Marginalizing over the waveform systematics of compact ...

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Rochester Institute of Technology Rochester Institute of Technology RIT Scholar Works RIT Scholar Works Theses 8-2021 Marginalizing over the waveform systematics of compact binary Marginalizing over the waveform systematics of compact binary coalescence models using RIFT coalescence models using RIFT Aasim Zahoor Jan [email protected] Follow this and additional works at: https://scholarworks.rit.edu/theses Recommended Citation Recommended Citation Jan, Aasim Zahoor, "Marginalizing over the waveform systematics of compact binary coalescence models using RIFT" (2021). Thesis. Rochester Institute of Technology. Accessed from This Thesis is brought to you for free and open access by RIT Scholar Works. It has been accepted for inclusion in Theses by an authorized administrator of RIT Scholar Works. For more information, please contact [email protected].

Transcript of Marginalizing over the waveform systematics of compact ...

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Rochester Institute of Technology Rochester Institute of Technology

RIT Scholar Works RIT Scholar Works

Theses

8-2021

Marginalizing over the waveform systematics of compact binary Marginalizing over the waveform systematics of compact binary

coalescence models using RIFT coalescence models using RIFT

Aasim Zahoor Jan [email protected]

Follow this and additional works at: https://scholarworks.rit.edu/theses

Recommended Citation Recommended Citation Jan, Aasim Zahoor, "Marginalizing over the waveform systematics of compact binary coalescence models using RIFT" (2021). Thesis. Rochester Institute of Technology. Accessed from

This Thesis is brought to you for free and open access by RIT Scholar Works. It has been accepted for inclusion in Theses by an authorized administrator of RIT Scholar Works. For more information, please contact [email protected].

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Marginalizing over the waveformsystematics of compact binary

coalescence models using RIFT

Aasim Zahoor Jan

A Thesis Submitted in Partial Fulfillment of theRequirements for the Degree of Master of Science in

Physics

School of Physics and Astronomy

College of Science

Rochester Institute of Technology

Rochester, NY

August , 2021

Approved by:George Thurston, Ph.D. DateDirector, Physics MS program

Approval Committee: Richard O’Shaughnessy, Carlos Lousto, George Thurston, YosefZlochower

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School of Physics and Astronomy

College of Science

Rochester Institute of Technology

Rochester, NY

CERTIFICATE OF APPROVAL

M.S. DEGREE THESISThe M.S. Degree Thesis of Aasim Zahoor Janhas been examined and approved by the thesis

committee as satisfactory for the thesisrequirement for the M.S. degree in Physics.

Dr. Richard O’Shaughnessy, Thesis Advisor

Dr. Carlos Lousto

Dr. George Thurston

Dr. Yosef Zlochower

Date

1

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To my parents: None of this would be possible without you.

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Aasim Zahoor Jan Master’s Thesis

Acknowledgements

I would like to thank Dr.Richard O’Shaughnessy for being a wonderful advisor and help-

ing me delve deeper into the world of gravitational waves.

I would like to thank Dr.George Thurston for being a great program coordinator.

I would like to thank Anjali Yelikar for helping me get started with my research.

I would like to like to thank Dr.Carlos Lousto and Dr.Yosef Zlochower for showing in-

terest in my research.

I am grateful for the computational resources provided by the LIGO Hanford Observa-

tory. I am grateful for the computational resources provided by Leonard E Parker Center

for Gravitation, Cosmology, and Astrophysics at the University of Wisconsin-Milwaukee.

I am grateful for the computational resources provided by California Institute of Tech-

nology. I am grateful to the School of Physics and Astronomy, Rochester Institute of

Technology for allowing me to complete this work.

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Abstract

As Einstein’s equations for binary compact object inspiral have only been approximately

or intermittently solved by analytic or numerical methods, the models used to infer pa-

rameters of gravitational wave (GW) sources are subject to waveform modeling uncer-

tainty. We illustrate these differences and then introduce a very efficient technique to

marginalize over waveform uncertainties, relative to a prespecified sequence of waveform

models. We also extend this technique to include dynamic weighting by calculating over-

lap of models with Numerical Relativity. Being based on RIFT, a very efficient parameter

inference engine, our technique can directly account for any available models, including

very accurate but computationally costly waveforms. Our evidence and likelihood-based

method works robustly on a point-by-point basis, enabling accurate marginalization for

models with strongly disjoint posteriors while simultaneously increasing the reusability

and efficiency of our intermediate calculations.

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Contents

1 Introduction 1

1.1 General Theory of Relativity . . . . . . . . . . . . . . . . . . . . . . . . . 1

1.2 Gravitational waves . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 2

1.3 Sources of gravitational waves . . . . . . . . . . . . . . . . . . . . . . . . 5

1.4 Detection of gravitational waves . . . . . . . . . . . . . . . . . . . . . . . 7

1.5 Binary systems . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8

1.5.1 Ordinary binary systems . . . . . . . . . . . . . . . . . . . . . . . 8

1.5.2 Binary mergers . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11

1.6 Modeling gravitational waves . . . . . . . . . . . . . . . . . . . . . . . . 14

1.7 Motivation and brief discussion . . . . . . . . . . . . . . . . . . . . . . . 15

2 Assessing and Marginalizing over compact binary coalescence wave-

form systematics using RIFT 17

2.1 Bayes’ theorem . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17

2.2 RIFT review . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18

2.3 Waveform models . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 20

2.4 Fiducial synthetic sources and P-P tests . . . . . . . . . . . . . . . . . . 21

2.5 Zero noise runs to assess systematic biases . . . . . . . . . . . . . . . . . 22

2.6 Marginalizing over waveform systematics . . . . . . . . . . . . . . . . . . 24

2.7 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26

2.7.1 Demonstrating and quantifying waveform systematics . . . . . . . 26

2.7.2 A P-P plot test for marginalizing over waveform errors . . . . . . 30

3 Numerical Relativity weighted model marginalization 32

3.1 Mismatch, overlap and calculating weights . . . . . . . . . . . . . . . . . 32

3.2 Nearest neighbor interpolator . . . . . . . . . . . . . . . . . . . . . . . . 36

3.3 Results . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 36

4 Conclusions and Discussions 39

4.1 Future work . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39

4.2 Conclusions . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 39

References 41

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1 Introduction

In 1907 Einstein had a thought which would ultimately lead to the Theory of Relativity

and also this thesis. The thought was that in a free-falling frame a person wouldn’t

be able to feel their weight. It seems obvious to us from our physical experiences but

Einstein felt that such common observation held deeper meanings. His suspicions were

also fueled by the fact that acceleration due to gravity experienced by an object at a point

in space does not depend on the constitution of that object. This thought process lead

him to extend the already established Equivalence Principle to the Modern Equivalence

Principle, also called the Strong Equivalence Principle.

The Strong Equivalence Principle states that for an observer in free-fall in a

gravitational field, the results of all local experiments are independent of the magnitude

of the gravitational field [1]. This made Einstein theorize that gravitational force is

a fictitious force and the reason we believe it exists is that we carry out experiments

in non-inertial frames [2]. Einstein further theorized that gravity is not a property of

masses but a universal property of the spacetime itself, ultimately leading him to develop

the General Theory of Relativity which was published in 1915.

1.1 General Theory of Relativity

General Theory of Relativity is a relationship between mass and curvature that imple-

ments the principles of equivalence [1]. It is one of the most successful theories of gravity

we have and has stood up extremely well to tests. After it was published, it not only

explained physical phenomena that had already been explained by Newton’s theory of

gravity but also elegantly explained phenomena that were still puzzling physicists. It

was also able to predict several other physical phenomena and the existence of objects

which hadn’t yet been discovered.

