a fundamental inverse problem in geosciences
TRANSCRIPT
A fundamental inverse problem in geosciences
Predict the values of a spatial random field
(SRF) using a set of observed values of the
same and/or other SRFs.
nivuLy iii ,...,1 , )( =+=
)()}({ PmPuE =
),())}()(( ))()({( QPCQmQuPmPuE u=−−
?)( =Pu
trend of the unknown field
CV function
:)(uLi linear functionals :iv random noise
Setting the stage �
nivsvuLy iii
iPs
ii ,...,1 , )(
)(
=+=+=���
0s === }{ , 0}{ , 0)}({ EsEPuE i
vsy +=
Auxiliary hypotheses:
1) 0s === }{ , 0}{ , 0)}({ EsEPuE i
0Csv= vsy CCC +=
),( ],[ jiuji PPCLL ji=sC
1)
jvivjiji vvE σ }{ ],[ ==vC
),( ][T
)( iui PPCLiPu =sc
2)
3)
CV propagation law
Noise CV model
Signal CV model+
4)
Optimal generalized interpolation
1T −+=
Linear unbiased prediction of the unknown field
with minimum mean squared error
nivsvuLy iii
iPs
ii ,...,1 , )(
)(
=+=+=��� vsy +=
yCCc vss 1)( )(ˆ
T)(
−+= PuPu
− Least-squares collocation (LSC)
− Kriging
− Wiener-Kolmogorov (WK) theory
yCCCu vsus 1)( ˆ −
+=
“Hidden” characteristics of the LSC solution
The signal prediction algorithm is not affected
by the spatial distribution of the prediction points
(the LSC estimate at P is the same, regardless of the
number and/or the geometry of other prediction points).
yCCc vss 1)( )(ˆ
T)(
−+= QuQu
yCCc vss 1)( )(ˆ T
)(−
+= PuPu
... )(ˆ =Ru
Data points
Prediction points
iii vsy +=
number and/or the geometry of other prediction points).
yCCCu vsus 1)( ˆ −
+=
P
Q
R
“Hidden” characteristics of the LSC solution
Model-denial occurs through the LSC
estimation procedure, in the sense that:
yCCCu vsus 1)( ˆ −
+=
uusvsusu CCCCCC )( T1ˆ ≠+=
−
The auto-covariance structure of the estimated
SRF is different from the auto-covariance structure
of the corresponding true SRF (field smoothing).
),( ],[ jiuji PPC=uC
euu CCC −= ˆ
uue −= ˆ
Due to the fact that:
- Smoothing effectSmoothing effect in the field estimate
ueuu CCCC ˆ ≠−=
- Field “images” based on LSC are unsuitable for
).(ˆ Pu
- Field “images” based on LSC are unsuitable for applications where the spatial signal variabilityspatial signal variability is a key element for scientific inference.
- Signal details not inherent or proven by the actual data (i.e. artifacts) are notnot produced, but ..
).,( QPCu
- Inability to reproduce even the empirically determined CV function model
Example
2
)(1
C )( ),(
a
QPCQPC ouu ττ
+
=−==
2mgal 750 C =o
km 9.5 ξ = Spatial resolution: 2 km
Smoothed image that does
represent realistically the spatial
variability of the underlying field
Histogram of the LSC signal solution
-80 -60 -40 -20 0 20 40 60 80 1000
10
20
30
40
50
60
70
80Histogram of the true signal realization
Signal realization
Max = 65.30
Min = -76.85
Mean = 0.70
σ = 22.71
u
-80 -60 -40 -20 0 20 40 60 80 1000
10
20
30
40
50
60
70Histogram of the LSC signal solution
LSC solution
Max = 42.62
Min = -49.86
Mean = 2.95
σ = 15.39
theoretical σ = 27.39 mgal
ˆ u
Preliminary conclusions
− Signal predictions from LSC should be listed, not mappednot mapped!
− LSC is the optimal prediction method for localized signal recoverylocalized signal recovery (minimum pointwise MSE).
− The final result of LSC denies its fundamental building component (i.e. the CV function of the underlying unknown signal)!
− LSC is unsuitable for spatial field mappingspatial field mapping(fails to reproduce the model-based spatio-statistical variability of the unknown field).
