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ABSTRACT
Reconstructing magnetizations from measurements of the generated magnetic potential is generally non-unique. The non-uniqueness still remains if one restricts the magnetization to those induced by an ambient magnetic dipole field (i.e. the magnetization is described by a scalar susceptibility and the dipole direction). Here, we investigate the situation under the additional constraint that the susceptibility is either spatially localized in a subregion of the sphere or that it is band-limited. If the dipole direction is known, then the susceptibility is uniquely determined under the spatial localization constraint while it is only determined up to a constant under the assumption of band-limitedness. If the dipole direction is not known, uniqueness is lost again. However, we show that all dipole directions that could possibly generate the measured magnetic potential need to be zeros of a certain polynomial which can be computed from the given potential. We provide examples of non-uniqueness of the dipole direction and examples on how to find admissible candidates for the dipole direction under the spatial localization constraint.
1. Introduction
Assuming a magnetic field of the form
on a sphere
that is generated by a magnetization
on a sphere
of radius
, we are interested in the question of which contributions of
can be reconstructed from knowledge of the potential V. In particular, we are interested in magnetizations that are induced by an ambient dipole magnetic field, i.e.
is of the form
(1.1)
(1.1)
where denotes the direction of the dipole (which we assume to be located in the center of the sphere
) and Q the susceptibility on
. For brevity, several physical quantities and constants are implicitly included in the function Q (so, technically, Q is not a susceptibility, but we still call it ‘susceptibility’ throughout this paper). More precisely,
, where
is the actual susceptibility and d the norm of the inducing dipole moment. For the magnetic field
we assume that it has no other sources than
, i.e. outside
, it can be written in the form
with a harmonic potential V given by
(1.2)
(1.2)
When is of induced form as described in (Equation1.1
(1.1)
(1.1) ), we typically write
instead of the more general notation
.
In general, even if the dipole direction is known, the susceptibility Q is not determined uniquely by knowledge of the potential
on the sphere
(see, e.g. [Citation1], where they named magnetizations that produce no magnetic potential on
‘annihilators’; here, we call such magnetizations ‘silent from outside’). If we make the additional assumption that Q is locally supported in some subregion
, then the susceptibility is actually determined uniquely (cf. [Citation2], based on results from [Citation3,Citation4] in a Euclidean set-up). Therefore, in the latter scenario, but under the condition that the dipole direction is not known, our goal is to find suitable candidates for the dipole direction
. If the magnetization
was known, then a standard procedure such as described in [Citation5, Chapter 7] can be used to derive
from the direction of
or to see that
cannot be of the form (Equation1.1
(1.1)
(1.1) ). However, just given the corresponding magnetic potential
on the sphere
, only certain components of
can be reconstructed uniquely (cf. [Citation2,Citation3,Citation6]; a summary is provided in Section 2). Namely, if
(1.3)
(1.3)
is the Hardy-Hodge decomposition (cf. Theorem 2.2) of the magnetization, then only is determined uniquely. If we know in advance that
is localized in a subregion
, then
and
are determined uniquely.
In other words, the question we are interested in can be reformulated as follows: Knowing only the uniquely determined components of , what can be said about
and Q? An illustration of the effect of non-uniqueness on classical methods of paleopole estimation can be found in [Citation7], for the case that no further a priori assumptions are made on the induced magnetization. In the paper at hand, we investigate the influence of certain constraints on
(namely, the constraint that the magnetization is localized in a subdomain
of the sphere or that it is band-limited). More precisely, we provide examples of non-uniqueness for the simultaneous reconstruction of Q and
from knowledge of
on
, even under the mentioned additional constraints. But we also show that all possible candidates for the dipole direction
for which the given potential can be expressed in the form
need to be zeros of a particular polynomial that can be obtained from the given potential (cf. Sections 3 and 4). This allows to restrict the set of candidates for the dipole direction and, to some extent, improve the handling of the non-uniqueness. An overview on the mentioned uniqueness results for the reconstruction of general or induced magnetizations is provided in Table .
The spatial localization constraint can be a geophysically reasonable assumption in certain situations. For example, localization could be enforced if one has knowledge of the true magnetization in a small subregion of (the magnetic field produced by this known magnetization can be subtracted from the given magnetic field, so that the residual has to be produced by a magnetization that satisfies the spatial localization assumption) or if it is known in advance that there exists a region with nearly vanishing magnetization (which is expected for some craters on Mars; see, e.g. [Citation8]). Being able to compute the set of admissible candidates for the dipole direction could be of use, e.g. for paleopole estimations. The assumption that the magnetization
is concentrated on a spherical surface
is fairly common in geophysical applications since magnetization typically occurs only in the upper few tens of kilometers of the Earth’s lithosphere. Actually, for any ‘sufficiently nice’ volumetric magnetization in the ball
there can be found a magnetization concentrated on
that produces the same magnetic potential on
,
, as its volumetric counterpart (see, e.g. [Citation9, Section 3]). For the notion of vertically integrated magnetizations, the reader is referred to [Citation6]. The complicated fact that magnetizations often have remanent and induced contributions are not accounted for in our approach. We require the knowledge of the induced magnetic field and regard all non-induced contributions as ‘noise’. Last, it should be noted that the inversion of the magnetic potential
from (Equation1.2
(1.2)
(1.2) ) is closely related to the gravimetric problem (see, e.g. [Citation10,Citation11] and references therein). However, while the gravimetric problem is unique when restricted to harmonic mass densities, the vectorial nature of the inverse magnetization problem causes the described non-uniqueness issues.
Finally, the structure of the paper at hand is as follows: In Section 2, we provide some notations and a brief recapitulation of the spherical Helmholtz and Hardy-Hodge decompositions. The latter classifies those components of the magnetization (not necessarily of the form (Equation1.1
(1.1)
(1.1) )) that are determined uniquely by knowledge of
on
. Namely, if
is the Hardy-Hodge decomposition, then only
is determined uniquely (e.g. [Citation2,Citation3,Citation6]; we say that
and
are ‘equivalent from outside’). We also formulate the Helmholtz and Hardy-Hodge decompositions in terms of some well-known vector spherical harmonics, which will be of use for our considerations on band-limited magnetizations. However, it should already be noted that the constraint of
being band-limited, opposed to being spatially localized, still only yields that
is determined uniquely by
on
.
