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h ij

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(11)

hot

hot

cold

cold

cold cold

hot hot

Detecting GW by CMB Polarisation

Space is stretched => Wavelength of light is also stretched

h + ij

11

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h ij

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(12)

horizontally polarised

Photo Credit: TALEX

(13)

Photo Credit: TALEX

(14)

Physics of CMB Polarisation

Necessary and sufficient conditions for generating polarisation in CMB:

Thomson scattering

Quadrupolar temperature anisotropy around an electron

By Wayne Hu

(15)
(16)

Credit: ESA

(17)

Credit: ESA

(18)

E and B mode

E mode

: Polarisation directions

parallel or perpendicular

to the wavevector

B mode

: Polarisation directions

45 degree tilted

with respect to the wavevector

(19)

E&B decomposition:

A closer look

(20)

Polarisation

No polarisation

Polarised in x-direction

(21)

Stokes Parameters

[Flat Sky, Cartesian coordinates]

a

b

(22)

Stokes Parameters

change under coordinate rotation

x’

Under (x,y) -> (x’,y’):

y’

(23)

Compact Expression

Using an imaginary number, write

Then, under coordinate rotation we have

(24)

E and B decomposition

That Q and U depend on coordinates is not very convenient…

Someone said, “I measured Q!” but then someone else may say, “No, it’s U!”. They flight to death, only to

realise that their coordinates are 45 degrees rotated from one another…

The best way to avoid this unfortunate fight is to define a coordinate-independent quantity for the distribution of

polarisation

patterns

in the sky

To achieve this, we need

to go to Fourier space

(25)

ˆ

n = (sin ✓ cos , sin ✓ sin , cos ✓ )

“Flat sky”,

if θ is small

(26)

Fourier-transforming Stokes Parameters?

As Q+iU changes under rotation, the Fourier coefficients change as well

So…

where

(27)

Tweaking Fourier Transform

Under rotation, the azimuthal angle of a Fourier wavevector, φl, changes as

This

cancels

the factor in the left hand side:

where we write the coefficients as(*)

(*) Nevermind the overall minus sign. This is just for convention

(28)

Tweaking Fourier Transform

We thus write

And, defining

By construction El and Bl do not pick up a factor of exp(2iφ) under coordinate rotation.

That’s

great!

What kind of polarisation patterns do these quantities represent?

Seljak (1997); Zaldarriaga & Seljak (1997); Kamionkowski, Kosowky, Stebbins (1997)

(29)

Pure E, B Modes

Q and U produced by E and B modes are given by

Let’s consider Q and U that are produced by a single Fourier mode

Taking the x-axis to be the direction of a wavevector, we obtain

(30)

Pure E, B Modes

Q and U produced by E and B modes are given by

Let’s consider Q and U that are produced by a single Fourier mode

Taking the x-axis to be the direction of a wavevector, we obtain

(31)

Geometric Meaning

E mode

: Stokes

Q

, defined with respect to as the x-axis

B mode

: Stokes

U

, defined with respect to as the y-axis IMPORTANT: These are all

coordinate-independent

statements

(32)

Parity

E mode

: Parity even

B mode

: Parity odd

(33)

Parity

E mode

: Parity even

B mode

: Parity odd

(34)

Power Spectra

However,

<EB> and <TB> vanish

for parity- preserving fluctuations because <EB> and <TB> change sign under parity flip

(35)

Power Spectra

However,

<EB> and <TB> vanish

for parity- preserving fluctuations because <EB> and <TB> change sign under parity flip

<EB> and <TB> can be non-zero if physics that produced gravitational waves during information

broke parity! This will be the topic on March 19

(36)

How do gravitational waves generate E&B

polarisation?

(37)

Distance between two points in space

Inhomogeneous curved space

In Cartesian comoving coordinates

“metric perturbation”

-> CURVED SPACE!

(38)

Now I am going to change notation (sorry!): h ij -> D ij

Notation in today’s lecture follows that of the text book

“Cosmology” by Steven Weinberg

(39)

Space-time Distance

Einstein told us that a clock ticks slowly when gravity is strong…

Space-time distance, ds4, is modified by the presence of gravitational fields

: Newton’s gravitational potential

: Spatial scalar curvature perturbation

: Tensor metric perturbation [=gravitational waves]

(40)

Tensor perturbation D ij :

Area-conserving deformation

Determinant of a matrix

is given by

Thus, Dij must be trace-less

if it is area-conserving deformation of two points in space

(41)

Curvature Perturbation

Einstein told us that a clock ticks slowly when gravity is strong…

Space-time distance, ds4, is modified by the presence of gravitational fields

: Newton’s gravitational potential

: Spatial scalar curvature perturbation

is a perturbation to the determinant of spatial metric

(42)

Evolution of

photon’s coordinates

Photon’s path is determined such that the distance

traveled by a photon between two points is minimised.

