CN107341449A - A kind of GMS Calculation of precipitation method based on cloud mass changing features - Google Patents
A kind of GMS Calculation of precipitation method based on cloud mass changing features Download PDFInfo
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- G06V20/13—Satellite images
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- G—PHYSICS
- G01—MEASURING; TESTING
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- G06V10/26—Segmentation of patterns in the image field; Cutting or merging of image elements to establish the pattern region, e.g. clustering-based techniques; Detection of occlusion
- G06V10/267—Segmentation of patterns in the image field; Cutting or merging of image elements to establish the pattern region, e.g. clustering-based techniques; Detection of occlusion by performing operations on regions, e.g. growing, shrinking or watersheds
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- Y02A90/00—Technologies having an indirect contribution to adaptation to climate change
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Abstract
The invention belongs to Calculation of precipitation technical field, discloses a kind of GMS Calculation of precipitation method based on cloud mass changing features, including:Satellite Simulation of Precipitation parameter attribute collection is obtained to portray the generation of cloud precipitation and evolution, different dimension Cloud-Picture Characteristics parameters are normalized from most value method for normalizing;Structure based on before three layers to the satellite Calculation of precipitation model of type reverse transmittance nerve network, for the region Calculation of precipitation, and using the Simulation of Precipitation precision of multi objective system anlysis model.The rainfall distribution that the present invention is derived using Utilizing Satellite Remote Sensing Data can compensate for the deficiency of conventional meteorological observation, there is provided the precipitation information of more horn of plenty;Beneficial to Nowcasting is carried out, be advantageous to monitor flood, be advantageous to make geological disaster and give warning in advance, have great importance to improving weather forecast accuracy rate and preventing and reducing natural disasters.
Description
Technical field
The invention belongs to Calculation of precipitation technical field, more particularly to a kind of GMS based on cloud mass changing features
Calculation of precipitation method.
Background technology
With the development of meteorological satellite, the distribution of applied satellite data estimation precipitation and intensity, as Satellite data application
An importance also grow up simultaneously.Ground observation and aerological sounding website are sparse, are influenceed by earth's surface heating power difference,
The local of precipitation differs greatly.
Image segmentation is a classical image processing problem, some significant the purpose is to which piece image is divided into
Region, wherein each region has similar a feature and meaning, but the complexity and the diversity of target dealt with objects due to it,
The always difficult point and hot issue of computer vision field.Particularly further go deep into recently as technological revolution, image
It is segmented in increasing field such as industrial production, Video Applications, Medical Image Processing, biometric image processing, intelligent transportation, electricity
Sub- commercial affairs, E-Government, man-machine interface, virtual reality etc. are widely used.Rapid development and net with internet
The increase of network type and bandwidth, the decline of imaging device cost, caused image rapidly increase, the product based on image procossing with
Our daily life is also increasingly closely related.Image is split as a key technology in image procossing, therefore to figure
As the research of cutting techniques is not only with important theory value but also with good practical value
Image segmentation research starts from nineteen seventies, by the development of nearly half a century, it is proposed that a large amount of classical
Image segmentation algorithm.Traditional classic map picture segmentation mainly has Threshold segmentation, the segmentation based on edge, point based on region
Cut, the segmentation based on global optimization criterion and the segmentation based on statistics etc..Many algorithms all obtain in specific application scenarios
Good segmentation effect, but due to the diversification of image imaging mode and equipment, handle object diversity and body form not
The reasons such as systematicness cause a kind of no image segmentation algorithm to can be good at handling all types of images.
Image is segmented in also referred to as cluster analysis in statistics.Finite mixture model (Finite based on statistics in recent years
Mixture Mode, FMM) research it is very active always.But a distinct disadvantage of the FMM based on Gaussian Profile is that it is right
Noise is very sensitive.And Xue Shengshi distributions have heavier afterbody compared with Gaussian Profile, therefore it has well to noise
Robustness, it is the healthy and strong replacement of Gaussian Profile.
In summary, the problem of prior art is present be:Ground observation and aerological sounding website are sparse at present, by Ground Heat
The influence of power difference, the local of precipitation differ greatly;It is larger deviation to be also present in the data of Calculation of precipitation;Conventional images segmentation side
It in method, can not efficiently be split in the presence of noise, reduce the complexity for solving parametric procedure;And it can not improve
The robustness of image segmentation, improve the quality of image segmentation.