Table 1. Overview on uniqueness results for magnetizations, provided that the magnetic potential V is known on , with radius
. By
we mean the underlying magnetization, by
,
,
the contributions of its Hardy-Hodge decomposition (Equation1.3
(1.3)
(1.3) ). In the case of induced magnetizations
of the form (Equation1.1
(1.1)
(1.1) ),
denotes the inducing dipole direction and
, where
is the susceptibility and d the norm of the inducing dipole moment.
Based on the results from Sections 2, 3 and 4 focus on the case of induced magnetizations of the form (Equation1.1(1.1)
(1.1) ) under the constraint that the susceptibilities Q are localized in a subregion
or that Q is band-limited, respectively. In both cases, we supply counter-examples to the uniqueness issue, i.e. we construct two susceptibilities Q and
and dipole directions
that satisfy the respective constraints and additionally yield
on
(throughout the course of this paper, we call
and
‘equivalent (from outside)’ if they produce the same potential on
). Although non-uniqueness prevails under the additional constraints, for a given potential V of the form (Equation1.2
(1.2)
(1.2) ), we derive a way of computing a subset of
which contains all dipole directions
for which there exists a susceptibility Q such that
on
. Namely, in the case of spatially localized susceptibilities, the admissible dipole directions are zeros of a fourth order polynomial that can be computed from the known potential V (cf. Theorem 3.3). This way, we at least obtain some additional information on the otherwise non-unique problem. In the optimal case, there exists only a single zero
of the polynomial, which would guarantee uniqueness for the particular measured magnetic potential V (note that uniqueness is only understood up the sign because, obviously,
). Similar results can be obtained for band-limited susceptibilities (cf. Section 4). However, here the degree of the polynomial of which the zeros need to be determined depends on the band-limit (furthermore, the zeros do not directly resemble the dipole direction
but rather the vector
of spherical harmonics of degree one evaluated at the point
). Additionally, while for the spatial localization constraint, a known dipole direction uniquely determines the susceptibility, the assumption of band-limitedness only implies that a given dipole direction determines the susceptibility up to an additive constant (cf. Lemma 4.3). It should be noted at this point that we included the section on band-limited magnetizations mainly for the sake of completeness, since we believe that the spatial localization constraint could be more useful for geophysically reasonble scenarios. Nonetheless, the band-limited case shows that the commonly used finite expansion of magnetizations in terms of spherical harmonics introduces some level of uniqueness that is not inherent to the original problem (similar to the case of reconstructing magnetic fields from intensity data; see, e.g. [Citation13]).
Eventually, in Section 5, we provide some numerical examples on how the considerations from Section 3 for spatially localized magnetizations can help to obtain suitable candidates for the dipole directions and on how to decide if a given potential V on
can be produced by a dipole induced magnetization of the form (Equation1.1
(1.1)
(1.1) ) in the first place. For brevity, we restrict the numerical examples to the case of spatial localization constraints (and not the constraint of band-limitation) as we believe this to be more relevant for potential applications. For notational reasons, we choose
throughout the remainder of this paper, since dipole induced magnetizations then have the form
while the radius R of the sphere where the potential V is given can still be any radius . However, the results hold true for any
.
2. Auxiliary results and notations
Throughout this paper, bold-face letters typically denote vector valued functions mapping
,
, or
into
, while f, g, F, G denote scalar valued functions mapping
,
, or
into
. For brevity, we denote the unit sphere
by
throughout the course of this paper. Accordingly,
and
mean the function space of vector valued square-integrable functions and the Sobolev space as denoted, e.g. in [Citation14], respectively.
and
denote the corresponding scalar valued function spaces. For the rest of this section, we briefly recapitulate some notations and results from [Citation2,Citation3,Citation6,Citation14,Citation17]. In particular, proofs of the main results of this section, i.e. Theorems 2.2, 2.4 and Corollary 2.5, can be found in [Citation2]. First, we define the following Helmholtz operators, acting at a point
:
(2.1)
(2.1)
(2.2)
(2.2)
(2.3)
(2.3)
where denotes the surface gradient on the unit sphere
,
the surface curl gradient (
means the vector product), and ‘
’ the identity operator (i.e. the operator
simply represents multiplication with the radial vector). The Euclidean gradient is denoted by
and can be expressed in the form
, for
. These operators allow to decompose a spherical vector field into a radial, surface curl-free, and a surface divergence-free tangential contribution.
Theorem 2.1:
[Spherical Helmholtz Decomposition] Any function can be decomposed into
(2.4)
(2.4)
where the scalar functions ,
,
are uniquely determined by the conditions
.
A further decomposition that is of particular importance for the characterization of magnetizations is based on the spherical Hardy-Hodge operators(2.5)
(2.5)
(2.6)
(2.6)
(2.7)
(2.7)
where denotes the pseudo-differential operator
(2.8)
(2.8)
and the spherical Beltrami operator. These operators above reflect the decomposition into a surface curl-free tangential contribution and two further contributions generated by the gradient of functions that are harmonic in the interior and the exterior of
, respectively.
Theorem 2.2:
[Spherical Hardy-Hodge Decomposition] Any function can be decomposed into
(2.9)
(2.9)
where the scalar functions ,
,
are uniquely determined by the conditions
. If
,
,
are the Helmholtz scalars of
as given in Theorem 2.1, then
(2.10)
(2.10)
(2.11)
(2.11)
(2.12)
(2.12)
Although, the Hardy-Hodge decomposition in Theorem 2.2 reflects the decomposition that we require to describe the uniqueness issues of the treated inverse magnetization problem, the contributions ,
,
from the Helmholtz decomposition in Theorem 2.1 are often easier to handle and compute (e.g.
