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'''Isoline retrieval''' is a [[remote sensing]] [[Inverse problem|inverse method]] that retrieves one or more [[isoline]]s of a trace atmospheric constituent or variable. When used to validate another contour, it is the most accurate method possible for the task. When used to retrieve a whole field, it is a general, nonlinear inverse method and a robust estimator.
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==For validating advected contours==
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===Rationale===
 
Suppose we have, as in [[contour advection]], inferred knowledge of a
single contour or isoline of an atmospheric constituent, ''q''
and we wish to validate this against satellite remote-sensing data.
Since satellite instruments cannot measure the constituent directly,
we need to perform some sort of inversion.
In order to validate the contour, it is not necessary to know,
at any given point, the exact value of the constituent. We only need to
know whether it falls inside or outside, that is, is it greater
than or less than the value of the contour, ''q<sub>0</sub>''.
 
This is a classification problem.  Let:
 
: <math>
j = \begin{cases} 1; & q < q_0 \\
2; & q \geq q_0\end{cases}
</math>
 
be the discretized variable.
This will be related to the satellite ''measurement vector'', <math>\vec y</math>,
by some conditional probability, <math>P(\vec y|j)</math>,
which we approximate by collecting samples, called ''training data'', of both the
measurement vector and the state variable, ''q''.
By generating classification results over the region of interest
and using any contouring algorithm to separate the
two classes, the isoline will have been "retrieved."
 
The accuracy of a retrieval will be given by integrating
the conditional probability over the area of interest, ''A'':
 
:<math>
a = \frac {1}{A} \int_A P \left[c(\vec{r}) | \vec{y}(\vec{r}) \right]
                \, d\vec{r}
</math>
 
where ''c'' is the retrieved class at position, <math>\vec r</math>.
We can maximize this quantity by maximizing the value of the integrand
at each point:
 
:<math>
\max(a) = \frac{1}{A} \int_A \left \lbrace \max_j P \left [j |
        \vec{y}(\vec{r}) \right ] \right \rbrace \, d\vec{r}
</math>
 
Since this is the definition of maximum likelihood,
a [[statistical classification|classification algorithm]] based on [[maximum likelihood]]
is the most accurate method possible of validating an advected contour.
A good method for performing maximum likelihood classification
from a set of training data is [[variable kernel density estimation]].
 
===Training data===
 
There are two methods of generating the training data.
The most obvious is empirically, by simply matching measurements of
the variable, ''q'', with [[collocation (remote sensing)|collocated]]
measurements from the satellite instrument.  In this case,
no knowledge of the actual physics that produce the measurement
is required and the retrieval algorithm is purely statistical.
The second is with a forward model:
 
:<math>
\vec y = \vec f(\vec x) \,
</math>
 
where <math>\vec x</math> is the ''state vector'' and
''q = x<sub>k</sub>'' is a single component.
An advantage of this method is that state vectors need not
reflect actual atmospheric configurations, they need only
take on a state that could reasonably occur in the real atmosphere.
There are also none of the errors inherent in
most [[collocation (remote sensing)|collocation]] procedures,
e.g. because of offset errors in the locations of the paired samples
and differences in the footprint sizes of the two instruments.
Since retrievals will be biased towards more common states,
however, the statistics ought to reflect those in the real world.
 
===Error characterization===
 
The conditional probabilities, <math>P(\vec y|j)</math>, provide
excellent error characterization, therefore the classification
algorithm ought to return them.
We define the ''confidence rating'' by rescaling the conditional
probability:
 
: <math>
C = \frac{n_c P(c|\vec y) - 1}{n_c - 1}
</math>
 
where ''n<sub>c</sub>'' is the number of classes (in this case, two).
If ''C'' is zero, then the classification is little better than
chance, while if it is one, then it should be perfect.
To transform the confidence rating to a statistical ''tolerance'',
the following line integral can be applied to an isoline retrieval
for which the true isoline is known:
 
:<math>
\delta(C) = \frac{1}{l} \int_0^l h(C - C^\prime(\vec{r})) \, ds
</math>
 
where ''s'' is the path, ''l'' is the length of the isoline
and <math>C^\prime</math> is the retrieved confidence as a function
of position.
While it appears that the integral must be evaluated separately
for each value of the confidence rating, ''C'', in fact it may be
done for all values of ''C'' by sorting the confidence ratings of the
results, <math>C^\prime</math>.
The function relates the threshold value of the confidence rating
for which the tolerance is applicable.
That is, it defines a region that contains a fraction of the true
isoline equal to the tolerance.
 
===Example: water vapour from AMSU===
 
[[Image:tolerance from confidence.png|thumb|right|upright=1.5|alt=Tolerance vs. confidence|Statistical tolerance versus confidence rating for water-vapour isoline retrieval.]]
 
The [[Advanced Microwave Sounding Unit]] (AMSU) series of satellite instruments
are designed to detect temperature and water vapour.  They have a high
horizontal resolution (as little as 15&nbsp;km) and because they are
mounted on more than one satellite, full global coverage can be
obtained in less than one day.
Training data was generated using the second method from
[[European Centre for Medium-Range Weather Forecasts]] (ECMWF) ERA-40
data fed to a fast [[radiative transfer]] model called
[[RTTOV (radiative transfer code)|RTTOV]].
The function, <math>\delta(C)</math> has been generated from
simulated retrievals and is shown in the figure to the right.
This is then used to set the 90 percent tolerance in the figure
below by shading all the confidence ratings less than 0.8.
Thus we expect the true isoline to fall within the shading
90 percent of the time.
 