The content of the invention
The problem of existing for prior art, the invention provides a kind of GMS based on cloud mass changing features
Calculation of precipitation method.
The present invention is achieved in that a kind of GMS Calculation of precipitation system based on cloud mass changing features, institute
Stating the GMS Calculation of precipitation system based on cloud mass changing features includes:
Normalized module, for obtaining satellite Simulation of Precipitation parameter attribute collection to portray the generation of cloud precipitation and development
Process, different dimension Cloud-Picture Characteristics parameters are normalized from most value method for normalizing;
The normalized module utilizes this attribute of shadow region, by being carried out as follows to colored RGB images
Normalized:
Wherein:R, G, B are respectively original RGB component, and R ', G ', B ' are respectively the RGB component after normalizing;At B ' points
In amount, what shadow region mainly occupied is high pixel value end, the method by using Threshold segmentation to B ' component maps, sets one
Higher threshold value just obtains shadow region substantially;
The method of the Threshold segmentation includes:
1) image to be split is inputted, obtains the colouring information of image;Assuming that N number of pixel, these pictures are shared in a sub-picture
Element is divided into K class;
2) clusters number K and the likelihood function changing value of iteration ends and the maximum times of iteration are set, calculate pixel
Maximum a posteriori probability, the classification of pixel is obtained according to maximum a posteriori probability principle;Formula below is pressed in the solution of the average value of pixel
Solved,In formulaRepresent adjacent-systems, NnRepresent the number of neighbour in adjacent-systems;
3) initiation parameter, mean μ and covariance Σ are obtained using K- mean algorithms, then initializing variable, sets and become
Measure η=1, precision Λ=(η Σ)-1, v=1,The average of each pixel in pixel is tried to achieve using neighbor relationships
Specifically include:
Calculate parameter Λ=(the η Σ) of student t distributions-1;
Gaussian Profile and the multiplication relationship of gamma distribution can be decomposed into according to student t distributions
St (x | μ, Λ, v)=N (x | μ, (η Λ)-1Gam(η|v/2,v/2))
Wherein gamma distribution definition be
Using parameter η, Λ, μ, the v tried to achieve, the value that student t is distributed is tried to achieve;
4) current μ is utilizedkAnd ΣkGaussian Profile is calculated, calculates student t distributions;Calculate scene mixed coefficint πnkWith it is rear
Test probability znk;According to the gauss of distribution function and student's t distribution functions tried to achieve, scene mixed stocker is tried to achieve according to following two formula
Number πnkWith posterior probability znk
Obtain carrying out image by the image procossing submodule built in normalized module behind shadow region substantially
Processing;The processing of described image includes:Image procossing submodule is filtered place to gray level image using high pass/low pass filter
Reason is to construct the reference picture of image to be evaluated, using 3*3 mean filters, using each pixel of Filtering Template traversing graph picture,
Template center is placed in current pixel every time, the average value of all pixels is newly worth as current pixel using in template, and template is
Calculate before and after image filtering each edge half-tone information respectively, the image F statistical informations to be evaluated before filtering process
For sum_orig, the reference picture F2 statistical informations after filtering process are sum_filter, and specific formula for calculation is as follows:
Wherein, w1 and w2 is according to from the weights set with a distance from center pixel, w1=1, w2=1/3;
Using the ratio of the image filtering front and rear edges grey-level statistics drawn as fuzziness index, for convenience of evaluating,
Take larger for denominator, less is molecule, keeps the value between (0,1);
A fuzziness indication range [min, max] according to corresponding to being drawn the DMOS scopes of the best visual effect;Draw
Final image be shown in on the intelligent terminal screen of normalized module wireless connection;
Calculation of precipitation module, build based on to the satellite Calculation of precipitation model of type reverse transmittance nerve network, being used before three layers
In the region Calculation of precipitation, and using the Simulation of Precipitation precision of multi objective system anlysis model;
The multi objective system anlysis model calculation formula
In formula:--- the average value of meteorological variables in observation period;
yi--- the sampled instantaneous value of i-th of meteorological variables, i.e. sample in observation period, wherein, it is mistake, suspicious anon-normal
True sample should be discarded without in calculating, even yi=0;
N --- the total sample number in observation period, determined by sample frequency peace mean time section;
M --- correct sample number (m≤N) in observation period.