). Therefore, the relations (Equation2.10
(2.10)
(2.10) )–(Equation2.12
(2.12)
(2.12) ) can be quite helpful. Some related applications and information on such a decomposition on the Euclidean plane instead of a sphere can be found in [Citation3,Citation4,Citation18].
In the following, we recapitulate some earlier results on how the Hardy-Hodge decomposition characterizes the uniqueness of general magnetization (for details and proofs, the reader is referred to [Citation2,Citation3]). First, we introduce the notion of equivalent magnetizations, which simply means that the two magnetizations produce the same potential V (i.e. the same magnetic field
) on some sphere
. In other words, if there exist two equivalent magnetizations, we have non-uniqueness (i.e. the knowledge of
on
does not uniquely determine
). It should be noted that, when talking about induced magnetizations with susceptibility Q and dipole direction
, uniqueness is only meant up to the sign because, clearly,
.
Definition 2.3:
Two magnetizations ,
are called equivalent from outside if
on
for an
. They are called equivalent from inside if
on
for an
. A magnetization
is called silent from outside or inside if it is equivalent to the zero-magnetization
from outside or inside, respectively (i.e. if
on
for
or
, respectively; such silent magnetizations are also frequently called annihilators).
If the magnetizations ,
are of the form (Equation1.1
(1.1)
(1.1) ), with susceptibilities Q,
and dipole directions
,
, then we say that
and
are equivalent from inside/outside or we say that
is silent from inside/outside if the corresponding magnetizations
,
have these properties.
For us, the case (i.e. equivalence/silence from outside) is of major relevance since we are eventually interested in using satellite magnetic field measurements, which are obviously collected in the exterior of a planet. Now we can formulate the characterization of those contributions of
that are uniquely determined by knowledge of the potential
using the notion of equivalent magnetizations.
Theorem 2.4:
Let and its decomposition into
,
,
be given as in Theorem 2.2. Then, the following assertions hold true:
The magnetization
is equivalent from outside to
while
is equivalent from inside to
.
The magnetization
is silent from outside if and only if
while
is silent from inside if and only if
.
If
, for a region
with
, then
is silent from outside if and only if it is silent from inside.
We see that the contribution is determined uniquely by
on a sphere
of radius
. If additionally
, then both
and
are determined uniquely. The latter follows from part (c) of the previous theorem: if
and
were two magnetizations with
on
, then
would be silent from outside with
. Thus,
must also be silent from inside and we get
and
from parts (a) and (b). Observing that
is non-tangential for all
that are not orthogonal to
, the next corollary is a direct consequence of Theorem 2.4 for dipole induced magnetizations.
Corollary 2.5:
Let be of the induced form (Equation1.1
(1.1)
(1.1) ), with
and
, and supp
for a fixed region
with
. Then there does not exist another susceptibility
with supp
such that
and
are equivalent from outside or inside.
In other words, a spatially localized susceptibility Q is uniquely determined by the knowledge of on a sphere
of radius
if
is assumed to be given in advance. Next, we introduce two classical sets of vector spherical harmonics that reflect the decompositions from Theorems 2.1 and 2.2 in spectral domain. For details, the reader is referred to, e.g. [Citation14–Citation16,Citation19].
Definition 2.6:
For ,
, and
, we set
and
with normalization constants ,
, and
,
,
. The
denote an orthonormal set of scalar spherical harmonics (to be consistent with later computations in Section 4, we particularly choose
to be the complex-valued spherical harmonics as defined in [Citation20,Citation21]). It is to note that the type-(2) and type-(3) vector spherical harmonics vanish for degree
while this is not the case for type (1). To avoid introducing additional notation, the type-(2) and type-(3) vector spherical harmonics should, therefore, simply be regarded as void whenever they appear for degree
.
The sets and
each form a complete orthonormal system in
. Thus, a Fourier expansion
(2.13)
(2.13)
of a magnetization , with Fourier coefficients
, inherits the properties of the Hardy-Hodge decomposition described in Theorem 2.4. For example.,
is silent from outside if and only if all type-(2) Fourier coefficients vanish, i.e.
(2.14)
(2.14)
Analogously, is silent from inside if and only if
for all
,
. Just as the Helmholtz and Hardy-Hodge decomposition in Theorem 2.2, the two sets of vector spherical harmonics have a simple connection: obviously
, and additionally
(2.15)
(2.15)
(2.16)
(2.16)
3. Spatially localized induced magnetizations
Let with
,
for a region
with closure
, and
. In order to check whether
and
are equivalent from outside, we are led to investigating if the residual magnetization
(3.1)
(3.1)
is silent from outside. According to Theorem 2.4, the latter would imply(3.2)
(3.2)
(3.3)
(3.3)
which by Theorems 2.1 and 2.2 directly implies(3.4)
(3.4)
(3.5)
(3.5)
where and
,
, denote the scalar functions appearing in the Helmholtz decomposition and the Hardy-Hodge decomposition of
according to Theorems 2.1 and 2.2, respectively. Equations (Equation3.1
(3.1)
(3.1) ) and (Equation3.4
(3.4)
(3.4) ) yield
(3.6)
(3.6)
which can be reformulated to and leads to the following representation of
:
(3.7)
(3.7)
For later reference, we define(3.8)
(3.8)
Additionally, equations (Equation3.4(3.4)
(3.4) ) and (Equation3.5
(3.5)
(3.5) ) imply that
has to be surface divergence-free if it is silent from outside, since it must hold
, where
is the vectorial surface divergence-free function of the Helmholtz and Hardy-Hodge decomposition of
. Summarizing, we are led to the following assertion on uniqueness of dipole-induced magnetizations.
Lemma 3.1:
Let , with
, and
. Then, for a given
, there exists a
with
such that
and
are equivalent from outside if and only if
and
as in (Equation3.7
(3.7)
(3.7) ) is surface divergence-free.
