 |
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 | Model fitting by least squares |  |
![[pdf]](icons/pdf.png) |
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The relation (96) between the phases and the phase differences is
![\begin{displaymath}
\left[
\begin{array}{rrrr}
-1 & 1& 0& 0 \\
0 & 0& -1& 1 ...
...
\Delta \phi_{ac} \\
\Delta \phi_{bd}
\end{array}\right]
\end{displaymath}](img414.png) |
(97) |
Starting from the phase differences,
equation (97) hope to find all the phases themselves
because an additive constant cannot be found.
In other words,
the column vector
is in the null space.
Likewise, if we add phase increments while we move around a loop,
the sum should be zero.
Let the loop be
.
The phase increments that sum to zero are:
 |
(98) |
Rearranging to agree with the order in equation (97) yields
 |
(99) |
which says that the row vector
premultiplies (97),
yielding zero.
Rearrange again
 |
(100) |
and finally interchange signs and directions
(i.e.,
)
 |
(101) |
This is the finite-difference equivalent of
 |
(102) |
and is also
the
-component of the theorem that the curl of a gradient
vanishes for any
.
The four
summed around the
mesh
should add to zero.
I wondered what would happen if random complex numbers
were used for
,
,
, and
,
so I computed the four
s with equation (96),
and then computed the sum with (98).
They did sum to zero for 2/3 of my random numbers.
Otherwise,
with probability 1/6 each, they summed to
.
The nonvanishing curl represents a phase that is changing
too rapidly between the mesh points.
Figure 13 shows the locations
at Vesuvius where bad data occurs.
This is shown at two different resolutions.
The figure shows a tendency for
bad points with curl
to have a neighbor with
.
If Vesuvius were random noise instead of good data,
the planes in Figure 13 would be one-third covered with dots
but as expected, we see considerably fewer.
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screw
Figure 13.
Values of curl at Vesuvius.
The bad data locations at both coarse and fine resolution
tend to occur in pairs of opposite polarity.
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 |
 |
 |
 | Model fitting by least squares |  |
![[pdf]](icons/pdf.png) |
Next: Discontinuity in the solution
Up: VESUVIUS PHASE UNWRAPPING
Previous: Estimating the inverse gradient
2011-07-17