2 Non-linear Iteration of the Vacuum Field Equations
2.1 Einstein’s field equations
The field equations of general relativity are obtained by varying the space-time metric in the famous
Einstein–Hilbert action,






In most of this paper we adopt the conditions of harmonic coordinates, sometimes also called de Donder coordinates. We define, as a basic variable, the gravitational-field amplitude
where









The Einstein field equations in harmonic coordinates can be written in the form of inhomogeneous flat d’Alembertian equations,
where





As is clear from this expression, is made of terms at least quadratic in the gravitational-field
strength
and its first and second space-time derivatives. In the following, for the highest
post-Newtonian order that we shall consider, we will need the quadratic, cubic and quartic pieces of
;
with obvious notation, we can write them as
As we said, the condition (21*) is equivalent to the matter equations of motion, in the sense of the
conservation of the total pseudo-tensor ,
- The matter stress-energy tensor
is of spatially compact support, i.e., can be enclosed into some time-like world tube, say
, where
is the harmonic-coordinate radial distance. Outside the domain of the source, when
, the gravitational source term, according to Eq. (27*), is divergence-free,
- The matter distribution inside the source is smooth:
.16 We have in mind a smooth hydrodynamical fluid system, without any singularities nor shocks (a priori), that is described by some Euler-type equations including high relativistic corrections. In particular, we exclude from the start the presence of any black holes; however, we shall return to this question in Part B when we look for a model describing compact objects;
- The source is post-Newtonian in the sense of the existence of the small parameter defined by Eq. (1*). For such a source we assume the legitimacy of the method of matched asymptotic expansions for identifying the inner post-Newtonian field and the outer multipolar decomposition in the source’s exterior near zone;
- The gravitational field has been independent of time (stationary) in some remote past, i.e., before
some finite instant
in the past, namely
The latter condition is a means to impose, by brute force, the famous no-incoming radiation condition,
ensuring that the matter source is isolated from the rest of the Universe and does not receive any radiation
from infinity. Ideally, the no-incoming radiation condition should be imposed at past null infinity. As we
shall see, this condition entirely fixes the radiation reaction forces inside the isolated source. We shall later
argue (see Section 3.2) that our condition of stationarity in the past (29*), although weaker than the ideal
no-incoming radiation condition, does not entail any physical restriction on the general validity of the
formulas we derive. Even more, the condition (29*) is actually better suited in the case of real
astrophysical sources like inspiralling compact binaries, for which we do not know the details of the
initial formation and remote past evolution. In practice the initial instant can be set
right after the explosions of the two supernovæ yielding the formation of the compact binary
system.
Subject to the past-stationarity condition (29*), the differential equations (22*) can be written equivalently into the form of the integro-differential equations
containing the usual retarded inverse d’Alembertian integral operator, given by extending over the whole three-dimensional space
2.2 Linearized vacuum equations
In what follows we solve the field equations (21*) – (22*), in the vacuum region outside the compact-support
source, in the form of a formal non-linearity or post-Minkowskian expansion, considering the field variable
as a non-linear metric perturbation of Minkowski space-time. At the linearized level (or
first-post-Minkowskian approximation), we write:






We want to solve those equations by means of an infinite multipolar series valid outside a time-like world
tube containing the source. Indeed the multipole expansion is the appropriate method for describing the
physics of the source as seen from its exterior (). On the other hand, the post-Minkowskian series is
physically valid in the weak-field region, which surely includes the exterior of any source, starting at a
sufficiently large distance. For post-Newtonian sources the exterior weak-field region, where both multipole
and post-Minkowskian expansions are valid, simply coincides with the exterior region
. It is
therefore quite natural, and even, one would say inescapable when considering general sources, to combine
the post-Minkowskian approximation with the multipole decomposition. This is the original idea of the
“double-expansion” series of Bonnor and collaborators [94, 95, 96, 251], which combines the
-expansion (or
-expansion in their notation) with the
-expansion (equivalent to the
multipole expansion, since the
-th order multipole moment scales with the source radius like
).
The multipolar-post-Minkowskian (MPM) method will be implemented systematically, using symmetric-trace-free (STF) harmonics to describe the multipole expansion [403*], and looking for a definite algorithm for the approximation scheme [57*]. The solution of the system of equations (33) takes the form of a series of retarded multipolar waves17
where











Theorem 1. The most general solution of the linearized field equations (33) outside some
time-like world tube enclosing the source (), and stationary in the past [see Eq. (29*)], reads