Remark 3.2:
In particular, the lemma above implies that if and
, then there exists no other susceptibility
with
such that
and
are equivalent from outside. This is a condition that should guarantee uniqueness for many geophysically relevant dipole induced magnetizations since non-uniqueness would require the susceptibility Q to be zero along at least one meridian.
Furthermore, in geophysical reality susceptibilities are non-negative. If Q is such a non-negative susceptibility, then, we know from the previous considerations that any equivalent susceptibility with needs to be of the form
. However, if
, there always exist
such that
and
have different signs. If such an x where a sign change occurs is contained in
, then
cannot be non-negative. In other words, the assumption of non-negative susceptibilities does supply some additional information but it does not generally lead to uniqueness of the problem.
In general, it is fairly easy to construct examples where non-uniqueness is given: Let and assume Q to be such that the function
given by
is continuously differentiable on
. Then, in order for a
with
to exist such that
and
are equivalent from outside, Lemma 3.1 implies that
as in (Equation3.7
(3.7)
(3.7) ) has to be surface divergence-free, i.e.
(3.9)
(3.9)
A closer investigation of (Equation3.9(3.9)
(3.9) ) shows that the spherical circles
,
, represent the characteristic curves of the given differential equation and that
has to be constant along these curves. Thus,
has to be of the form
, where
is a continuously differentiable function with
for all
that satisfy
. Given such a P, we see from Lemma 3.1 that
satisfy and that
and
are equivalent from outside. An illustration of two such magnetizations, with
being the eastern hemisphere, is shown in Figure .
Figure 1. Illustration of two dipole induced magnetizations of the form described in Remark 3.2 that are equivalent from outside. We chose the auxiliary function to be , the region
to be the eastern hemisphere, and the dipole directions
and
, respectively. Left: susceptibility Q, Center: susceptibility
, Right: dipole directions
(blue) and
(red).
![Figure 1. Illustration of two dipole induced magnetizations of the form described in Remark 3.2 that are equivalent from outside. We chose the auxiliary function to be P(t)=e-1t2χ[0,1](t), the region Γ={x∈S:(0,-1,0)T·x≥0} to be the eastern hemisphere, and the dipole directions d=(0,0,1)T and d¯=(1,0,0)T, respectively. Left: susceptibility Q, Center: susceptibility Q¯, Right: dipole directions d (blue) and d¯ (red).](/cms/asset/dec2275f-e4a7-4bb6-9a65-f852e01df7bd/gipe_a_1438426_f0001_oc.gif)
Let now , with
, and
be the corresponding potential on
. We are interested in finding out if there exists a dipole induced magnetization of the form (Equation1.1
(1.1)
(1.1) ) that produces the same magnetic potential on
as
(which is not necessarily of dipole induced form). If there exist
, with
, and
such that the corresponding magnetization
is equivalent from outside to
(we also say
is equivalent from outside to
), then Theorem 2.4 together with the Helmholtz and the Hardy-Hodge decomposition tells us
(3.10)
(3.10)
where and
are the radial contributions of
and
, respectively. The higher smoothness assumption of
is only required to allow differentiation of
and
later on. From (Equation3.10
(3.10)
(3.10) ) we get for the susceptibility Q that
(3.11)
(3.11)
It remains to find the dipole direction . Again, referring to Theorem 2.4 and the decompositions from Theorems 2.1 and 2.2, we get, additionally to
, that
. This yields, together with (Equation3.11
(3.11)
(3.11) ),
Multiplying the above by leads to the condition
(3.12)
(3.12)
Eventually, integrating the square of the left hand side of (Equation3.12(3.12)
(3.12) ) over
, we find that the dipole direction
has to be a zero of the following fourth-order polynomial
(3.13)
(3.13)
where(3.14)
(3.14)
and . We can now summarize these observations in the following theorem.
Theorem 3.3:
Let with
, for some region
with
. Furthermore, we set
. Then there exists a susceptibility
with
and a dipole direction
such that
is equivalent to
from outside if and only if there exists a
that satisfies
and , where
is given as in (Equation3.13
(3.13)
(3.13) ).
Remark 3.4:
On the one hand, Theorem 3.3 provides a means of deciding whether a given potential V on can be produced by a dipole induced magnetization of the form (Equation1.1
(1.1)
(1.1) ). Namely, one first inverts V to find a general magnetization
such that
on
. Afterwards one can use Theorem 3.3 to check whether V can also be expressed in the form
. On the other hand, Theorem 3.3 can give hints at the uniqueness of the susceptibility Q and dipole direction
: if
has only one zero (up to the sign), then uniqueness is given.
4. Band-limited induced magnetizations
Analogous questions as in Section 3 are investigated under the assumption that the magnetization is band-limited (and not spatially localized in the sense
).
Definition 4.1:
We call a function
band-limited if there exists a
such that
i.e. all Fourier coefficients vanish from some degree on. N is called the band-limit of
. A scalar function
is called band-limited if there exists a
such that
We start by computing the Fourier expansion of magnetizations of the form (Equation1.1
(1.1)
(1.1) ). The inducing vectorial dipole field part can be expressed as
(4.1)
(4.1)
For a susceptibility with Fourier expansion
one can then use the calculus of Wigner symbols (e.g. [Citation19,Citation22]; a notation compatible with ours is used in [Citation20]) to obtain the following expression for the corresponding dipole induced magnetization
:
(4.2)
(4.2)
where if
,
if
, and
if
, and
(4.3)
(4.3)
The brackets denote Wigner-6j symbols while
denote Wigner-3j symbols. It is to note that round brackets are also used for matrices, however, it should be clear from the context if we mean Wigner-3j symbols or matrices.
An expansion of the magnetization in terms of
, which reflects the Hardy-Hodge decomposition from Theorem 2.2, can be directly obtained from (Equation4.2
(4.3)
(4.3) ), (Equation2.15
(2.15)
(2.15) ), and (Equation2.16
(2.16)
(2.16) ). This is summarized in the following proposition.