Further, the method for the Threshold segmentation also includes:
Calculate mean μkWith covariance Σk;Change ηkValue and try to achieve accuracy value
Further, the method for the Threshold segmentation also includes:The value of log-likelihood function is calculated, calculates its changing value
Or iterations just exits circulate operation more than stated number, initiation parameter step is otherwise performed;
The maximum a posteriori probability of pixel is calculated, the classification of pixel is obtained according to maximum a posteriori probability principle.
Further, in the value for calculating log-likelihood function, according to the log-likelihood function of whole image
The complexity of parameter is solved, introduces implicit variable znkSo that log-likelihood function is written as again
The internal relation that can be made up of according to student t distributions Gaussian Profile and gamma distribution product, log-likelihood letter
Number is re-written as following depicted
Further, L (Θ) is found a function on parameter ηkDerivative be
Wherein D represents the dimension of data, image for it is colored when D=3, D=1 during gray scale;SetObtain
Try to achieve ηkValue be
L (Θ) is found a function on parameter ΛkDerivative be
SetObtain equation
Try to achieve ΛkValue be
Further, L (Θ) is found a function on parameter μkDerivative be
SetObtain equation,
Try to achieve μkValue be
Further, the cycle-index for certain limit or iteration being reached when the rate of change of log-likelihood function value reaches certain
After input, according to maximum posteriori criterion
Obtain the mark of pixel.
Another object of the present invention is to provide a kind of GMS Calculation of precipitation side based on cloud mass changing features
Method, comprise the following steps:
Step 1, satellite Simulation of Precipitation parameter attribute collection is obtained to portray the generation of cloud precipitation and evolution, from most
Different dimension Cloud-Picture Characteristics parameters are normalized value method for normalizing;
Step 2, build based on before three layers to the satellite Calculation of precipitation model of type reverse transmittance nerve network, for the ground
Domain Calculation of precipitation, and using the Simulation of Precipitation precision of multi objective system anlysis model.
Advantages of the present invention and good effect are:The rainfall distribution derived using Utilizing Satellite Remote Sensing Data can be big
The deficiency of conventional meteorological observation is made up greatly, there is provided the precipitation information of more horn of plenty;Beneficial to Nowcasting is carried out, be advantageous to supervise
Flood is surveyed, is advantageous to make geological disaster and gives warning in advance, to improving weather forecast accuracy rate and preventing and reducing natural disasters with weight
The meaning wanted.To between the estimation result of type reverse transmittance nerve network satellite Calculation of precipitation model and rainfall gauge measured value before layer
Correlation can reach 0.57;Model estimation result is systematic to be underestimated less than normal, and imply that will have to the weak precipitation intensity in the region
It is preferably indicative.
A distinct disadvantage of FMM based on Gaussian Profile is that it does not account for the spatial relationship of pixel.Therefore to noise
Noise immunity it is not strong.The present invention has effectively drawn the direct spatial relationship of pixel, has more preferable robustness;
The present invention is had stronger noise immunity, can obtain preferably segmentation effect;
What scene hybrid parameter proposed by the present invention was shown is expressed as probability vector, and this avoid in most number space
It, which is solved, in mixed model needs the extra efficiency remedied calculating, improve algorithm;
There is inherent incidence relation in the present invention, with Gaussian Profile using the model of student t distributions so as to which student t be distributed
Gaussian Profile is converted to, on the one hand reduces the number of parameters of solution, on the other hand simplifies solution procedure so that the present invention is easily
In realization.
The present invention combines the advantage of spatial variations mixed model and the robustness of student t- distributions, it is proposed that one kind is based on learning
The spatial variations mixed model of Sheng Shi distributions.In the present invention, the weight function of definition is used for representing the spatial relationship between pixel,
The Gaussian Profile of the spatial relationship and pixel is closely related.Scene mixed coefficint is explicit to be expressed as probability vector.They
Automatically this restrictive condition of probability vector is met.Therefore the step for remedying calculating is eliminated in reasoning process, so as to simplify
Solution procedure, and then improve the high efficiency of algorithm.The present invention is based on log-likelihood function is maximized, in view of student t is distributed letter
Several complicated representative, according to student t distributions and the internal relation of Gaussian Profile, the solution of student's t distributed constants is converted to
The solution of Gaussian Distribution Parameters.This mode not only simplifies the number for solving parameter, and also reduces parametric solution process
Complexity so that whole Algorithm for Solving process is relatively simple.