The Theory of Relativity was able to explain the orbital precession of Mercury,

gravitational lensing, frame-dragging, and gravitational time dilation. It also predicted

the existence of black holes and gravitational waves.

In the present form, equations of the Theory of Relativity also known as Einstein’s

Field Equations (EFE) are given by equation 1. This quote from Physicist John Wheeler

perfectly encapsulates the essence of EFE: “Space-time tells matter how to move and

matter tells space-time how to curve”.

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Rµν −1

2Rgµν + λgµν =

8πGTµνc4

(1)

where Rµν is the Ricci tensor, R is the Ricci scalar, gµν is the metric tensor, Tµν is the

Energy-momentum tensor, G is the Newtonian gravitational constant, λ is the cosmo-

logical constant, and c is the speed of light in vacuum. It should be noted that despite

its simple appearence, this equation represents ten different equations as it is a tensor

equation (16 due to this being a 2nd order tensor equation but since the tensors in this

equation are symmetric, they reduce to 10).

1.2 Gravitational waves

In 1978, Russell Hulse and Joseph Taylor discovered a binary neutron star system (“Hulse

Taylor” pulsar PSR 1913+16) which provided the first experimental proof for the exis-

tence of gravitational waves [3]. It was observed that the neutron stars in the binary

system were getting closer to each other and the rate at which they were getting closer

to each other was exactly at the rate predicted by Einstein’s Theory of Relativity if the

energy loss was in the form of gravitational waves. This served as the indirect confirma-

tion for the existence of gravitational waves and also as a test for the Theory of General

Relativity. Russell Hulse and Joseph Taylor were awarded the Nobel Prize in 1993 for

the discovery of the binary system. However, this was an indirect confirmation of the

existence of gravitational waves so the race to detect gravitational waves continued. It

was not until September 14, 2015 that the first gravitational waves were detected by

Laser Interferometer Gravitational wave Observatory (LIGO). These waves were emit-

ted during the merger of a binary black hole system approximately 1.3 billion light-years

away. For their contributions to the LIGO detector and the first ever direct detection

of gravitational waves, Barry Barish, Kip Thorne, and Rainer Weiss were awarded the

Nobel Prize in 2017.

In the Theory of Relativity, gravitational waves are interpreted as propagating

perturbations and visualized as ripples through space-time. In the weak field regime,

meaning we are far away from a gravitational wave source and in a nearly flat space-time,

we can express the metric tensor in terms of Minkowski metric and a perturbation.

gµν = ηµν + hµν

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where ηµν is the Minkowski metric (diag(−1, 1, 1, 1)), hµν is the perturbation (|hµν | <<1), and if we introduce trace reversed perturbation, then we have

hµν = hµν −1

2ηµνh (3)

Also, if we utilize our gauge freedom and decide to use Lorentzian gauge

∂ν hνµ = 0 (4)

Plugging these back into Einstein’s field equations we have the common form of the

Einstein’s equation for linearized gravity

�hµν = −16πGTµνc4

(5)

where � is the d’Alembertian operator, a four dimensional Laplacian (� = − ∂2

∂t2+∇2).

This equation is not only solvable but also has wave solutions and those solutions are

called gravitational waves. These gravitational waves are generated by the second time

derivative of the quadrupole moment of the source.

In vacuum (Tµν = 0), the linearized equation of gravity becomes

�hµν = 0 (6)

The solutions for this equation are expected to be a superposition of plane waves of the

form (Einstein’s summation convention being used)

hµν(x) = αµνeikαxα

where αµν is a constant, symmetric 4×4 matrix called the polarization tensor, kµ is the 4-

wavevector such that kµ = (ω/c,k), where ω is the wave angular velocity. Instead of 16,

the polarization tensor has only 10 independent components as it can be represented by a

symmetric matrix. Also, due to the Lorentz gauge condition the number of independent

components reduce to 6 as the Lorentz gauge condition implies:

kµαµν = 0 (7)

We can further reduce the number of independent components by utilizing our gauge

freedom to choose the Transverse Traceless (TT) gauge, which is represented by the

four equations given in equation (8). This gives us four more constraints reducing the

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number of independent components to 2

h0i = 0

Trh ≡ hµµ = 0(8)

here i = (1, 2, 3). In terms of polarization tensor, these conditions can be expressed as

α0i = 0

Trα = αµµ = 0(9)

From equation (7) and equation (9) we get

α0µ = 0 (10)

Also, if we assume the wave to be moving in z direction so that kµ = (ω, 0, 0, ω) and ω

is a constant, then the polarization tensor can be represented as

αµν =

0 0 0 0

0 α11 α12 0

0 α12 −α11 0

0 0 0 0

(11)

This causes the perturbation to take the form

hµν(t, z) =

0 0 0 0

0 α11 α12 0

0 α12 −α11 0

0 0 0 0

eiω(z−t) (12)

The part of the wave which is proportional to α11 is called plus polarized (+) and the

part of the wave which is proportional to α12 is called cross polarized (×).

Gravitational versus Electromagnetic Waves

There are a lot of similarities between gravitational waves and electromagnetic

waves. Both travel at the speed of light, both are transverse waves, both carry energy and

momentum, both don’t need a medium to travel, and both are emitted by accelerating

objects. However, gravitational and electromagnetic waves are fundamentally different

[1]. Some of the key differences are:

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• Interaction with matter. Electromagnetic waves interact strongly with matter but

gravitational waves do not. This makes gravitational waves harder to detect and

also, they do not carry much information regarding the material composition of

the source.

• Wavelength relative to source size. Wavelengths of electromagnetic waves are typ-

ically smaller than the source emitting them, allowing us to form an image of the

emitting source. In contrast, wavelengths of gravitational waves are usually larger

than the source.

• Phase coherence. Electromagnetic waves are generated by individual moving charges

whereas gravitational waves are generated by bulk motion of the source. This

causes the electromagnetic waves to be phase incoherent and gravitational waves

to be phase coherent.

• Field of view. Electromagnetic waves have a small field of view allowing us to get

a large amount of information by just observing a small region of the sky, whereas

gravitational waves cover almost the entire sky.

1.3 Sources of gravitational waves

Every accelerating massive object emits gravitational waves (provided it isn’t a spher-

ically symmetric motion), which means cars, trucks, planes and even humans can emit

gravitational waves. But the gravitational waves emitted by such sources are too faint

to be observed by our current detectors. Even the gravitational waves we detect from

highly energetic events, such as mergers of binary black hole systems, produce a strain

of the order of 10−21[4]. This greatly reduces the kind of events we can observe using

gravitational waves. We usually divide the viable sources of gravitational waves on the

basis of duration of the event and how well the waveform (strain-time series) produced

is known. Based on that we have four broad classifications:

1. Short-lived and well defined. Coalescence of compact binary objects is an

example. When a pair of compact objects such as black holes, neutron stars

or white dwarfs orbit around each other, they emit gravitational waves. As the

system emits gravitational waves, the orbital separation decreases. This phase

of the merger is called inspiral and it occurs over millions of years. As time

passes the objects orbit closer and closer together. As they move closer they start

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orbiting each other faster which causes them to emit stronger gravitational waves,

which causes them to lose more orbital energy, come even closer and finally merge.

Usually the end product of such mergers is a rotating black hole.

2. Short-lived and a poorly known. Such sources are also known as bursts and

refer to events of very short duration with no periodicity. Core collapse in massive

stars is an example. When a massive star undergoes supernova, it ejects mass

at really high speeds (up to 10% of the speed of light). However, if the mass

ejected is not spherically symmetrical, meaning the ejected mass is sent at different

speeds, it will result in a varying quadrupole moment resulting in the emission of

gravitational waves. To be able to detect gravitational waves generated by such

sources, we would need to know the details of the microphysics going on in the

source as the gravitational waves emitted by such sources are heavily influenced

by it.