A revised formulation
}ˆ{ ˆ uu ℜ=′
Apply a postApply a post--processing “correction” processing “correction”
algorithm (dealgorithm (de--smoothing transformation) smoothing transformation)
on the LSC solutionon the LSC solution
such that:
1) The CV structure of the SRF is preserved
uu CC ˆ =′
2) The estimation error remains small in some sense
eC ′of functional some minimize i.e.
uue −′=′ ˆ
uRu ˆ ˆ ⋅=′
A linear revised formulation
Linear transformation of the LSC solution
where R is a filtering matrix that needs to be
determined according to some optimality criteria
T)()( ˆ RICRICC uee −−+=′
determined according to some optimality criteria
Note that:
uue −′=′ ˆ
uue −= ˆ LSC estimation error
(LSC &R-filtering) estimation error
uRu ˆ ˆ =′
Filtering optimization
Determine the transformation matrix R
such that
T
uue −′=′ ˆ
subject to the optimal prediction criterion
uuu CRCRC T ˆˆ ==′ CV-matching constraint
T)()( ˆ RICRICC uee −−+=′
eC ′δ minimum δ =′eCtraceFrom LSC
The optimal matrix R
Solving the previous optimization problem,
we get the result:
2121212121 )( ˆ/////uuuuu CCCCCR −
=
2121212121ˆˆˆˆ )( ///// −−
= uuuuu CCCCCR
- Symmetric
- Positive definite
or equivalently
Alternative forms for the optimal filtering matrix R
Using the matrix identity: 21112/1 )( /−−= STSSST
we obtain the equivalent compact expressions for the matrix R
uuu CCCR 21)( ˆ/−
=
expressions for the matrix R
121ˆˆ )( −
=uuu CCCR
/
211 )( ˆˆ/
uuuCCCR
−=
21)( ˆ/−
= uuu CCCR
Prediction error
Co-variance matrix of the prediction error
If all eigenvalues of the filtering matrix R*
T)()( ˆ RICRICC uee −−+=′
If all eigenvalues of the filtering matrix R*
are larger than one, i.e.
)(2 )( ee CC tracetrace ×≤′
δRIR +=
then it can be shown that
positive definite matrix
* not necessarily optimal..
Test 1 (noise filtering)
2
)(1
C )(
a
C ou ττ
+
=
2mgal 220 C =o km 7 ξ =
Spatial resolution: 2 km
noise) (white mgal 35 σ =v
Signal realization
Max = 45.33
Min = -42.88
Mean = -0.04
σ = 14.96
LSC solution
Max = 27.42
Min = -29.10
ˆ u
u
theoretical σ = 14.83 mgal
Min = -29.10
Mean = 0.74
σ = 10.29
CV-adaptive solution
Max = 41.47
Min = -42.48
Mean = 0.73
σ = 14.64
ˆ u ′
LSC
estimation errors
Max = 28.70
Min = -31.94
Mean = 0.78
σ = 9.88
ˆ uu −
CV-adaptive
estimation errors
Max = 31.98
Min = -32.05
Mean = 0.77
σ = 11.01
ˆ uu −′
Test 2(noise filtering + spatial interpolation)
2C 220 mgalo = ξ 8 km=
Spatial resolution: 2 km
(white noise)σ 5 mgal v =2
)(1
C )(
a
C ou ττ
+
=
Max = 35.76
Min = -40.09
Mean = -1.19
σ = 14.94
LSC solution
Max = 31.04
Min = -24.38
ˆ u
uSignal realization
Min = -24.38
Mean = 0.67
σ = 8.85
Max = 32.48
Min = -28.56
Mean = 0.94
σ= 11.18
ˆ u ′
theoretical σ = 14.83 mgal
CV-adaptive solution
LSC estimation
errors
Max = 39.01
Min = -35.59
Mean = 1.86
σ = 11.58
ˆ uu −
CV-adaptive
estimation errors
Max = 34.25
Min = -36.92
Mean = 2.13
σ = 11.81
ˆ uu −′
Conclusions
− LSC provides optimal local accuracy, yet poor
global spatial rendering in SRF prediction problems.
− New prediction approach based on optimal de-
smoothing through CV-matching filtering;
i.e. reproduce the signal CV function with minimum i.e. reproduce the signal CV function with minimum i.e. reproduce the signal CV function with minimum i.e. reproduce the signal CV function with minimum loss in the MSE accuracyloss in the MSE accuracyloss in the MSE accuracyloss in the MSE accuracyloss in the MSE accuracyloss in the MSE accuracyloss in the MSE accuracyloss in the MSE accuracy
− Are there any “fundamental” issues hidden on the
trade-off between local and global accuracy in SRF
estimation from discrete data?
− Identify relevant application areas where global
spatial accuracy is an important issue (preserving
non-stationary patterns, spatial field mapping,F)