The present invention has taken into full account the spatial relationship between pixel, while represents the scene mixed coefficint of pixel space relation
Shown is expressed as probability vector.Number of parameters needed for the present invention is much smaller than other models based on markov random file
Parameter, therefore it is easily achieved.In addition, carrying out the solution of parameter using expectation-maximization algorithm, the optimization of parameter is obtained
Value.
Image blur evaluation method provided by the invention, established different from traditional evaluation method in image to be evaluated certainly
On the basis of body structure feature, from the angle of relative evaluation, the reference picture of image to be evaluated is constructed using wave filter, is calculated
The ratio of image border statistical information is as evaluation index before and after change.The principle of the present invention is simple, realizes image blur
The content independence and real-time of evaluation, fuzziness that can quick and precisely between any image of evaluation comparison.
Brief description of the drawings
Fig. 1 is the GMS Calculation of precipitation method flow provided in an embodiment of the present invention based on cloud mass changing features
Figure.
Fig. 2 is the GMS Calculation of precipitation system signal provided in an embodiment of the present invention based on cloud mass changing features
Figure.
In figure:1st, normalized module;2nd, Calculation of precipitation module.
Embodiment
In order to make the purpose , technical scheme and advantage of the present invention be clearer, with reference to embodiments, to the present invention
It is further elaborated.It should be appreciated that the specific embodiments described herein are merely illustrative of the present invention, it is not used to
Limit the present invention.
The application principle of the present invention is explained in detail below in conjunction with the accompanying drawings.
As shown in figure 1, the GMS Calculation of precipitation side provided in an embodiment of the present invention based on cloud mass changing features
Method comprises the following steps:
S101:Satellite Simulation of Precipitation parameter attribute collection is obtained to portray the generation of cloud precipitation and evolution, from being most worth
Different dimension Cloud-Picture Characteristics parameters are normalized method for normalizing;
S102:Structure based on before three layers to the satellite Calculation of precipitation model of type reverse transmittance nerve network, for the region
Calculation of precipitation, and using the Simulation of Precipitation precision of multi objective system anlysis model.
As shown in Fig. 2 the GMS Calculation of precipitation system provided in an embodiment of the present invention based on cloud mass changing features
System, the GMS Calculation of precipitation system based on cloud mass changing features include:
Normalized module 1, for obtaining satellite Simulation of Precipitation parameter attribute collection to portray the generation of cloud precipitation and hair
Exhibition process, different dimension Cloud-Picture Characteristics parameters are normalized from most value method for normalizing;
The normalized module utilizes this attribute of shadow region, by being carried out as follows to colored RGB images
Normalized:
Wherein:R, G, B are respectively original RGB component, and R ', G ', B ' are respectively the RGB component after normalizing;At B ' points
In amount, what shadow region mainly occupied is high pixel value end, the method by using Threshold segmentation to B ' component maps, sets one
Higher threshold value just obtains shadow region substantially;
The method of the Threshold segmentation includes:
1) image to be split is inputted, obtains the colouring information of image;Assuming that N number of pixel, these pictures are shared in a sub-picture
Element is divided into K class;
2) clusters number K and the likelihood function changing value of iteration ends and the maximum times of iteration are set, calculate pixel
Maximum a posteriori probability, the classification of pixel is obtained according to maximum a posteriori probability principle;Formula below is pressed in the solution of the average value of pixel
Solved,In formulaRepresent adjacent-systems, NnRepresent the number of neighbour in adjacent-systems;
3) initiation parameter, mean μ and covariance Σ are obtained using K- mean algorithms, then initializing variable, sets and become
Measure η=1, precision Λ=(η Σ)-1, v=1,The average of each pixel in pixel is tried to achieve using neighbor relationships
Specifically include:
Calculate parameter Λ=(the η Σ) of student t distributions-1;
Gaussian Profile and the multiplication relationship of gamma distribution can be decomposed into according to student t distributions
St (x | μ, Λ, v)=N (x | μ, (η Λ)-1Gam(η|v/2,v/2))
Wherein gamma distribution definition be
Using parameter η, Λ, μ, the v tried to achieve, the value that student t is distributed is tried to achieve;
4) current μ is utilizedkAnd ΣkGaussian Profile is calculated, calculates student t distributions;Calculate scene mixed coefficint πnkWith it is rear