3. Long-lived and well defined. Also, known as continuous wave sources. Spin-

ning neutron stars are an example. A mass distribution will emit gravitational

radiation only if there is an asymmetrical motion of individual masses. A spinning

neutron star is usually assumed be spherically symmetric because neutron stars are

dense objects with a strong gravitational pull that keeps them perfectly spherical.

However, sometimes small deformities on the surface called ”mountains”, which

are bumps extending no more than 10 centimeters (4 inches), are formed and can

produce enough asymmetry to produce detectable gravitational waves. The reason

is that the star has a quadrupole moment that changes with time, and since they

are rotating with speeds of the order of speed of light, they will emit gravitational

waves that can be detected. Such stars emit gravitational waves until the bumps

are smoothed out. One interesting thing about a spinning source is that it can emit

gravitational waves at a single frequency for a long time, so the signal builds up

in a narrow frequency bin. Hence in principle , they can be seen even at relatively

low amplitudes.

4. Long-lived and stochastic. Early cosmological expansion is an example. It

is theorized that during the early years of the universe, the universe underwent

rapid expansion in a short amount of time. If the expansion was not spherically

symmetrical, then gravitational waves must have been produced which should be

detectable today as a gravitational wave background. However, this background

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signal is too weak for any currently operational gravitational wave detector to

observe but there is a possibility of us detecting these kind of gravitational waves

with future detectors.

Out of all these sources, we have only been able to detect gravitational waves

from the coalescence of binary objects. We have detected gravitational waves from

binary black hole systems, binary black hole neutron star systems, and binary neutron

star systems. The reason is that binary systems are relatively easier to model, enabling

us to find gravitational waves hidden in the data observatories such as LIGO collect.

1.4 Detection of gravitational waves

As of now, Laser Interferometer Gravitational-wave Observatory (LIGO), the largest

ground based gravitational wave detector, is at the forefront of gravitational wave detec-

tion. LIGO consists of two laser interferometers, one at Livingston and one at Hanford

(approximately 3000km apart). While the detectors in themselves are an engineering

marvel, at their core they are just Michelson-Morley interferometers.

LIGO interferometers, similar to the Michelson-Morley interferometer, shoot a

beam of light towards a mirror, which in turn splits the light into two separate beams

perpendicular to each other. If gravitational waves are not passing through the obser-

vatory then the two beams merge in phase with each other. However, if gravitational

waves are passing through the observatory then that causes one of arms to get stretched

and one of the arms to get shorter, then vice versa, back and forth as long as the wave is

passing. This changes the distance travelled by each beam, causing the beams to arrive

at different times and merge out of phase. The difference in phase is measured, and

plotted by LIGO, and both detectors’ results are compared to verify that a gravitational

wave has actually passed through the detector [5].

While LIGO interferometers are Michelson-Morley interferometers at their core,

they differ from them in one major way. The arms in Michelson-Morley interferometers

are 1.3m long whereas the arms in the LIGO interferometers are 4.5km long, and the two

beams of light are reflected around 300 times in Fabry-Perot cavities before they merge

again. The cavities are formed by introducing an additional mirror placed in each arm

near the beam splitter, 4km from the mirror at the end of that arm. The reason for such

long arms and introducing Fabry-Perot cavities is to increase the distance travelled by

the light (from 4km to 1200km), thereby increasing the sensitivity of the interferometer.

However, one should note that even with such large distances the change in length of

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Figure 1: This figure shows the working of a LIGO interferometer.Courtesy Caltech/MIT/LIGO Laboratory

the arm caused by gravitational waves is as small as 10−19m (1/10, 000th the width of

the proton). This is one of the reasons LIGO detectors are limited by the kind of events

they can observe, the change in arm length caused by a gravitational wave source should

be significantly more than the background noise (usually seismic disturbances).

1.5 Binary systems

In this section, we will first mathematically describe an ordinary binary system to give

an idea of the mathematics behind gravitational wave generation and in the second part

we will elaborate on the different kind of compact binary mergers we observe.

1.5.1 Ordinary binary systems

Consider two stars far enough from each other that they can be considered as point

particles of mass m1 and m2 [6]. Let the frame we observe them in be the Center Of

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Figure 2: This figure shows the configuration of an ordinary binary system. x1, x2 and x3

correspond to x,y and z axes respectively. Reproduced from Gravitational-Wave Physicsand Astronomy by Jolien D. E. Creighton and Warren G. Anderson

Mass (COM) frame with the two bodies revolving in x-y plane with an angular speed

ω. In the COM frame, the two bodies are at a distance of r1 and r2 from the origin.

Let’s define orbital separation a = r1 + r2, total mass M = m1 + m2 and reduced mass

µ =m1m2/M. After defining these quantities we can express r1=a m2/M and r2=a m1/M.

Now we can calculate the components of the inertia tensor Iij using this equation

Iij =∑k

mk(|rk|2δij − xkixkj)

Using the previous equation, we have

I11 = m1[r1 cos(φ)]2 +m2[r2 cos(φ+ π)]2

= µa2 cos(φ)2 =1

2µa2(1 + cos(2φ))

(13a)

I22 = m1[r1 sin(φ)]2 +m2[r2 sin(φ+ π)]2

= µa2 sin(φ)2 =1

2µa2(1− cos(2φ))

(13b)

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I12 = I21 = m1r1 sin(φ)r1 cos(φ) +m2[r2 sin(φ+ π)][r2 cos(φ+ π)]

= µa2 sin(φ) cos(φ) =1

2µa2(sin(2φ))

(13c)

I31 = I32 = I33 = I23 = I13 = 0 (13d)

where φ = ωt. We take double time derivatives to calculate the metric perturbation hTT

as hTTij = 2Gc4rIij

I11 = −2µa2ω2 cos(2φ) (14a)

I22 = 2µa2ω2 cos(2φ) (14b)

I12 = I21 = −2µa2ω2 sin(2φ) (14c)

For an observer along the z-axis we have

hTTij = −4Gµa2ω2

c4r

cos(2φ) sin(2φ) 0

sin(2φ) − cos(2φ) 0

0 0 0

(15)

from the previous equation we can see

h+ = −4Gµa2ω2

c4rcos(2φ) (16a)

h× = −4Gµa2ω2

c4rsin(2φ) (16b)

We can observe that the frequency of the gravitational wave emitted is twice the

orbital frequency. A factor ν = aω is introduced to eliminate a and ω. From Kepler’s

third law of gravitation we have, GM = a3ω2, we have GMω = ν3. Therefore

ν = (πGMf)1/3 (17a)

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or in terms of orbital period P,

ν =

(2πGM

P

)1/3

(17b)

or in terms of orbital separation

ν =

√GM

a(17c)

We can express the two gravitational wave polarizations in terms of ν

h+ = −4Gµ

c2r

(vc

)2

cos(2φ) (18a)

h× = −4Gµ

c2r

(vc

)2

sin(2φ) (18b)

For an observer not on the orbital axis, which is usually the case, the gravitational

wave polarizations can be expressed in terms of the angle of inclination `

h+ = −2Gµ

c2r(1 + cos2 `)

(vc

)2

cos(2φ) (19a)

h= −4Gµ

c2rcos `

(vc

)2

sin(2φ) (19b)

The gravitational wave emitted is monochromatic at twice the orbital frequency. But the

system will keep on losing energy in the form of gravitational waves. We can calculate

energy lost by calculating the triple derivative of inertia tensor.