[[Image:ret colour.gif|thumb|center|upright=3|alt=Sample isoline retrieval|Water vapour isoline retrieved from AMSU measurements and compared with ECMWF reanalysis.]]
 
==For continuum retrievals==
 
[[Image:conditional probability proxy.png|thumb|left|upright=1.5|alt=The conditional probability as proxy for the continuum variable|Specific humidity versus conditional probabilities from water-vapour isoline retrieval.]]
 
Isoline retrieval is also useful for retrieving a continuum variable
and constitutes a general, [[nonlinear]] [[inverse method]].
It has the advantage over both a [[neural network]], as well as iterative
methods such as [[optimal estimation]] that invert the forward model
directly, in that there is no possibility of getting stuck in a
[[local minimum]].
 
There are a number of methods of reconstituting the continuum variable
from the discretized one.  Once a sufficient number of contours
have been retrieved, it is straightforward to [[interpolate]] between
them.  Conditional probabilities make a good [[Proxy (statistics)|proxy]] for
the continuum value.
 
Consider the transformation from a continuum to a discrete variable:
 
:<math>
P(1 | \vec{y}) = \int_{-\infty}^{q_0} P(q | \vec{y}) \, dq
</math>
 
:<math>
P(2 | \vec{y}) =  \int^{\infty}_{q_0} P(q | \vec{y}) \, dq
</math>
 
Suppose that <math>P(q | \vec y)</math> is given by a Gaussian:
 
:<math>
P(q | \vec y) = \frac{1}{\sqrt{2 \pi} \sigma_q}
\exp \left \lbrace - \frac{\left [q - \bar q (\vec y)\right ]^2}{2 \sigma_q} \right \rbrace
</math>
 
where <math>\bar q</math> is the expectation value and <math>\sigma_q</math>
is the standard deviation, then the conditional probability is related to the
continuum variable, ''q'', by the error function:
 
:<math>
R=P(2 | \vec{y})-P(1 | \vec{y}) = \mathrm{erf} \left [ \frac{q_0 - \bar q (\vec y)}{\sqrt 2 \sigma_q} \right ]
</math>
 
The figure shows conditional probability versus specific humidity for the example
retrieval discussed above.
 
===As a robust estimator===
 
The location of ''q''<sub>0</sub> is found by setting the conditional probabilities
of the two classes to be equal:
 
: <math>
\int_{-\infty}^{q_0} P(q | \vec{y}) \, dq =
\int^\infty_{q_0} P(q | \vec{y}) \, dq
</math>
 
In other words, equal amounts of the "zeroeth order moment" lie on either side
of ''q''<sub>0</sub>. This type of formulation is characteristic of a [[robust estimator]].
 
==References==
 
* {{Cite journal
| author = Peter Mills
| title = Isoline retrieval: An optimal method for validation of advected contours
| journal = Computers & Geosciences
| volume = 35
| number = 11
| pages = 2020–2031
| year = 2009
| doi = 10.1016/j.cageo.2008.12.015
| url = http://peteysoft.users.sourceforge.net/Mills2009.pdf
}}
 
* {{Cite journal
| author = Peter Mills
| title = Efficient statistical classification of satellite measurements
| journal = International Journal of Remote Sensing
| doi = 10.1080/01431161.2010.507795
| year = 2010
| url = http://peteysoft.users.sourceforge.net/TRES_A_507795.pdf
}}
 
==External links==
* [http://isoret.sourceforge.net Software for isoline retrieval]
 
[[Category:Remote sensing]]
[[Category:Inverse problems]]

Latest revision as of 08:28, 1 January 2015

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It'll have you on the edge of your seat and holding your breath for Zink to land this record-breaking backflip. One way to increase exercise fun is to find a friend to run with you. The price you can expect to pay for stems is actually determined by the materials used along with its weight. Sometimes they are internal (drum and coaster brakes), and sometimes they are external (disc brakes). Browse a number of the on-line forums to determine what other riders like and do not like about their bicycles.

The steeper the angles, the more beneficial it would be for stability and high speed pedaling. If you do it as soon as you get home, then its done and you can concentrate on eating and relaxing. Apply a generous amount of mountain bike lube to your chain as you move the pedals around backward. Mounting biking is a fun sport for professionals and beginners alike. There is a key point that you should always remember when going on any bicycle ride, especially one of great length.

With knowledge on the strengths and weakness of the MTB model, they are a great source of help. As a form of transport in itself bike riding is great but because of the design of these bikes you can travel over harsher terrain which will lead to you tossing in your old bike and traveling to work on your newly discovered fun machine. These four websites are important to serious bikers. People like to ride the mountain bike to those terrains because they enjoy the thrill and the adventure. You should be selective in choosing mountain bike tires since mountain bike is already made heavy and if you choose heavy tires you should consider yourself about how you will handle the bike and the terrain at the same time.

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