This yields the equation of motion for photon’s coordinates

This equation is known as the “geodesic equation”.

The second term is needed to keep the form of the equation unchanged under general coordinate transformation => GRAVITATIONAL EFFECTS!

y

x

“u” labels photon’s path

(43)

Evolution of

photon’s momentum

It is more convenient to write down the geodesic equation in terms of the photon momentum:

y

x

“u” labels photon’s path then

Magnitude of the photon momentum is equal to the photon energy:

(44)

Some calculations…

With ( )

Scalar perturbation [valid to all orders] Tensor perturbation [valid to 1st order in D]

(45)

Recap

Requiring photons to travel between two points in

space-time with the minimum path length, we obtained the geodesic equation

The geodesic equation contains that is required to make the form of the equation unchanged under

general coordinate transformation

Expressing in terms of the metric perturbations, we obtain the desired result - the equation that describes the rate of change of the photon energy!

Math may be messy but the concept is transparent!

(46)

Let’s interpret this equation physically

The Result

γi is a unit vector of the direction of photon’s momentum:

Sachs & Wolfe (1967)

(47)

Cosmological redshift

Photon’s wavelength is stretched in proportion to the scale factor, and thus the photon energy decreases as

The Result

γi is a unit vector of the direction of photon’s momentum:

p / a 1

Sachs & Wolfe (1967)

(48)

Cosmological redshift - part II

The spatial metric is given by

Thus, locally we can define a new scale factor:

Then the photon momentum decreases as

The Result

ds

2

= a

2

(t) exp( 2 )dx

2

˜

a(t, x) = a(t) exp( )

p / a ˜ 1

Sachs & Wolfe (1967)

(49)

Gravitational blue/redshift (Scalar)

The Result

Potential well (φ < 0)

Sachs & Wolfe (1967)

(50)

Gravitational blue/redshift (Tensor)

The Result

Sachs & Wolfe (1967)

(51)

The Result

Gravitational blue/redshift (Tensor)

Sachs & Wolfe (1967)

(52)

Formal Solution (Scalar)

or

Line-of-sight direction

Coming distance (r)

Sachs & Wolfe (1967)

“L” for “Last scattering surface”

(53)

Formal Solution (Scalar)

Line-of-sight direction

Coming distance (r) Initial Condition

Sachs & Wolfe (1967)

(54)

Formal Solution (Scalar)

Line-of-sight direction

Comoving distance (r) Gravitational Redshit

Sachs & Wolfe (1967)

(55)

Formal Solution (Scalar)

Line-of-sight direction

Coming distance (r)

“integrated Sachs-Wolfe” (ISW) effect

Sachs & Wolfe (1967)

(56)

Formal Solution (Tensor)

Sachs & Wolfe (1967)

negligible contribution before the last scattering

(57)

Formal Solution (Tensor)

negligible contribution before the last scattering Sachs & Wolfe (1967)

(58)

Formal Solution (Tensor)

negligible contribution before the last scattering Sachs & Wolfe (1967)

When a plane wave gravitational wave propagates in the z direction, no temperature anisotropy is seen towards the poles (θ=0, π). The anisotropy is

maximised on the horizon (θ=π/2) with cos(2φ) &

sin(2φ) modulation in the azimuthal directions.

(59)

Formal Solution (Tensor)

negligible contribution before the last scattering Sachs & Wolfe (1967)

Spherical harmonics Ylm(θ,φ) with (l,m)=(2,2)

(60)

E-mode!

(61)

E-mode!

Pol on the horizon is 1/2

of the zenith

(62)

B-mode!

Pol on the horizon vanishes

(63)

propagation direction of GW h

+

=cos(kx)

Polarisation directions perpendicular/parallel to the

wavenumber vector -> E mode polarisation

(64)

propagation direction of GW h

x

=cos(kx)

Polarisation directions 45 degrees tilted from to the

wavenumber vector -> B mode polarisation

(65)

CAUTION: we are NOT seeing a single plane wave propagating perpendicular to our line of sight

Signature of gravitational

waves in the sky [?]

(66)

CAUTION: we are NOT seeing a single plane wave propagating perpendicular to our line of sight

Signature of gravitational waves in the sky [?]

if you wish, you could associate one pattern with one plane wave…

BUT

(67)

Propagation of cosmological gravitational waves

Tensor anisotropic stress can do two things:

It can generate gravitational waves

It can damp gravitational waves (neutrino anisotropic stress)

tensor

But we ignore the tensor anisotropic stress today

(68)

Super-horizon Solution

Super-horizon tensor perturbation is conserved

Thus, no ISW temperature anisotropy on super-horizon scales

It does not look like “gravitational waves”, but it will start oscillating and behaving like waves once it enters the

horizon

D ij = constant + decaying term

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(69)

Matter-dominated Solution

∂Dij/∂t gives the ISW. It peaks at the horizon crossing, qη~2

The energy density is given by (∂Dij/∂t)2, which indeed decays like radiation, a–4

/ 1 a(t)

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/ 1

a 2 (t)

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η: “conformal time”, or the distance traveled by photons

(70)

Temperature C l from GW

Scale-invariant

(71)

Entered the horizon after the last scattering

Tensor mode damped by

redshifts between the horizon re-

entry and the decoupling Tensor

ISW

Temperature C l from GW

Scale-invariant

(72)

Temperature C l from GW

Scale-invariant

This is NOT a Silk- like damping!