...I11 = −

...I22 = 4

G

c5

µ

M

(vc

)5

sin(2φ) (20a)

...I12 =

...I21 = −4

G

c5

µ

M

(vc

)5

cos(2φ) (20b)

The gravitational-wave luminosity (LGW = −dE/dt), where η = µ/M , is

LGW =G

5c5〈...I

211 +

...I

222 + 2

...I

212〉 =

32c5

5Gη2(vc

)10

(21)

1.5.2 Binary mergers

Gravitational waves detected on Earth arise due to mergers of three different compact

binary systems. They are (1) Binary Black Hole (BBH) systems (2) Binary Black hole

Neutron star systems (BHNS) and (3) Binary Neutron Star systems (BNS). Gravita-

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tional waves emitted by such systems have many qualitative similarities, one of them

being that all three mergers are comprised of three phases: inspiral, merger and ring-

down. During the inspiral phase the two objects revolve around each other, as they

revolve they lose energy in the form gravitational waves and as they lose energy, they

come closer to each other. This continues until they finally reach the merger phase.

During the merger phase the two objects merge, usually to form a Kerr black hole. Dur-

ing the ringdown phase, the perturbed and distorted end product emits a final burst of

gravitational radiation and quickly settles into a quiet, symmetric state. The inspiral

phase is characterized by continuous gravitational waves with increasing frequency and

increasing amplitude, the merger phase is characterized by an abrupt increase in am-

plitude and ringdown is characterized by abrupt decrease in amplitude (refer to Figure

3 for a template waveform). Despite the qualitative similarities, binary mergers can be

divided into three different categories depending on the type of compact objects the

systems are made of.

Binary Neutron Star systems: Gravitational waves emitted by the merger of neutron

star systems should be detectable by our current Earth based observatories, provided

these events happen in our galaxy or in relatively nearby ones. However, it might seem

that such events are unlikely. Such an event would not only require the formation of

two neutron stars but also for them to remain gravitationally bound and eventually

merge within the Hubble time (approximately 14 billion years). However, calculations

and observations show that such events are not only likely but also such events happen

often enough to produce one BNS merger each day in the observable universe [1].

The outcome of a BNS merger depends on the initial mass of the systems. Cur-

rently it is understood that if the mass of the system is lower than 2− 3 Msun then the

end result of the merger is a spinning neutron star. If the mass of the system is more

than 2− 3 Msun then the end result is expected to be a Kerr black hole. BNS mergers

can also produce short-period gamma ray bursts, which can be detected simultaneously

with gravitationally waves. Gravitational waves (GW170817) detected on August 17,

2017 were due to a binary neutron star merger. We not only detected gravitational

waves but also short-period gamma ray bursts associated with the merger and that has

led to the emergence of multi-messenger astronomy.

Binary Black Hole systems: Binary black hole mergers are strong sources of gravi-

tational waves. These mergers are much similar to BNS mergers but there is one major

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Figure 3: This figure shows the template waveform produced during a BBH merger.Similar to the merger the waveform is divided three parts: (1) Inspiral (2) Merger (3)Ringdown. The velocity is in terms of speed of light (c), Rs is the Schwarzschild radiusfor Sun’s mass and is equal to 3km.Reproduced from LIGO Scientific and Virgo Collaborations (2016), “Observation ofGravitational Waves from a Binary Black Hole Merger,” Physical Review Letters116:061102

difference, BBH mergers do not involve matter - just gravity, since all the mass of a black

hole is concentrated at the singularity. Hence a BBH merger is a much simpler event

to analyze compared to a BNS merger. The end product of a BBH merger is always a

Kerr black hole, which only needs mass and spin to be completely characterized. The

very first gravitational wave event (GW150914), observed on September 14, 2015, was

due to a pair of black holes of around 36 and 29 Msun.

Binary Black hole Neutron Star systems: Similar to the BBH and BNS systems,

there are evidences for the existence BHNS systems, and as this thesis is being written,

the news of the first BHNS merger (GW200105 and GW200115) being detected by LIGO

is being celebrated. Equations of state and observations place an upper limit of 2 Msun

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on the neutron star but there is no limit on the mass of the companion black hole. Due

to the presence of matter, the analysis of BHNS systems is much more complicated than

a BBH system. The end result of a BHNS merger is a rapidly spinning Kerr black hole.

1.6 Modeling gravitational waves

As LIGO detects gravitational waves, the data is analyzed to determine the parameters

of binary systems emitting them. The process of determining the parameters of binary

systems from gravitational waves is called parameter estimation. Parameters of a binary

system are divided into two sets, intrinsic parameters (8) and extrinsic parameters (9).

Intrinsic parameters determine the physics of the binary coalescence and the extrinsic

parameters are due to our position relative to the binary system.

Intrinsic parameters (λ)

• Mass ratio (q)

• Total mass (M)

• Spins (~S1, ~S2)

Extrinsic parameters (θ)

• Right ascension

• Declination

• Luminosity distance

• Coalescence time

• Three Euler angles characterizing orientation (e.g., inclination, orbital phase, and

polarization)

To determine parameters of binary systems using gravitational waves, we need

to be able to model binary systems. Due to the lack of analytical solutions to two-

body problems in General Relativity, physicists end up using analytical and numerical

approximations to model binary systems. Some of these approximations are:

1. Post-Newtonian Theory. The Post-Newtonian (PN) formalism is an approx-

imation to General Relativity (GR) in the slow-motion, weak field regime. It is

suitable for explaining the inspiral regime of the coalescence, but it breaks down

during the merger and ringdown phases of the merger.

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2. Numerical Relativity. Numerical Relativity involves solving Einstein’s equa-

tions numerically to study the dynamics of the binary system and hence gravita-

tional waves. It is the most accurate way of modeling gravitational waves but it

is computationally expensive [7, 8].

3. Effective-One-Body. The Effective-One-Body formalism is also an approxima-

tion to GR. It is based on an ansatz that the binary system can be reduced to a

test particle with the reduced mass µ moving in an effective Kerr (rotating black

hole) background spacetime. Similar to PN, it is able to explain the inspiral phase

of the merger, but breaks down during the merger and ringdown phases of the

coalescence.

4. Phenomenological Waveforms. Compared to the previously mentioned for-

malisms, this takes a different approach. Instead of focusing on the dynamics of

gravitational wave source, it models the gravitational wave directly. Phenomeno-

logical waveform models are constructed in the frequency domain, which makes

them computationally fast to evaluate.

5. Numerical Relativity Surrogates. This approach involves interpolation be-

tween different Numerical Relativity solutions. This is the most accurate way

after Numerical Relativity but is limited by the number of Numerical Relativity

solutions .

1.7 Motivation and brief discussion

Numerical Relativity (NR) is the only ab-initio approach that produces waveforms from

the merger of a binary system accurately [9]. However, NR simulations are computa-

tionally expensive with a single simulation taking anything from weeks to months to

finish. Parameter estimation of gravitational wave signals involves the use of Monte

Carlo Markov Chain algorithms and these algorithms go through thousands of points in

parameter space before they finally converge onto the most probable point. This makes

the NR time-inefficient, leaving us with approximated models to perform parameter es-

timation. However, each of these approximations results in different template families

which in turn leads to waveform systematics. Errors and biases completely attributable

to waveform modeling choices are called Waveform Systematics [10]. As illustrated most

recently by GW190521 [11, 12], GW190814 [13], GW190412 [14], and the discussion in

GWTC-2 [15], these approximations disagree more than enough to produce noticeable

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differences, consistent with prior work [16, 17, 18]. Despite the ongoing generation of new

waveforms with increased accuracy, these previous investigations suggest that waveform

model systematics can remain a limiting factor in inferences about individual events and

populations. And as we are improving the sensitivity of detectors, the study of wave-

form systematics will become even more important. The main aim of this thesis to study

waveform systematics and implement a technique to marginalize over these waveform

systematics.