Test probability znk;According to the gauss of distribution function and student's t distribution functions tried to achieve, scene mixed stocker is tried to achieve according to following two formula
Number πnkWith posterior probability znk
Obtain carrying out image by the image procossing submodule built in normalized module behind shadow region substantially
Processing;The processing of described image includes:Image procossing submodule is filtered place to gray level image using high pass/low pass filter
Reason is to construct the reference picture of image to be evaluated, using 3*3 mean filters, using each pixel of Filtering Template traversing graph picture,
Template center is placed in current pixel every time, the average value of all pixels is newly worth as current pixel using in template, and template is
Calculate before and after image filtering each edge half-tone information respectively, the image F statistical informations to be evaluated before filtering process
For sum_orig, the reference picture F2 statistical informations after filtering process are sum_filter, and specific formula for calculation is as follows:
Wherein, w1 and w2 is according to from the weights set with a distance from center pixel, w1=1, w2=1/3;
Using the ratio of the image filtering front and rear edges grey-level statistics drawn as fuzziness index, for convenience of evaluating,
Take larger for denominator, less is molecule, keeps the value between (0,1);
A fuzziness indication range [min, max] according to corresponding to being drawn the DMOS scopes of the best visual effect;Draw
Final image be shown in on the intelligent terminal screen of normalized module wireless connection;
Calculation of precipitation module 2, build based on to the satellite Calculation of precipitation model of type reverse transmittance nerve network, being used before three layers
In the region Calculation of precipitation, and using the Simulation of Precipitation precision of multi objective system anlysis model;
The multi objective system anlysis model calculation formula
In formula:--- the average value of meteorological variables in observation period;
yi--- the sampled instantaneous value of i-th of meteorological variables, i.e. sample in observation period, wherein, it is mistake, suspicious anon-normal
True sample should be discarded without in calculating, even yi=0;
N --- the total sample number in observation period, determined by sample frequency peace mean time section;
M --- correct sample number (m≤N) in observation period.
Further, the method for the Threshold segmentation also includes:
Calculate mean μkWith covariance Σk;Change ηkValue and try to achieve accuracy value
The method of the Threshold segmentation also includes:The value of log-likelihood function is calculated, calculates its changing value
Or iterations just exits circulate operation more than stated number, initiation parameter step is otherwise performed;
The maximum a posteriori probability of pixel is calculated, the classification of pixel is obtained according to maximum a posteriori probability principle.
In the value for calculating log-likelihood function, according to the log-likelihood function of whole image
The complexity of parameter is solved, introduces implicit variable znkSo that log-likelihood function is written as again
The internal relation that can be made up of according to student t distributions Gaussian Profile and gamma distribution product, log-likelihood letter
Number is re-written as following depicted
L (Θ) is found a function on parameter ηkDerivative be
Wherein D represents the dimension of data, image for it is colored when D=3, D=1 during gray scale;SetObtain
Try to achieve ηkValue be
L (Θ) is found a function on parameter ΛkDerivative be
SetObtain equation
Try to achieve ΛkValue be
L (Θ) is found a function on parameter μkDerivative be
SetObtain equation,
Try to achieve μkValue be
After the cycle-index that the rate of change of log-likelihood function value reaches certain limit or iteration reaches certain input,
According to maximum posteriori criterion
Obtain the mark of pixel.
The method GMS infrared band of the present invention can relatively accurately disclose the precipitation mechanism of cloud, higher time point
Resolution remote sensing images can monitor the change details of cloud atlas, and obtain the Simulation of Precipitation parameter that can reflect cloud atlas Characteristics of Precipitation;
Artificial neural network can preferably portray the non-linear rule of the region satellite Characteristics of Precipitation;To type Back propagation neural before three layers
The estimation result of network satellite Calculation of precipitation model can reach 0.57 with the correlation between rainfall gauge measured value.Model estimation knot
Fruit is systematic underestimate it is less than normal, imply that will have to the weak precipitation intensity in the region it is preferably indicative.
The foregoing is merely illustrative of the preferred embodiments of the present invention, is not intended to limit the invention, all essences in the present invention
All any modification, equivalent and improvement made within refreshing and principle etc., should be included in the scope of the protection.