Proposition 4.2:
Let ,
, and
,
, be the coefficients as in (Equation4.3
(4.6)
(4.6) )–(Equation4.5
(4.8)
(4.8) ). Then, the dipole induced magnetization
has the Fourier expansion
with
The properties of the Wigner-3j symbols yield that if
, so that the fourth sum in the above representation of
has contributions only for
. Any Fourier coefficients
with
or
are zero by definition.
Now we are in a place to characterize silent band-limited dipole induced magnetizations. Theorem 2.4(b) essentially states that a magnetization is silent from outside if and only if all type-(2) Fourier coefficients
vanish. In consequence, the representation in Proposition 4.2 implies that
is silent from outside if and only if
(4.6)
(4.6)
For ,
, and
, we can compute from the representation in Proposition 4.2 that
(4.7)
(4.7)
so that if and only if
. Analogously, one can see that
for all
,
, and
. This leads us to the following statement.
Lemma 4.3:
Let be band-limited and
. If
is another band-limited susceptibility such that
and
are equivalent from outside, then all Fourier coefficients for degrees greater or equal to one coincide, i.e.
for all
,
.
Proof Let us assume for now that is silent from outside. The equations in (Equation4.6
(4.6)
(4.6) ) can be rewritten in the form
(4.8)
(4.8)
where ,
are tri-band matrices and
,
vectors. More precisely, the matrix
and the vector
are of the form
(4.9)
(4.9)
with ,
,
, and the auxiliary vector
. The matrix
has the form
(4.10)
(4.10)
with ,
,
. For
we have seen in (Equation4.7
(4.10)
(4.10) ) that
and for
that
. Furthermore, for any
, at least one of the expressions
,
,
is non-zero. In consequence, for
, the entries of at least one of the three main diagonals of
are all non-zero, so that the matrix has full rank, i.e.
. The same holds true for
.
Since Q is band-limited, there must exist a such that
, for
. Thus, iteratively, we obtain from (Equation4.8
(4.11)
(4.11) ) and the full rank of
that any band-limited dipole induced magnetization that is silent from outside has to satisfy
, for
, i.e.
for all
,
.
If is not silent from outside but Q and
are two susceptibilities such that
and
are equivalent from outside, then the difference of the two corresponding magnetizations must be silent from outside, i.e. it must be satisfied that
(4.11)
(4.11)
for all . Now, the previous considerations imply the statement of the lemma.
Remark 4.4:
Equation (Equation4.6(4.9)
(4.9) ) contains contributions of the Fourier coefficient
only for the choice
. The observations in (Equation4.7
(4.10)
(4.10) ), however, yield that
,
, so that
does not have any effect on the magnetic potential
on
,
. In other words, any constant susceptibility Q leads to a dipole induced magnetization that is silent from outside. Lemma 4.3 implies that those are all silent band-limited dipole induced magnetizations.
If the particular dipole direction is chosen, then
for
. For this setting, the equations (Equation4.6
(4.9)
(4.9) ) reduce to
(4.12)
(4.12)
Latter is essentially identical to the recursion relation that was obtained in [Citation1] to characterize silent magnetizations (which they called annihilators). In this sense, Lemma 4.3 and the first part of this remark are just slightly more general statements of these results.
Next, we are interested in the equivalence of two dipole induced magnetizations with possibly different dipole directions. More precisely, for a given band-limited and
, we want to determine if there exists another susceptibility
and dipole direction
such that
and
are equivalent from outside (for
this is, of course, always possible by Lemma 4.3 and Remark 4.4). Equivalence from outside means that the residual magnetization
(4.13)
(4.13)
is silent from outside. According to (Equation4.6(4.9)
(4.9) ) and (Equation4.8
(4.11)
(4.11) ) this is possible if and only if
(4.14)
(4.14)
The quantities ,
,
are defined as in (Equation4.9
(4.12)
(4.12) ) and (Equation4.10
(4.13)
(4.13) ).
denotes the counterpart of
corresponding to
. Since the susceptibilities Q,
are assumed to be band-limited, there exists some
such that
for all
, so that, for
, (Equation4.14
(4.17)
(4.17) ) reduces to
(4.15)
(4.15)
Now, given and
, the first question to answer is if there exist
and a dipole direction
such that (Equation4.15
(4.18)
(4.18) ) is satisfied. The system of linear equations is overdetermined, but from the proof of Lemma 4.3 we know that
has full rank. From now on, we assume that
because then
. This yields that the matrix
, which is obtained from
by deleting the first two rows, is invertible. Analogously,
denotes
with its first two rows deleted. The uniquely determined candidate for
,
, is then obtained by
(4.16)
(4.16)
It remains to check whether (Equation4.15(4.18)
(4.18) ) is valid for this
, i.e. if
(4.17)
(4.17)
holds true for . By construction it actually suffices to check if the first two rows of the above system of equations hold true. From the structure of the inverse of upper triangular matrices, we find that
is a matrix with entries that are polynomials with respect to
(the coefficients
are defined as in (Equation4.9
(4.12)
(4.12) ) and depend on p and
). In conclusion, if
is an admissible candidate for a dipole direction, then
has to be a zero of the vector-valued polynomials
given by
(4.18)
(4.18)
for . It remains to check the cases
(
is not of interest since the coefficients
and
can be chosen arbitrarily according to Lemma 4.3 and Remark 4.4). In this case, the second and fourth summand in (Equation4.14
(4.17)
(4.17) ) cannot be omitted and we get that
additionally needs to be a zero of the polynomials
given by
(4.19)
(4.19)
for . The additional product
is only included to guarantee that
is a polynomial, although this is not crucial for our statements. The required vectors
can be computed iteratively from the results of the previous steps: starting with (Equation4.16
(4.19)
(4.19) ) for
and continuing with
(4.20)
(4.20)
for .