The remainder of this thesis is outlined as follows: Chapter 2 of this thesis fol-

lows our paper Assessing and Marginalizing over compact binary coalescence waveform

systematics using RIFT which was published in Physical Review D. In Chapter 3 we

extend our technique of marginalizing over waveform systematics to include dynamically

changing weights associated with each model. In Chapter 4 we discuss the conclusions

of this thesis.

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2 Assessing and Marginalizing over compact binary

coalescence waveform systematics using RIFT

2.1 Bayes’ theorem

After an observatory, such as LIGO, detects gravitational waves, the data is processed

and then made to pass through a parameter inference/estimation algorithm. The param-

eter estimation algorithm explores the parameter space, generating gravitational wave

signals for points in parameter space and then comparing them against the detected GW

signal. This enables the algorithm to find the set of parameters that best explain the

detected GW. For this work, we have used RIFT which is one such parameter inference

algorithm and is discussed in detail in section 2.2.

Parameter estimation algorithms are usually Bayesian in nature, that means they

employ Bayes’ theorem to infer parameters of a binary system from the gravitational

wave signal. Bayes’ theorem is used to calculate probability of an event when we have

some prior knowledge of conditions that are related to the event [19]. Mathematically,

Bayes’ theorem is given by this formula:

P (A|B) =P (B|A)P (A)

P (B)

here, P (A) is the probability of event A, P(B) is the probability of event B, P (A|B) is

the probability of A given B is already true and P (B|A) is the probability of event B

given A is already true.

In the context of gravitational wave data analysis, we express the the Bayes’ theorem

as:

P (λ|d) =P (d|λ)P (λ)

P (d)(22)

here, λ is the set of parameters, d is the data we have observed. P (d|λ) is called the

likelihood which we calculate using our models, P (λ) is called the prior and is usually our

guess on how likely that set of parameters is based on our earlier observations, P (d) is

called the evidence and is just a normalizing constant, and P (λ|d) is called the posterior

and is usually the probability we are interested in. Parameter inference algorithms such

as RIFT use equation (22) to find the most likely set of parameters which would generate

the detected gravitational waves.

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2.2 RIFT review

A coalescing compact binary in a quasicircular orbit can be completely characterized by

its intrinsic and extrinsic parameters. By intrinsic parameters we refer to the binary’s

masses mi, spins, and any quantities characterizing matter in the system. For simplicity

and reduced computational overhead, in this work we assume all compact object spins are

aligned with the orbital angular momentum. This simplifying measure greatly reduces

the computational time, as the code has to got through a four dimensional parameter

space instead of eight dimensional parameter space. By extrinsic parameters we refer

to the seven numbers needed to characterize its spacetime location and orientation. We

will express masses in solar mass units and dimensionless nonprecessing spins in terms of

cartesian components aligned with the orbital angular momentum χi,z. We will use λ, θ

to refer to intrinsic and extrinsic parameters, respectively. Specifically the likelihood of

the data given gaussian noise has the form (up to normalization)

lnL(λ; θ) = −1

2

∑k

〈hk(λ, θ)− dk|hk(λ, θ)− dk〉k − 〈dk|dk〉k, (23)

where hk are the predicted response of the kth detector due to a source with param-

eters (λ, θ) and dk are the detector data in each instrument k; λ denotes the combi-

nation of redshifted mass Mz and the remaining parameters needed to uniquely spec-

ify the binary’s dynamics; θ represents the seven extrinsic parameters; and 〈a|b〉k ≡∫∞−∞ 2dfa(f)∗b(f)/Sh,k(|f |) is an inner product implied by the kth detector’s noise power

spectrum Sh,k(f) (a and b are the Fourier transform of a and b respectively).

Since we are interested in the physics of the binary system, we will eliminate the

extrinsic variables characterizing the spacetime coordinates and orientation of the binary

relative to the Earth by integrating over them. To do this we use ILE, which is a specific

algorithm to “integrate over extrinsic parameters” and provides a straightforward and

efficient mechanism to compare any specific candidate gravitational wave source with

real or synthetic data. The likelihood obtained after marginalizing over the extrinsic

variables is called the marginalized likelihood.

RIFT [20] consists of a two-stage iterative process to interpret gravitational wave

data d via comparison to predicted gravitational wave signals h(λ, θ).

First stage : In this stage, for each λα from some proposed “grid” α = 1, 2, . . . N

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Figure 4: This figure shows inferred posterior parameter distributions for a non-precessing BBH source using RIFT. The blue crosshairs indicate true parameter valuesand contours in two dimensional plots (bottom left) indicate the 90% credible region asestimated by each iteration. The colored contours correspond to different iterations.

of candidate parameters, RIFT computes a marginal likelihood

Lmarg ≡∫L(λ, θ)p(θ)dθ (24)

from the likelihood L(λ, θ) of the gravitational wave signal in the multi-detector network,

accounting for detector response; see the RIFT paper for a more detailed specification

[20].

Second stage : In this stage, RIFT performs two tasks. First, it generates an

approximation to L(λ) based on its accumulated archived knowledge of marginal likeli-

hood evaluations (λα,Lα). This approximation can be generated by gaussian processes,

random forests, or other suitable approximation techniques. Second, using this approx-

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imation, it generates the (detector-frame) posterior distribution

ppost =Lmarg(λ)p(λ)∫dλLmarg(λ)p(λ)

. (25)

where prior p(λ) is the prior on intrinsic parameters like mass and spin. The posterior

is produced by performing a Monte Carlo integral: the evaluation points and weights in

that integral are weighted posterior samples, which are fairly resampled to generate con-

ventional independent, identically-distributed “posterior samples.” For further details

on RIFT’s technical underpinnings and performance, see [20, 21, 22].

2.3 Waveform models

We have used the waveform models to generate synthetic data and to perform parameter

estimation on such data. Most of the models we have until now come from three families,

Effective One Body (EOB) models, phenomenological frequency-domain inspiral and

merger models, and and surrogate waveforms, directly calibrated to numerical relativity.

For our work, we employ two well-studied models for non-precessing binaries, whose

differences are known to be significant. We use SEOBNRv4 [23], an effective-one-

body model for quasi-circular inspiral, and IMRPhenomD [24, 25], a phenomenological

frequency-domain inspiral-merger-ringdown model.

SEOBNRv4 models the inspiral and spin dynamics of coalescing binaries via an

ansatz for the two-body Hamiltonian [26], whose corresponding equations of motion are

numerically solved in the time domain. For non-precessing binaries, outgoing gravita-

tional radiation during the inspiral phase is generated using an ansatz for resumming

the post-Newtonian expressions for outgoing radiation including non-quasicircular cor-

rections, for the leading-order ` = 2 subspace. For the merger phase of non-precessing

binaries, the gravitational radiation is generated via a resummation of many quasinor-

mal modes, with coefficients chosen to ensure smoothness. The final BH’s mass and

spin, as well as some parameters in the non-precessing inspiral model, are generated via

calibration to numerical relativity simulations of BBH mergers.

The IMRPhenomD model is a part of an approach that attempts to approx-

imate the leading-order (` = 2) gravitational wave radiation using phenomenological

fits to the Fourier transform of the gravitational wave strain, computed from numer-

ical relativity simulations, effective-one-body waveforms and post-newtonian calcula-

tion [27, 28, 29]. Also using information about the final BH state, this phenomenological

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frequency-domain approach matches standard approximations for the post-Newtonian

gravitational wave phase to an approximate, theoretically-motivated spectrum charac-

terizing merger and ringdown.

