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(1)

Lecture 5

- Polarisation (continued)

- Gravitational waves and their imprints on the CMB

(2)

The Single Most Important Things You Need to Remeber

• Polarisation

is generated by the local

quadrupole temperature anisotropy

,

which is proportional to

viscosity

(3)

(l,m)=(2,0) (l,m)=(2,1)

(l,m)=(2,2)

Local quadrupole

temperature anisotropy

seen from an electron

(4)

(l,m)=(2,0) (l,m)=(2,1)

(l,m)=(2,2)

Let’

s symbolise (l,m)=(2,0) as

Hot

Hot Cold Cold

(5)

(l,m)=(2,0) (l,m)=(2,1)

(l,m)=(2,2)

Let’

s symbolise (l,m)=(2,0) as

Polarisation pattern you will see

(6)

Polarisation pattern in the sky

generated by a single Fourier mode

r

L

(7)

Polarisation pattern in the sky

generated by a single Fourier mode

r

L

E-mode!

(8)

E-mode Power Spectrum

Viscosity at the last-scattering surface is given by the velocity potential:

Velocity potential is

Sin(qr

L

)

, whereas the temperature power spectrum is predominantly

Cos(qr

L

)

(9)

WMAP 9-year Power Spectrum

Bennett et al. (2013)

(10)

Planck 29-mo Power Spectrum

Planck Collaboration (2016)

(11)

[1] Trough in T -> Peak in E

[2] T damps -> E rises

because ClTT ~ cos2(qrs) whereas ClEE ~ sin2(qrs)

because

T damps by viscosity, whereas

E is created by viscosity

[3] E Peaks are sharper

because ClTT is the sum of cos2(qrL) and Doppler shift’s sin2(qrL), whereas

ClEE is just sin2(qrL)

(12)

[1] Trough in T -> Peak in E

[2] T damps -> E rises

because ClTT ~ cos2(qrs) whereas ClEE ~ sin2(qrs)

because

T damps by viscosity, whereas

E is created by viscosity

[3] E Peaks are sharper

because ClTT is the sum of cos2(qrL) and Doppler shift’s sin2(qrL), whereas

ClEE is just sin2(qrL)

(13)

Polarisation from

Re-ionisation

(14)

Polarisation from Re-ionisation

C

lEE

~

(15)

Cross-correlation between T and E

Velocity potential is

Sin(qr

L

)

, whereas the temperature power spectrum is predominantly

Cos(qr

L

)

Thus, the TE correlation is

Sin(qr

L

)Cos(qr

L

)

which

can change sign

(16)

WMAP 9-year Power Spectrum

Bennett et al. (2013)

(17)

Planck 29-mo Power Spectrum

Planck Collaboration (2016)

(18)

TE correlation is useful for understanding physics

T roughly traces gravitational potential, while E traces velocity

With TE, we witness how plasma falls into gravitational potential wells!

(19)

Example:

Gravitational Effects

Gravitational Potential, Φ

Plasma motion Coulson et al. (1994)

(20)

TE correlation in angular space

First, let’s define Stokes parameters in sphere

New X-axis: Polar angles θ

In this example, they are all Q<0

(21)

TE correlation in angular space

Put a gravitational potential well at β=0;

plasma flows to the centre. What happens?

(22)

Average Q polarisation around temperature hot spots

Komatsu et al. (2011); Planck Collaboration (2016)

Planck Data Simulation Q

(23)

Gravitational Waves

GW changes the distances between two points

d`

2

= dx

2

= X

ij

ij

dx

i

dx

j

d`

2

= X

ij

(

ij

+ D

ij

)dx

i

dx

j

(24)

Laser Interferometer

Mirror

Mirror

detector No signal

(25)

Laser Interferometer

Mirror

Mirror

Signal!

detector

(26)

Laser Interferometer

Mirror

Mirror

Signal!

detector

(27)

LIGO detected GW from binary blackholes, with the wavelength

of thousands of kilometres

But, the primordial GW affecting the CMB has a wavelength of

billions of light-years!! How

do we find it?

(28)

Detecting GW by CMB

Isotropic electro-magnetic fields

(29)

Detecting GW by CMB

h +

GW propagating in isotropic electro-magnetic fields

h

(30)

hot

hot

cold

cold

cold cold

hot hot

Detecting GW by CMB

Space is stretched => Wavelength of light is also stretched

(31)

Generation and erasure

of tensor quadrupole (viscosity)

Gravitational waves create quadrupole temperature anisotropy [i.e.,

tensor viscosity

of a photon- baryon fluid] gravitationally, without velocity potential

Still, tight-coupling between photons and baryons erases the tensor viscosity exponentially before the last

scattering

(32)

Temperature C l from GW

Scale-invariant

(33)

Entered the horizon after

the last scattering

Tensor viscosity

damped by tight coupling Tensor

ISW

Temperature C l from GW

Scale-invariant

(34)

hot

hot

cold

cold

cold cold

hot hot

Detecting GW by CMB Polarisation

electron electron

Space is stretched => Wavelength of light is also stretched

(35)

hot

hot

cold

cold

cold cold

hot hot

Detecting GW by CMB Polarisation

Space is stretched => Wavelength of light is also stretched

(36)

(l,m)=(2,0) (l,m)=(2,1)

(l,m)=(2,2)

Local quadrupole

temperature anisotropy

seen from an electron

(37)

(l,m)=(2,0) (l,m)=(2,1)

(l,m)=(2,2)

Let’s symbolise (l,m)=(2,2) as

Cold Hot

(38)

E-mode!

(39)

E-mode!

Pol on the horizon is 1/2

of the zenith

(40)

B-mode!

Pol on the horizon vanishes

(41)

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

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

(42)

Entered the horizon after the last scattering

Tensor ISW

Tensor viscosity damped by tight coupling

Polarisation generated by

tensor viscosity at the last scattering

(43)

Polarisation generated by

tensor viscosity at the last scattering

TE correlation

(44)

B-mode from lensing E-mode

from sound waves

Temperature from sound waves

B-mode from GW

We understand this

We understand this

We understand this

(45)

B-mode from lensing E-mode

from sound waves

Temperature from sound waves

B-mode from GW

We understand this

We understand this

We understand this

Enjoy starting at these power spectra, and

being able to explain all

the features in them!

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