The other terms represent a linearized gauge transformation, with gauge vector parametrized by
four other multipole moments, say
,
,
and
[see Eqs. (37)].
The conservation of the lowest-order moments gives the constancy of the total mass of the
source, , center-of-mass position,
, total linear momentum
,18
and total angular momentum,
. It is always possible to achieve
by translating the
origin of our coordinates to the center of mass. The total mass
is the ADM mass of the Hamiltonian
formulation of general relativity. Note that the quantities
,
,
and
include the
contributions due to the waves emitted by the source. They describe the initial state of the source, before
the emission of gravitational radiation.
The multipole functions and
, which thoroughly encode the physical properties of the
source at the linearized level (because the other moments
parametrize a gauge
transformation), will be referred to as the mass-type and current-type source multipole moments. Beware,
however, that at this stage the moments are not specified in terms of the stress-energy tensor
of the
source: Theorem 1 follows merely from the algebraic and differential properties of the vacuum field
equations outside the source.
For completeness, we give the components of the gauge-vector entering Eq. (35*):
Because the theory is covariant with respect to non-linear diffeomorphisms and not merely with respect
to linear gauge transformations, the moments do play a physical role starting at the
non-linear level, in the following sense. If one takes these moments equal to zero and continues the
post-Minkowskian iteration [see Section 2.3] one ends up with a metric depending on
and
only, but that metric will not describe the same physical source as the one which would have
been constructed starting from the six moments
altogether. In other words, the
two non-linear metrics associated with the sets of multipole moments
and
are not physically equivalent – they are not isometric. We shall point out
in Section 2.4 below that the full set of moments
is in fact physically
equivalent to some other reduced set of moments
, but with some moments
,
that differ from
,
by non-linear corrections [see Eqs. (97) – (98)]. The
moments
,
are called “canonical” moments; they play a useful role in intermediate
calculations. All the multipole moments
,
,
,
,
,
will be computed in
Section 4.4.
2.3 The multipolar post-Minkowskian solution
By Theorem 1 we know the most general solution of the linearized equations in the exterior of the source. We then tackle the problem of the post-Minkowskian iteration of that solution. We consider the full post-Minkowskian series
where the first term is composed of the result given by Eqs. (35*) – (37). In this article, we shall always understand the infinite sums such as the one in Eq. (38*) in the sense of formal power series, i.e., as an ordered collection of coefficients,
We substitute the post-Minkowski ansatz (38*) into the vacuum Einstein field equations (21*) – (22*), i.e.,
with simply given by the gravitational source term
, and we equate term by term the factors of
the successive powers of our book-keeping parameter
. We get an infinite set of equations for each of the
’s: namely,
,
The right-hand side of the wave equation (39a) is obtained from inserting the previous iterations, known
up to the order , into the gravitational source term. In more details, the series of equations (39a)
reads
The quadratic, cubic and quartic pieces of are defined by Eq. (25*) – (26).
Let us now proceed by induction. Some being given, we assume that we succeeded in
constructing, starting from the linearized solution
, the sequence of post-Minkowskian solutions
, and from this we want to infer the next solution
. The right-hand side of
Eq. (39a),
, is known by induction hypothesis. Thus the problem is that of solving a flat
wave equation whose source is given. The point is that this wave equation, instead of being
valid everywhere in
, is physically correct only outside the matter source (
), and
it makes no sense to solve it by means of the usual retarded integral. Technically speaking,
the right-hand side of Eq. (39a) is composed of the product of many multipole expansions,
which are singular at the origin of the spatial coordinates
, and which make the retarded
integral divergent at that point. This does not mean that there are no solutions to the wave
equation, but simply that the retarded integral does not constitute the appropriate solution in that
context.
What we need is a solution which takes the same structure as the source term , i.e., is expanded
into multipole contributions, with a singularity at
, and satisfies the d’Alembertian
equation as soon as
. Such a particular solution can be obtained, following the
method of Ref. [57*], by means of a mathematical trick, in which one first “regularizes” the
source term
by multiplying it by the factor
, where
is the spatial radial
distance and
is a complex number,
. Let us assume, for definiteness, that
is
composed of multipolar pieces with maximal multipolarity
. This means that we start
the iteration from the linearized metric (35*) – (37) in which the multipolar sums are actually
finite.19
The divergences when
of the source term are typically power-like, say
(there are also powers
of the logarithm of
), and with the previous assumption there will exist a maximal order of divergency,
say
. Thus, when the real part of
is large enough, i.e.,
, the “regularized”
source term
is regular enough when
so that one can perfectly apply the retarded integral
operator. This defines the
-dependent retarded integral, when
is large enough,


















As we see, the case shows that the finite-part coefficient in Eq. (43*), namely
, is a
particular solution of the requested equation:
. Furthermore, we can prove that this solution,
by its very construction, owns the same structure made of a multipolar expansion singular at
as the
corresponding source.
Let us forget about the intermediate name , and denote, from now on, the latter solution by
, or, in more explicit terms,















From that expression we are able to find a new object, say , which takes the same
structure as
(a retarded solution of the source-free wave equation) and, furthermore, whose
divergence is exactly the opposite of the divergence of
, i.e.
. Such a
is not unique, but we shall see that it is simply necessary to make a choice for
(the simplest one) in order to obtain the general solution. The formulas that we adopt are
Notice the presence of anti-derivatives, denoted e.g., by ; there is no problem
with the limit
since all the corresponding functions are zero when
. The choice made
in Eqs. (48) is dictated by the fact that the
component involves only some monopolar and
dipolar terms, and that the spatial trace
is monopolar:
. Finally, if we pose