It’s not

exponential, but a

power-law due

simply to redshifts

(73)

E and B modes are produced nearly equally, but on small

scales B is smaller than E because B vanishes on the horizon

(74)

E and B modes are produced nearly equally, but on small

scales B is smaller than E because B vanishes on the horizon

(75)

E and B modes are produced nearly equally, but on small

scales B is smaller than E because B vanishes on the horizon

This damping is actually due to the “Fuzziness”

damping from the finite extent of the

last-scattering

surface

(76)

No Fuzziness damping

Pritchard and Kamionkowski (2005)

(77)

With damping

Pritchard and Kamionkowski (2005)

(78)

Entered the horizon after the last scattering

Tensor ISW

Polarisation generated by scattering at the

last scattering

(79)

Polarisation generated by scattering at the

last scattering

TE correlation

(80)

B-mode from lensing E-mode

from sound waves

Temperature from sound waves

B-mode from GW

We understand this

(81)

Appendix:

Experimental Landscape

(82)

What comes next?

Advanced Atacama Cosmology Telescope

South Pole Telescope “3G”

CLASS

BICEP/Keck Array

(83)

Advanced Atacama

Cosmology Telescope

(84)

South Pole Telescope “3G”

CLASS BICEP/Keck Array

CMB-S4(?)

(85)

The Biggest Enemy:

Polarised Dust Emission

The upcoming data will NOT be limited by statistics, but by systematic effects such as the Galactic contamination

Solution: Observe the sky at multiple frequencies, especially at high frequencies (>300 GHz)

This is challenging, unless we have a superb, high- altitude site with low water vapour

CCAT-p!

(86)

CCAT-p Collaboration

(87)

Frank Bertoldi’s slide from the Florence meeting

(88)

Frank Bertoldi’s slide from the Florence meeting

Cornell U. + German consortium + Canadian consortium + …

(89)

A Game Changer

CCAT-p

: 6-m, Cross-dragone design, on Cerro Chajnantor (5600 m)

Germany makes great telescopes!

Design study completed, and the contract has been signed by

“VERTEX Antennentechnik GmbH”

CCAT-p is a great opportunity for Germany to make

significant contributions towards the CMB S-4 landscape (both US and Europe) by providing telescope designs and the “lessons learned” with prototypes.

(90)

Simons Observatory (USA)

in collaboration

South Pole?

(91)

Simons Observatory (USA)

in collaboration

South Pole?

This could be

“CMB-S4”

(92)

To have even more

frequency coverage…

(93)

ESA

2025– [proposed]

JAXA

LiteBIRD

+ participations from USA, Canada, Europe

Polarisation satellite dedicated to measure CMB polarisation from

primordial GW, with a few thousand TES bolometers in space

2028–

(94)

ESA

2025– [proposed]

JAXA

LiteBIRD

May 21, 2019: JAXA has chosen LiteBIRD as the strategic large-class mission.

We will go to L2!

+ participations from USA, Canada, Europe

Selected!

2028–

(95)

Polarized foregrounds

Synchrotron radiation and thermal emission from inter-galactic dust Characterize and remove foregrounds

15 frequency bands between 40 GHz - 400 GHz

Split between Low Frequency Telescope (LFT) and High Frequency Telescope (HFT) LFT: 40 GHz 235 GHz

HFT: 280 GHz 400 GHz

Foreground Removal

7

Polarized galactic emission (Planck X) LiteBIRD: 15 frequency bands

Slide courtesy Toki Suzuki (Berkeley)

(96)

LiteBIRD

LiteBIRD Spacecraft

LiteBIRD for B-mode from Space

2018/7/21 11

LFT (5K)

HG-antenna HFT (5K)

V-groove

radiators SVM/BUS

PLM 200K100K30K

JAXA

H3 LFT (Low frequency telescope) 34 – 161 GHz : Synchrotron + CMB HFT (high frequency telescope) 89 – 448 GHz : CMB + Dust

4.5 m

Focal plane 0.1K

Slide courtesy Yutaro Sekimoto (ISAS/JAXA)

European Contribution

(97)

LiteBIRD Collaboration

(98)

LiteBIRD Collaboration

Referenzen

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