2.4 Fiducial synthetic sources and P-P tests

We only explored the impact of systematics over a limited fiducial population. Specif-

ically, we consider a universe of synthetic signals for 3-detector networks, with masses

drawn uniformly in mi in the region bounded by M/M� ∈ [30, 60] and η ∈ [0.2, 0.25]

and with extrinsic parameters drawn uniformly in sky position and isotropically in Eu-

ler angles, with source luminosity distances drawn proportional to d2L between 1.5Gpc

and 4Gpc. These bounds are expressed in terms of M = (m1m2)3/5/(m1 + m2)1/5 and

η = m1m2/(m1 + m2)2, and encompass the detector-frame parameters of many mas-

sive binary black holes seen in GWTC-1 [30] and GWTC-2 [15]. All our sources have

non-precessing spins, with each component assumed to be uniform between [−1, 1]. For

complete reproducibility, we use SEOBNRv4 and IMRPhenomD, starting the signal evo-

lution at 18Hz but the likelihood integration at 20Hz, performing all analysis with

4096Hz timeseries in Gaussian noise with known advanced LIGO design PSDs [31]. For

each synthetic event and for each interferometer, the same noise realization is used for

both waveform approximations. Ensuring convergence of the analyses, the differences

between them therefore arise solely due to waveform systematics. For context, Figure

5 shows the cumulative SNR distribution of one specific synthetic population gener-

ated from this distribution. Though a small fraction have substantial signal amplitudes,

most events are near or below the level of typical detection candidates. By using a very

modest-amplitude population to assess the impact of waveform systematics, we demon-

strate their immediate impact on the kinds of analyses currently being performed on

real observations, let alone future studies.

One way to assess the performance of parameter inference is a probability-probability

plots (usually denoted P-P plot) [32]. Using RIFT on each source k, with true parameters

λk, we estimate the fraction of the posterior distributions which is below the true source

value λk,α [Pk,α(< λk,α)] for each intrinsic parameter α, again assuming all sources have

zero spin. After reindexing the sources so Pk,α(λk,α) increases with k for some fixed α,

the top panel of Figure 6 shows a plot of k/N versus Pk(λk,α) for all binary parameters.

For the top panel, both injections and inference are performed with the same model,

and the recovered probability distribution is consistent with P (< p) = p, as expected.

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5 10 15 20 25 30 35SNR

0.0

0.2

0.4

0.6

0.8

1.0

P(SN

R)zero-noise SNR

Figure 5: Cumulative SNR distribution for a synthetic population of 100 events drawnfrom the fiducial BBH population described in Section 2.4. To avoid ambiguity, thisfigure shows the expected SNR (i.e., the SNR evaluated using a zero-noise realization).

2.5 Zero noise runs to assess systematic biases

Our synthetic data consists of expected detector responses h(t) superimposed on detector

noise realization n(t). The recovered posterior distribution’s properties and in particular

maximum-likelihood parameters depend on the specific noise realization used. To dis-

entangle the deterministic effects of waveform systematics from the stochastic impact of

different noise realizations, we also repeat our analyses with the ”zero noise” realization:

n(t) = 0.

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0.0 0.2 0.4 0.6 0.8 1.0P(xinj)

0.0

0.2

0.4

0.6

0.8

1.0P

mcqs1zs2z

0.0 0.2 0.4 0.6 0.8 1.0P(xinj)

0.0

0.2

0.4

0.6

0.8

1.0

P

mcqs1zs2z

Figure 6: P-P plot of events injected with SEOBNRv4 and recovered with SEOB-NRv4(top panel) and IMRPhenomD(bottom panel) waveform. The dashed line indi-cates the 90% credible interval expected for a cumulative distribution drawn from 100uniformly-distributed samples.

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2.6 Marginalizing over waveform systematics

Suppose we have two models A and B for GW strain, and use them to interpret a

particular GW source. We have prior probabilities p(A|λ) and p(B|λ), characterizing

our relative confidence in these two models for a source with parameters λ. Suppose

we have produced a RIFT analysis with each model for this event, and have marginal

likelihood functions LA(λ) and LB(λ) evaluated at a single point λ. We can therefore

construct the marginal likelihood for λ by averaging over both models:

Lav(λ) = p(A|λ)LA(λ) + p(B|λ)LB(λ) (26)

For simplicity the calculations in this work always adopt p(A|λ) = p(B|λ) = 1/2. We

can therefore transparently integrate multi-model inference into RIFT as follows. We

assume we have a single grid of points λk such that both (λk,LA(λk) and (λk,LB(λk)

can be interpolated to produce reliable likelihoods and thus posterior distributions pA(λ)

and pB(λ), respectively. At each point λk we therefore construct Lav(λk) by the above

procedure. We then interpolate to approximate L(λ) versus the continuous parameters

λ.

Operationally speaking, we construct model-averaged marginal likelihoods by the

following procedure. First, we construct a fiducial grid for models A and B, for example

by joining the grids used to independently analyze A and B. We use an algorithm

to integrate the extrinsic likelihood (ILE), a process where each candidate GW signal

is compared to a regular grid of candidate source parameters to produce an array of

candidate likelihood values, to evaluate LA(λk) and LB(λk) on this grid [33, 20]. We

construct Lav(λk) as above. We use the combinations (λk,Lav) with an algorithm to

construct the intrinsic posterior (CIP) from this sampled data, to construct a model-

averaged posterior distribution [20].

Our procedure bears considerable resemblance to the approach suggested by Ash-

ton and Khan [34], but we have organized the calculation differently. In that approach,

AK used the evidences ZA =∫LAp(λ)dλ and ZB for the two waveform models. While

we can compute both quantities with very high accuracy, we prefer to directly average

between waveform models at the same choice of intrinsic parameters (i.e., via Eq. (26))

, to insure that marginalization over waveform models is completely decoupled from the

interpolation techniques used to construct L from the sampled data.

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Injection: Unknown Recovery: SEOBNRv4

Injection: Unknown Recovery: IMRPhenomD

Generated on same grid

Likelihood values for points in the grid

Likelihood values for points in the grid

Calculate average likelihood values

Model averaged posterior sample

Integrate over extrinsic variables

Integrate over

extrinsic variables

Constructing the intrinsic posterior distribution

𝐿𝑎𝑣() = 𝑝(𝐴)𝐿𝐴() + 𝑝(𝐵)𝐿𝐵()

100 non- precessing BBH

events

Figure 7: This flow chart shows the steps we followed to implement our technique ofmarginalizing over waveform systematics using RIFT.

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10 3 10 2 10 1 100 101

KL divergence

10 1

100

101

102

103

max

lnL

Figure 8: Figure showing KL-divergences between the two waveform models versus thelog of the maximum likelihood for the combined posteriors of M, q and χeff .

2.7 Results

Using our fiducial BBH population, we generated 100 synthetic signals using IMR-

PhenomD, and another 100 synthetic signals with SEOBNRv4. For each signal, we

performed parameter inference with both IMRPhenomD and SEOBNRv4. These

inferences allow us both to assess the impact of waveform systematics in our fiducial

population, and mitigate them.

2.7.1 Demonstrating and quantifying waveform systematics

The P-P plot provides the most compelling demonstration of waveform systematics’

pernicious impact. Ideally, when recovering a known model and a known population, we

expect to recover the injected values as often as they occur, producing a diagonal P-P

plot. The top panel of Figure 6 shows precisely what we expect, when we inject and

recover with the same model (here, SEOBNRv4).