2.4 Generality of the MPM solution
We have a solution, but is that a general solution? The answer, “yes”, is provided by the following result [57*].
Theorem 2. The most general solution of the harmonic-coordinates Einstein field equations in the vacuum region outside an isolated source, admitting some post-Minkowskian and multipolar expansions, is given by the previous construction as
It depends on two sets of arbitrary STF-tensorial functions of time


The proof is quite easy. With Eq. (49*) we obtained a particular solution of the system of equations (39).
To it we should add the most general solution of the corresponding homogeneous system of equations, which
is obtained by setting into Eqs. (39). But this homogeneous system of equations is nothing
but the linearized vacuum field equations (33), to which we know the most general solution
given by Eqs. (35*) – (37). Thus, we must add to our particular solution
a general
homogeneous solution that is necessarily of the type
, where
denote
some corrections to the multipole moments at the
-th post-Minkowskian order (with the
monopole
and dipoles
,
being constant). It is then clear, since precisely the
linearized metric is a linear functional of all these moments, that the previous corrections to
the moments can be absorbed into a re-definition of the original ones
by posing
After re-arranging the metric in terms of these new moments, taking into account the fact that the
precision of the metric is limited to the -th post-Minkowskian order, and dropping the superscript
“new”, we find exactly the same solution as the one we had before (indeed, the moments are arbitrary
functions of time) – hence the proof.
The six sets of multipole moments contain the physical information about any
isolated source as seen in its exterior. However, as we now discuss, it is always possible to find two, and only
two, sets of multipole moments,
and
, for parametrizing the most general isolated source as
well. The route for constructing such a general solution is to get rid of the moments
at
the linearized level by performing the linearized gauge transformation
, where
is
the gauge vector given by Eqs. (37). So, at the linearized level, we have only the two types
of moments
and
, parametrizing
by the same formulas as in Eqs. (36). We
must be careful to denote these moments with names different from
and
because
they will ultimately correspond to a different physical source. Then we apply exactly the same
post-Minkowskian algorithm, following the formulas (45*) – (49*) as we did above, but starting from the
gauge-transformed linear metric
instead of
. The result of the iteration is therefore some



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So why not consider from the start that the best description of the isolated source is provided by only
the two types of multipole moments, and
, instead of the six types,
? The reason
is that we shall determine in Theorem 6 below the explicit closed-form expressions of the six source
moments
, but that, by contrast, it seems to be impossible to obtain some similar
closed-form expressions for the canonical moments
and
. The only thing we can do is to write
down the explicit non-linear algorithm that computes
,
starting from
. In
consequence, it is better to view the moments
as more “fundamental” than
and
,
in the sense that they appear to be more tightly related to the description of the source, since they admit
closed-form expressions as some explicit integrals over the source. Hence, we choose to refer collectively to
the six moments
as the multipole moments of the source. This being said, the moments
and
are generally very useful in practical computations because they yield a simpler
post-Minkowskian iteration. Then, one can generally come back to the more fundamental source-rooted
moments by using the fact that
and
differ from the corresponding
and
only
by high-order post-Newtonian terms like 2.5PN; see Eqs. (97) – (98) below. Indeed, this is to
be expected because the physical difference between both types of moments stems only from
non-linearities.
2.5 Near-zone and far-zone structures
In our presentation of the post-Minkowskian algorithm (45*) – (49*) we have for the moment omitted a
crucial recursive hypothesis, which is required in order to prove that at each post-Minkowskian order
, the inverse d’Alembertian operator can be applied in the way we did – notably that the
-dependent retarded integral can be analytically continued down to a neighbourhood of
. This hypothesis is that the “near-zone” expansion, i.e., when
, of each one of the
post-Minkowskian coefficients
has a certain structure (here we often omit the space-time
indices
); this hypothesis is established as a theorem once the mathematical induction
succeeds.
Theorem 3. The general structure of the expansion of the post-Minkowskian exterior metric in the
near-zone (when ) is of the type:
,








For the proof see Ref. [57*]. As we see, the near-zone expansion involves, besides the simple powers of ,
some powers of the logarithm of
, with a maximal power of
. As a corollary of that theorem, we
find, by restoring all the powers of
in Eq. (53*) and using the fact that each
goes into the
combination
, that the general structure of the post-Newtonian expansion (
) is necessarily
of the type





Paralleling the structure of the near-zone expansion, we have a similar result concerning the
structure of the far-zone expansion at Minkowskian future null infinity, i.e., when with
:
,



Theorem 4. The most general multipolar-post-Minkowskian solution, stationary in the past [see Eq. (29*)],
admits some radiative coordinates , for which the expansion at future null infinity,
with
, takes the form



Proof. We introduce a linearized “radiative” metric by performing a gauge transformation of the harmonic-coordinates metric defined by Eqs. (35*) – (37), namely
where the gauge vector