Eventually, we see that in order to determine if, for a given band-limited susceptibility Q and dipole direction , there exists another band-limited susceptibility
and dipole direction
such that
and
are equivalent from outside, one possible way is to find common zeros of
,
, and
,
. If a common zero
other than
exists and if it is of the form
, then a candidate for
has been found (and the corresponding suceptibility
is determined up to a constant via the Fourier coefficients gathered in (Equation4.16
(4.19)
(4.19) ), (Equation4.20
(5.1)
(5.1) )). However, it is by no means true that all common zeros of
and
need to be representable in the form
in the first place. Finally, the so far excluded case
has to be checked separately (e.g. by choosing
to be the matrix that is obtained from
not by deleting the first two rows but by deleting the first and last row).
Remark 4.5:
From Lemma 4.3 and Remark 4.4 it is clear that for constant susceptibilities and
, with
, it holds that
and
are equivalent from outside for any
. A slightly more complex example for equivalent band-limited magnetizations would be for band-limit
. Let us choose
and
and construct
and
from (Equation4.16
(4.19)
(4.19) ) and (Equation4.17
(4.20)
(4.20) ). Clearly,
needs to be in the nullspace of of the matrix
, which is spanned by
. From (Equation4.16
(4.19)
(4.19) ) we then obtain
. This leads us to band-limited susceptibilities
(4.21)
(4.21)
They are illustrated in Figure . We see that, by the procedure described in the previous paragraphs, it is easy to construct band-limited and
, with
, that are equivalent from outside. However, to check if, for a given
, there exists another band-limited
and
such that
and
are equivalent from outside is somewhat more tedious. But essentially it boils down to finding zeros of polynomials.
Figure 2. Illustration of the two band-limited dipole induced magnetizations with band-limit described Remark 4.5 that are equivalent from outside. Left: susceptibility Q, Center: susceptibility
, Right: dipole directions
(blue) and
(red).
![Figure 2. Illustration of the two band-limited dipole induced magnetizations with band-limit N=1 described Remark 4.5 that are equivalent from outside. Left: susceptibility Q, Center: susceptibility Q¯, Right: dipole directions d (blue) and d¯ (red).](/cms/asset/bc743add-6ff3-4aa5-affe-870c4d844925/gipe_a_1438426_f0002_oc.gif)
To conclude this section, we summarize the previous considerations in the upcoming theorem. We actually formulate a slightly more general version that allows to decide if, for a given band-limited (not necessarily of dipole induced form (Equation1.1
(1.1)
(1.1) )), there exists a dipole direction
and a susceptibility
such that
and
are equivalent from outside. This is essentially a band-limited counterpart to Theorem 3.3.
Theorem 4.6:
Let be band-limited with band-limit
. Then, there exists a band-limited susceptibility
and a dipole direction
such that
is equivalent to
from outside if and only if there exists a vector
that is a zero of the vector-valued polynomial
and that can be written in the form for
. The square in
and
is to be understood as acting componentwise on the vectors. The polynomials
and
are defined by
with and
. The matrices
and
are given as in (Equation4.9
(4.12)
(4.12) ) and (Equation4.10
(4.13)
(4.13) ).
and
denote the matrices
and
, respectively, with its first two rows (for
) or its first and last row (for
) deleted. Analogously,
represents the vector
with its first two entries or its first and last entry deleted. The vectors
, containing the Fourier coefficients of Q, can be computed iteratively by
Proof The condition (Equation4.14(4.17)
(4.17) ) for two dipole induced magnetizations can be rewritten in the following way
(4.23)
(4.23)
to fit the set-up of the theorem. The desired results then follow in the exact same manner as described in the previous paragraphs. The polynomial has only been introduced to obtain a single non-negative polynomial of which the zeros have to be found, rather than finding zeros separately for all
and
.
Remark 4.7:
Just as mentioned in Remark 3.4, for a given magnetic potential V, one first has to find a general magnetization such that
on
. Afterwards one can use Theorem 4.6 to check whether V can also be expressed in the form
. For the construction of the polynomial
in Theorem 4.6, only the contribution
of
, which is determined uniquely by V, is required.
5. Numerical Examples
We now provide some numerical examples based on the considerations for spatial localization constraints in Section 3.
5.1. The Algorithm
Remark 3.4 motivates the following three-step procedure to check whether a susceptibility Q and dipole direction exist such that
for a given potential V on
and to actually compute such Q,
. In fact, the focus is on finding a suitable dipole direction
(this is the quantity of interest, e.g. in some paleomagnetic problems; and once the dipole direction is known, the susceptibility could be obtained by solving the linear inverse problem
for a given
).
Procedure 5.1:
Let a magnetic potential V be given on a sphere of radius
, and let
be a subregion with
. Then proceed as follows:
Find a magnetization
with
that satisfies
By
we denote the magnetic potential generated by
via (Equation1.2
(1.2)
(1.2) ).
Compute
,
, and
from the
obtained in (1). Find a
that satisfies
Find a susceptibility
with
such that
By
we denote the magnetic potential
generated by a magnetization
of the form (Equation1.1
(1.1)
(1.1) ).
Remark 5.2:
There are a few aspects of Procedure 5.1 that require further clarification and discussion:
If only interested in the dipole direction
: the first two steps in Procedure 5.1 are the important ones, with step (2) supplying the candidates
for
. The corresponding susceptibility is directly given by
. However, Theorem 3.3 requires
in order to guarantee that
. Due to measurement and reconstruction errors in V and
the latter is unlikely to be achieved in reality. Therefore, step (3) can be seen as a validation of the result of the first two steps. Inverting V again in step (3), now with a given
, supplies an approximation
of Q that lies in
. If the data misfit
is ‘small enough’, this indicates that
is an admissible dipole direction.
Why the minimization in step (2)?: Theorem 3.3 actually requires to find a zero
of
. However, such a zero might not exist either because there does not exist a dipole induced magnetization that produces V in the first place or because noise in the measurements or reconstruction errors may have lead to a deteriorated version of
. In order to exclude false conclusions due to the latter mentioned error sources, we minimize
instead of trying to find its zeros (since
is always non-negative by construction, this procedure is equivalent). The minimization of
is actually stable with respect to errors in the coefficients of the polynomial. The instability of the problem at hand is due to the ill-posedness of the inverse problem that has to be solved in step (1).