By contrast, the bottom panel shows a P-P plot generated using inference from

IMRPhenomD on the same SEOBNRv4 injections. The P-P plot is considerably non-

diagonal, reflecting frequent and substantial parameter biases in our fiducial population.

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1.5 1.0 0.5 0.0 0.5

10 1

100

101

0.50 0.25 0.00 0.25 0.50

10 1

100

101q

1.5 1.0 0.5 0.0 0.5scaled difference

10 1

100

101

BF

eff

Figure 9: Figure showing Bayes factor (BF) for SEOBNRv4 versus IMRPhenomDplotted against differences between the SEOBNRv4 and IMRPhenomD waveformsfor parameters M, q and χeff .

30 35 40 45 50 55 60 650.2

0.3

0.4

0.5

0.6

0.7

0.8

0.9

1.0

q

0.6

0.4

0.2

0.0

0.2

0.4

0.6

0.8

eff

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0.2 0.4 0.6 0.8 1.0q

0.75

0.50

0.25

0.00

0.25

0.50

0.75

1.00

eff

35

40

45

50

55

30 35 40 45 50 55 60

0.75

0.50

0.25

0.00

0.25

0.50

0.75

1.00

eff

0.4

0.5

0.6

0.7

0.8

0.9

q

Figure 10: Vector plot showing amplitude-scaled offsets between SEOBNRv4 and IM-RPhenomD for parameters M and q, M and χeff and q and χeff as a function of therespective parameters with color map being the value of the parameter mentioned onthe color scale.

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Parameter biases introduced by waveform systematics vary in magnitude and

direction over the parameter space. To illustrate these offsets for the parameters x =

M, q, χeff , we’ve evaluated the parameter shift ∆x between the mean inferred with IMR-

PhenomD and the mean inferred with SEOBNRv4, relative to σρ, which is a product

of ρ (the signal-to-noise ratio, a measure of the signal amplitude) and the statistical error

(as measured by the standard deviation σ of the posterior of the parameter x in ques-

tion). [The combination σρ is approximately independent of signal amplitude, allowing

us to measure the effect of waveform systematics for a fiducial amplitude.] Figure 10

shows a vector plot of these scaled offsets ∆x/ρσ, as a function of two of the parameters

at a time. The length of the arrow corresponds to the scaled shifts in the parameters

M, q and χeff , plotted against the injected parameter values. The color scale shows the

remaining parameter.

First two vector plots in Figure 10 show that shifts in q = m2/m1, χeff =

(m1χ1,z + m2χ2,z)/(m1 + m2) are substantial. Parameter shifts for q generally increase

with χeff . Shifts in χeff are generally positive for positive χeff , negative for negative χeff ,

and strongly dependent on mass ratio, with more substantial shifts at either comparable

mass or at very high mass ratio, respectively. In both cases, chirp mass M has modest

impact, with somewhat larger shifts occurring at somewhat larger values of chirp mass.

Most extreme waveform systematics seem to be associated with large mass ratio.

Relative differences in mean value only imperfectly capture the differences be-

tween the two posteriors. As a sharper diagnostic that includes parameter correlations,

we use the mean and covariance of each distribution in M, q, χeff to generate a local

gaussian approximation for each posterior, and then compute the Kullback–Leibler (KL)

divergence between these two gaussian approximations [20]. We expect more substantial

differences and thus larger KL divergence for stronger signals, whose posteriors are more

sharply constrained. To corroborate our intuition, Figure 8 shows a scatterplot, with

these KL divergences on the horizontal axis and the largest value of lnL on the verti-

cal axis. As expected, for the strongest signals, differences between the two waveform

models are the most pronounced.

One might expect that large parameter offsets are more likely to occur when

the data favors one model or another. While conceivably true asymptotically, for our

specific synthetic population, we don’t find a strong correlation between the Bayes factor

(ZSEOBNRv4/ZIMRPhenomD) and any parameter offsets. Figure 9 shows this Bayes factor

(BF) plotted versus the scaled parameter offsets in M, q, χeff . Large offsets can occur

without the data more strongly favoring one model or the other, and vice versa.

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Figure 11: Example of a model averaged result. The blue and black curves show the1D marginal distributions and 2D 90% credibles for SEOBNRv4 and IMRPhenomDinferences, respectively. The green curves show the corresponding model-averaged result.

2.7.2 A P-P plot test for marginalizing over waveform errors

We test our model-averaged waveform procedure using a full synthetic P-P plot proce-

dure. Specifically, we use the ns = 100 synthetic source parameters. For each source,

we pick one waveform model A,B with probabilities p(A), p(B), and use it to generate

the signal. We then analyze the signal using the model-averaged procedure described

above.

As a concrete example, Figure 11 shows our analysis of one fiducial event in our

synthetic sample. The colored points show likelihood evaluations, with color scale corre-

sponding to the marginalized likelihood evaluated with IMRPhenomD. The blue and

black contours show the 90% credible intervals for SEOBNRv4 and IMRPhenomD,

respectively; the two posteriors differ substantially (i.e., the shift in mean in m1 is of or-

der one standard deviation), illustrating the impact of model systematics on parameter

inference. The green contour shows our model-marginalized posterior.

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0.0 0.2 0.4 0.6 0.8 1.0P(xinj)

0.0

0.2

0.4

0.6

0.8

1.0

P

mcqs1zs2z

Figure 12: P-P plot test for our model-marginalized procedure.

For comparison, the cross shows the injected source parameters, and the model

was IMRPhenomD. Figure 12 shows one P-P plot corresponding to applying our model-

marginalized procedure to a population where each source is randomly selected from

either IMRPhenomD or SEOBNRv4. The dotted line shows a 90% frequentist interval

for the largest of four random cumulative distributions. This figure shows our P-P plots

are consistent with the diagonal, as desired.

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3 Numerical Relativity weighted model marginal-

ization

In our technique of marginalizing over waveform systematics, we have weights or priors

associated with each model when computing the average likelihood (refer to equation

(26)). In the results of the earlier chapter, we had assumed the priors p(A) and p(B) to

be constant. However, studies [35, 36] have shown that different models work best in dif-

ferent regions of parameter space, suggesting a dependence of these priors on parameters

λ. In this chapter, we develop a way to include this dependency in our technique.

3.1 Mismatch, overlap and calculating weights

Several previous investigations [37, 38, 39, 40, 41, 42, 43] have argued that the magnitude

of systematic biases are related to the model-model mismatch, a simple inner-product-

based estimate of waveform similarity between two model predictions h1(λ) and h2(λ)

at identical model parameters λ:

M(λ) = 1−maxtc,φc

|⟨h1|ei(2πftc+φc)h2

⟩|

|h1||h2|(27)

In this expression, the inner product 〈a|b〉k ≡∫∞−∞ 2dfa(f)∗b(f)/Sh,k(|f |) is im-

plied by the kth detector’s noise power spectrum Sh,k(f), which for the purposes of

waveform similarity is assumed to be the advanced LIGO instrument, H1. In practice

we adopt a low-frequency cutoff fmin so all inner products are modified to

〈a|b〉k ≡ 2

∫|f |>fmin

df[a(f)]∗b(f)

Sh,k(|f |). (28)

Figure 13 shows the distribution of mismatches for our synthetic population,

where h1 is generated using SEOBNRv4 and h2 with IMRPhenomD. For simplicity, we

regenerate all signals at zero inclination, to avoid polarization-related effects associated

with the precise emission direction. For our fiducial compact binary population, the

mismatches between these two models are typically below 10−2, consistent with previous

reports on systematic differences between these two waveforms and with their similarity

to even more accurate models and simulations [23, 44, 18]

We can extend equation (27) to find the mismatch between a model and Numer-

32

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Aasim Zahoor Jan Master’s Thesis

10 2

Mismatch

0.2

0.4

0.6

0.8

1.0

CDF

Figure 13: Cumulative Mismatch Distribution for all the synthetic sources in our popu-lation. We evaluate the GW strain along the z axis using SEOBNRv4 and IMRPhe-nomDand then compute the mismatch between them. This figure shows the cumulativedistribution of these mismatches, most of which are slightly less than 10−2.

ical Relativity. Equation (27) can also be written as:

M(λ) = 1− overlap(λ) (29)

or

overlap(λ) = maxtc,φc

|⟨h1|ei(2πftc+φc)h2

⟩|

|h1||h2|(30)

The overlap value tells us how much a model agrees with Numerical Relativity

for a given set of parameters, with the maximum value being 1 and minimum being 0.