What is meant by ‘too large’ and ‘too small’?: As always in inverse problems, this is a delicate question. One possible criterion could be the quantity
motivated by Morozov’s discrepancy principle (see, e.g. [Citation23]). If
is about the same order as the data noise level
, then we accept the candidate
. However, a detailed analysis of this criterion is outside the scope of this article.
Last but not least, it should be noted that the inverse problems in step (1) and (3) of Procedure 5.1 are linear (opposed to computing approximations
and
directly from a single inversion of V). Additionally, Procedure 5.1 supplies more information on possible candidates for dipole directions than the direct inversion.
Figure 3. Illustration of step (1) for situation (a): noise-free input data V (top left), underlying susceptibility Q (bottom left), radial component of the true magnetization
(center, and radial component
of the reconstructed magnetization
(right).
![Figure 3. Illustration of step (1) for situation (a): noise-free input data V (top left), underlying susceptibility Q (bottom left), radial component m1 of the true magnetization m (center, and radial component m1∗ of the reconstructed magnetization m∗ (right).](/cms/asset/a26cb0c2-515e-4845-852b-bdb2cfe4f27a/gipe_a_1438426_f0003_oc.gif)
Figure 4. Illustration of step (2) for situation (a): the figure shows the evaluation of on the unit sphere, the green dot indicates the location of the true dipole direction
. The color bar has been modified to emphasize the minimum, the actual minimum and maximum is indicated in the title.
![Figure 4. Illustration of step (2) for situation (a): the figure shows the evaluation of Tg∗,h∗,m1∗ on the unit sphere, the green dot indicates the location of the true dipole direction d. The color bar has been modified to emphasize the minimum, the actual minimum and maximum is indicated in the title.](/cms/asset/2f44d776-5c58-4e8c-9f8b-b00c21d0d229/gipe_a_1438426_f0004_oc.gif)
Figure 5. Illustration of step (1) for situation (a’): noisy input data V (top left), underlying susceptibility Q (bottom left), radial component of the true magnetization
(center), and radial component
of the reconstructed magnetization
(right).
![Figure 5. Illustration of step (1) for situation (a’): noisy input data V (top left), underlying susceptibility Q (bottom left), radial component m1 of the true magnetization m (center), and radial component m1∗ of the reconstructed magnetization m∗ (right).](/cms/asset/8fd74045-6594-441b-a74a-e1faa0d44ca0/gipe_a_1438426_f0005_oc.gif)
Figure 6. Illustration of step (2) for situation (a’): the figure shows the evaluation of on the unit sphere, the green dot indicates the location of the true dipole direction
. The color bar has been modified to emphasize the minimum, the actual minimum and maximum is indicated in the title.
![Figure 6. Illustration of step (2) for situation (a’): the figure shows the evaluation of Tg∗,h∗,m1∗ on the unit sphere, the green dot indicates the location of the true dipole direction d. The color bar has been modified to emphasize the minimum, the actual minimum and maximum is indicated in the title.](/cms/asset/1dfb01ac-16ae-4066-9cbd-6998a1e06122/gipe_a_1438426_f0006_oc.gif)
Figure 7. Illustration of step (3) for situation (a’): reconstructed susceptibility for
(left), data misfit
(right).
![Figure 7. Illustration of step (3) for situation (a’): reconstructed susceptibility Q∗ for d∗=(0.027,0.433,0.901)T (left), data misfit |Vε-V[Q∗,d∗]| (right).](/cms/asset/6495e15a-86d6-45e4-916b-620197adb59e/gipe_a_1438426_f0007_oc.gif)
Figure 8. Illustration of step (1) for situation (b): input data V (top left), underlying equivalent susceptibilities Q (center and bottom left), radial component and the contributions
and
of the true magnetization
(center), and radial component
and the contributions
and
of the reconstructed magnetization
(right). In the plots of the second and third row, colors indicate the absolute values
and
,
, and arrows the orientation.
![Figure 8. Illustration of step (1) for situation (b): input data V (top left), underlying equivalent susceptibilities Q (center and bottom left), radial component m1 and the contributions m(2) and m(3) of the true magnetization m (center), and radial component m1∗ and the contributions m∗,(2) and m∗,(3) of the reconstructed magnetization m∗ (right). In the plots of the second and third row, colors indicate the absolute values |m(i)| and |m∗,(i)|, i=1,2, and arrows the orientation.](/cms/asset/b0091b6d-3ca4-47b8-ab20-3e6d87134692/gipe_a_1438426_f0008_oc.gif)
Figure 9. Illustration of step (2) for situation (b): the figure shows the evaluation of on the unit sphere, the green and purple dots indicate the locations of the possible (true) dipole directions
and
, respectively. The color bar has been modified to emphasize the minimum, the actual minimum and maximum is indicated in the title.
![Figure 9. Illustration of step (2) for situation (b): the figure shows the evaluation of Tg∗,h∗,m1∗ on the unit sphere, the green and purple dots indicate the locations of the possible (true) dipole directions d and d¯, respectively. The color bar has been modified to emphasize the minimum, the actual minimum and maximum is indicated in the title.](/cms/asset/d3f23a3c-fda3-40e5-af5c-02d3e10e8ce6/gipe_a_1438426_f0009_oc.gif)
5.2. The examples
We illustrate Procedure 5.1 for three different situations. All situations have in common that the potential V is given on , with
(which simulates the situation of a satellite flying at an altitude of around 380km above the Earth’s surface). Furthermore, V is assumed to be given only in discrete points on an equiangular grid of 40, 401 points. The magnetization
on
that generates V is varied among the three situations, but it is always supported in the lower hemisphere, i.e.