After calculating the overlap values, we use equation 31 to find the the weight associated

with each model when combining the likelihoods.

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Figure 14: Continued to next page.

For the results in the previous chapter, we had assumed p(A|λ) and p(B|λ) to

be constant and equal to 12. However, we can improve our process of marginalizing over

waveform systematics by dynamically changing p(A|λ) and p(B|λ) as different models

34

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Figure 14: These figures show the interpolated overlap values for different mass ratios(q) and spin values (S1z, S2z). For these figures, overlap values are on y-axis and m2 ison x-axis. The red line represents the maximum possible overlap value. For the firstfour figures, q=2 and spin value goes from 0 to 0.75 with the increment size being 0.25.This is repeated for q= 2.5 and q=3. Since all our results are for non-precessing binarysystems, S1x = S2x = S1y = S2y = 0.

35

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work best in different regions of parameter space. Figure 14 shows the overlap values of

IMRPhenomD and SEOBNRv4 with NR and we can see that parameters determine

which model has a higher overlap value. The value of p(A|λ) and p(B|λ) is made to

depend on overlap value and is calculated using the equation:

p(Xk|λ) =exp(−(1− overlapXk) ∗ lnLref )∑k exp(−(1− overlapXk) ∗ lnLref )

(31)

here Xk is the kth model, overlapXk is the overlap of the kth model with NR for the

parameter values λ, and lnLref is the maximum likelihood value calculated by any of

the two models for an event.

3.2 Nearest neighbor interpolator

To calculate the overlap of a model with NR, we are restricted by the number of NR

solutions we have. To find overlap values for a set of parameters for which NR solutions

do not exist, we use the nearest-neighbor method of interpolation.

Nearest-neighbor interpolation is a simple method of multivariate interpolation

in one or more dimensions. The nearest neighbor interpolator selects the value of the

nearest point and does not consider the values of neighboring points. The training

data for the interpolator was created by calculating overlap values of IMRPhenomD

and SEOBNRv4 with the available NR simulations. That was achieved by using 923

aligned NR simulations from Rochester Institute of Technology’s library and 244 aligned

NR simulations from LIGO Scientific Collaboration’s library.

3.3 Results

We test our NR weighted model marginalization procedure using a full synthetic P-P

plot procedure. Specifically, we use the ns = 100 synthetic source parameters. For each

source, we pick one waveform model A,B with probabilities p(A), p(B), and use it to

generate the signal. We then analyze the signal using the model-averaged procedure as

described earlier.

As a concrete example, Figure 15 shows our analysis of one fiducial event in our

synthetic sample. The colored points show likelihood evaluations, with the color scale

corresponding to the marginalized likelihood evaluated with IMRPhenomD. The blue

and black contours show the 90% credible intervals for SEOBNRv4 and IMRPhe-

nomD, respectively; the two posteriors differ substantially, illustrating the impact of

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Figure 15: Example of a NR weighted model averaged result. The blue and blackcurves show the 1D marginal distributions and 2D 90% credibles for SEOBNRv4 andIMRPhenomD inferences, respectively. The green curves show the corresponding NRweighted result.

model systematics on parameter inference. The green contour shows our NR weighted

model-marginalized posterior.

For comparison, the cross shows the injected source parameters, and the model

was IMRPhenomD.

Figure 16 shows one P-P plot corresponding to applying our NR weighted model-

marginalized procedure to a population where each source is randomly selected from

either IMRPhenomD or SEOBNRv4. The dotted line shows a 90% frequentist interval

for the largest of four random cumulative distributions. This figure shows our P-P plots

are consistent with the diagonal, as desired.

37

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0.0 0.2 0.4 0.6 0.8 1.0P(xinj)

0.0

0.2

0.4

0.6

0.8

1.0

P

mcqs1zs2z

Figure 16: P-P plot test for our NR-weighted model-marginalized procedure.

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4 Conclusions and Discussions

4.1 Future work

Using our technique, we have been able to marginalize over waveform systematics but the

models used in this work are older models. So the next step would be to include newer

models and also to generalize the technique to include more than two models, as many

as the user feels necessary. We have also introduced parameter-dependent weighting of

the waveforms while calculating the average likelihood, but due to a limited number of

Numerical Relativity solutions we used the nearest neighbor interpolation to interpolate

between different overlap values. The next step would be to use a more efficient and

accurate interpolator such as Gaussian process interpolator.

4.2 Conclusions

Many waveform models exist currently that describe compact binary coalescences. Even

though these are derived by solving Einstein’s equations, the various analytical or numer-

ical approximations considered bring in differences and affect the parameter estimation

process leading to biased interpretation of results. Averaging over the waveform mod-

els can mitigate these biases that arise precisely due to the various differences in the

waveform models.

In this work, we performed simple tests which reproduce significant differences

between the models SEOBNRv4 and IMRPhenomD, and can be extended to other

available waveforms easily using RIFT, an efficient parameter estimation engine. The

Probability-Probability (P-P) plot test, a commonly used statistical test, can be used

to confirm differences between waveform models and as shown in Fig. 6, parameter

estimation performed using a model different from the injected model, gives a non-

diagonal P-P plot for most parameters. We calculated the magnitude and direction

of the offsets introduced due to using a waveform model different from the injected

model, and these differences are higher for extreme case scenarios, as expected. A linear

correlation between the KL divergence computed for the two models and the log of the

maximum likelihood of the injected model shows that a high-SNR signal will have larger

differences in the inferred parameter from various models. Because the most informative

signals exhibit the largest parameter biases, waveform systematics have the potential to

strongly contaminate population inference. Most importantly, we also demonstrated a

method to mitigate these waveform systematics by marginalizing over the models used

39

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Aasim Zahoor Jan Master’s Thesis

for parameter estimation analyses.

Our method requires as input some prior probabilities p(Xk|λ) for different wave-

form models Xk. One way these prior probabilities could be selected is by waveform

faithfulness studies between models and numerical relativity simulations. These fidelity

studies inevitably suggest waveform models vary in reliability over their parameter space

[35, 36], suggesting p(Xk|λ) will depend nontrivially on λ. We have developed a proce-

dure to include the dependency of these priors on λ in our work. RIFT performs these

calculations at minimal added computational expense.

Other techniques have been proposed to marginalize over waveform model system-

atics. Notably, several groups have proposed using the error estimates provided by their

model regressions (e.g., the gaussian process error) [45]. Relative to regression-based

methods, our method has two notable advantages. Our method can be immediately

generalized to include multiple waveform models. We have also introduced parameter-

dependent weighting of the likelihood from a waveform since different waveforms are

accurate in different regimes. No other model-marginalization technique can presently

provide this level of control.

40

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