for
being fixed:
(a) |
| ||||
(a’) | Same as in (a) but only a noisy version | ||||
(b) |
| ||||
(c) |
|
where denotes the Sobolev norm of
(see, e.g. [Citation16] for more details). The first term in (Equation5.1
(1.1)
(1.1) ) simply represents a data misfit that measures the deviation of
from the known magnetic potential V, while the second term is a Tikhonov-type regularization to reduce noise amplification resulting from the ill-posedness of the downward continuation of the potential field data V to the surface
(this is well-studied and can be found, e.g. in [Citation24,Citation25] and references therein). The third term in (Equation5.1
(1.1)
(1.1) ) eventually penalizes magnetizations
that have contributions outside
, i.e. magnetizations that do not satisfy supp
. For the discretization of
, we expand
in terms of (vectorial) Abel-Poisson kernels:
(5.2)
(5.2)
where is a fixed parameter (influencing the localization of K; we use
) and
is a set of uniformly distributed points indicating the centers of the kernel K (in our case, we choose
different centers). Some general properties of the Abel-Poisson kernel K can be found, e.g. in [Citation14]. With this discretization, the minimization of
reduces to solving a set of linear equations with respect to the coefficients
. In step (2), we compute
from the
obtained in step (1). For the purpose of illustration, we simply plot
over the sphere to indicate where the minima
are located. Eventually, given
, in step (3) we minimize a functional
similar to (Equation5.1
(1.1)
(1.1) ) in order to obtain
. More precisely, we minimize
(5.4)
(5.4)
where denotes the induced magnetization
,
. For the numerical evaluation, we proceed similarly as for (Equation5.1
(1.1)
(1.1) ) by expanding Q in terms of (scalar) Abel Poisson kernels and solving a corresponding system of linear equations (details for a similar problem can be found in [Citation2]). Any numerical integrations necessary during the procedure are performed via the methods of [Citation26] (when the integration region comprises the entire sphere
or
, respectively) and [Citation27] (when the integration is only performed over a spherical cap
).
The magnetizations involved in examples (a)–(c) are all localized in the Southern hemisphere. Choosing magnetizations with a larger support typically makes the numerical solution of the problem more delicate. However, as indicated in Remark 5.2(b), this instability affects mainly the inverse problems in steps (1) and (3) of Procedure 5.1. Numerical examples for these problems with susceptibilities covering larger portions of the sphere can be found, e.g. in [Citation2]. In the paper at hand we want to focus on the reconstruction of dipole directions and stick to a single set-up for the localization of the magnetizations.
The results of step (1) and (2) for situation (a) are indicated in Figures and , respectively. The reconstruction nicely fits the true
. For brevity, we illustrated only the radial components. Figure shows that the minimum of
coincides with the true dipole direction
(which is indicated by a green dot). The corresponding results for the noisy situation (a’) are indicated in Figures and . We see that the reconstructed radial contribution of
shows some minor artifacts but the dipole direction
still coincides quite well with the minimum of
. However, we see that the actual minimum value is rather large in the noisy set-up. Therefore, to make sure that we found an admissible candidate
for the dipole direction, we proceed to step (3) with the approximation
of the minimum of
. The reconstructed susceptibility
is indicated in Figure and matches the true susceptibility Q. The data misfit
allows to compute the quantity
from Remark 5.2(c) and does not require the knowledge of Q. In this case, we have
, leading us to accept
as an approximation of the true dipole direction.
Steps (1) and (2) for situation (b), where no uniqueness of Q and is given, are shown in Figures and , respectively. In Figure , we indicated all three contributions (i.e. the radial contribution
and the surface curl- and surface divergence-free contributions
and
, respectively) of
and
. It is seen that the radial contribution and the surface curl-free contribution of the true and the reconstructed magnetization coincide, as is expected from Theorem 2.4. However, the surface divergence-free contribution is not uniquely determined and therefore may differ, as is the case here. But the latter has no impact on our further procedure. Figure shows that the two possible (true) dipole directions
and
are located at the minima of
(
and
are indicated by green and purple dots). Which direction is the correct one cannot be decided without further a priori geophysical information due to the intrinsic non-uniqueness.
For situation (c), the magnetization has been reconstructed very well as can be exemplarily seen for the radial component in Figure . Figure shows that the minima of
are located on the equator, i.e. any possible candidate for a dipole direction
must lie in the equatorial plane. However, although no noise was included in the data, the acquired minimum value of
deviates so significantly from zero that this leads us to conclude that the potential V cannot be generated by a dipole induced magnetization.
6. Conclusion
The fact that generally only the -contribution of a spherical magnetization
can be uniquely reconstructed from satellite magnetic field measurements leads to uniqueness issues, e.g. in determining possible dipole directions (assuming that the underlying magnetization is of induced type). The additional assumption that
is localized in some subregion of a spherical planetary surface allows to uniquely determine the
- and
-contributions of
(although
is still unknown), which implies that the radial contribution
and the tangential surface curl-free contribution
are determined uniquely. Here, we have shown that for the latter situation there exists a procedure for the determination of candidates for the dipole direction
and for the decision if a measured magnetic field can be produced by a dipole induced magnetization in the first place (a similar procedure has been derived for band-limited magnetizations, but in our examples in Section 5 we focused on the spatial localization constraint as we believe it to be more feasible for actual applications). The numerical treatment of the involved extremal problems allows various approaches and should be investigated in more detail for future applications. Also the cooperation with geophysicists will be required in order to embed the proposed method into a scenario applicable for real geophysical problems (such as paleopole estimations). The focus of the paper in its current form is on the presentation and illustration of the conceptual set-up for the improved reconstruction of dipole directions and the investigation of uniqueness issues.
Acknowledgements
The author thanks Foteini Vervelidou, GFZ Potsdam, for pointing out the problem of studying the reconstruction of dipole directions. Furthermore, the author would like to thank the anonymous reviewers for their helpful remarks and suggestions for the improvement of the paper.
Additional information
Funding
Notes
No potential conflict of interest was reported by the author.
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