Claims (8)
1. a kind of GMS Calculation of precipitation system based on cloud mass changing features, it is characterised in that described to be based on cloud mass
The GMS Calculation of precipitation system of changing features includes:
Normalized module, the generation of cloud precipitation and developed with portraying for obtaining satellite Simulation of Precipitation parameter attribute collection
Journey, different dimension Cloud-Picture Characteristics parameters are normalized from most value method for normalizing;
The normalized module utilizes this attribute of shadow region, by carrying out following normalizing to colored RGB images
Change is handled:
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Wherein:R, G, B are respectively original RGB component, and R ', G ', B ' are respectively the RGB component after normalizing;In B ' components,
What shadow region mainly occupied is high pixel value end, the method by using Threshold segmentation to B ' component maps, is set one higher
Threshold value just obtain shadow region substantially;
The method of the Threshold segmentation includes:
1) image to be split is inputted, obtains the colouring information of image;Assuming that N number of pixel, these pixel quilts are shared in a sub-picture
It is divided into K class;
2) clusters number K and the likelihood function changing value of iteration ends and the maximum times of iteration are set, calculate the maximum of pixel
Posterior probability, the classification of pixel is obtained according to maximum a posteriori probability principle;The solution of the average value of pixel is carried out by formula below
Solve,θ in formulanRepresent adjacent-systems, NnRepresent the number of neighbour in adjacent-systems;
3) initiation parameter, mean μ and covariance Σ are obtained using K- mean algorithms, then initializing variable, setting variable η=
1, precision Λ=(η Σ)-1, v=1,The average of each pixel in pixel is tried to achieve using neighbor relationshipsSpecific bag
Include:
Calculate parameter Λ=(the η Σ) of student t distributions-1;
Gaussian Profile and the multiplication relationship of gamma distribution can be decomposed into according to student t distributions
St (x | μ, Λ, v)=N (x | μ, (η Λ)-1Gam(η|v/2,v/2))
Wherein gamma distribution definition be
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</mfrac>
<mo>)</mo>
</mrow>
<mrow>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mo>/</mo>
<mn>2</mn>
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</mrow>
</msup>
<mi>exp</mi>
<mrow>
<mo>(</mo>
<mrow>
<mo>-</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mrow>
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</mrow>
</mrow>
Using parameter η, Λ, μ, the v tried to achieve, the value that student t is distributed is tried to achieve;
4) current μ is utilizedkAnd ΣkGaussian Profile is calculated, calculates student t distributions;Calculate scene mixed coefficint πnkAnd posterior probability
znk;According to the gauss of distribution function and student's t distribution functions tried to achieve, scene mixed coefficint π is tried to achieve according to following two formulank
With posterior probability znk
<mrow>
<msub>
<mi>&pi;</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>=</mo>
<mfrac>
<mrow>
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</mrow>
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</munderover>
<msub>
<mi>&delta;</mi>
<mi>j</mi>
</msub>
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</msub>
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</mrow>
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<msub>
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<mi>n</mi>
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</munder>
<mi>N</mi>
<mo>(</mo>
<mrow>
<msub>
<mi>x</mi>
<mi>m</mi>
</msub>
<mo>|</mo>
<msub>
<mi>&Theta;</mi>
<mi>k</mi>
</msub>
</mrow>
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<mo>)</mo>
</mrow>
</mrow>
<mrow>
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<mo>&Sigma;</mo>
<mrow>
<mi>j</mi>
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</mrow>
<mi>K</mi>
</munderover>
<mi>exp</mi>
<mrow>
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</msub>
<mo>|</mo>
<msub>
<mi>&Theta;</mi>
<mi>j</mi>
</msub>
</mrow>
<mo>)</mo>
<mo>)</mo>
</mrow>
</mrow>
</mfrac>
</mrow>
<mrow>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>=</mo>
<mfrac>
<mrow>
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<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mi>S</mi>
<mi>t</mi>
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<mi>x</mi>
<mi>n</mi>
</msub>
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<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
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<mo>&Sigma;</mo>
<mrow>
<mi>j</mi>
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</mrow>
<mi>K</mi>
</munderover>
<msub>
<mi>&pi;</mi>
<mrow>
<mi>n</mi>
<mi>j</mi>
</mrow>
</msub>
<mi>S</mi>
<mi>t</mi>
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</msub>
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<mi>&theta;</mi>
<mi>j</mi>
</msub>
<mo>)</mo>
</mrow>
</mrow>
</mfrac>
<mo>;</mo>
</mrow>
Obtain carrying out behind shadow region substantially the processing of image by the image procossing submodule built in normalized module;
The processing of described image includes:Image procossing submodule using high pass/low pass filter to gray level image be filtered processing with
The reference picture of image to be evaluated is constructed, using 3*3 mean filters, using each pixel of Filtering Template traversing graph picture, every time
Template center is placed in current pixel, the average value of all pixels is newly worth as current pixel using in template, and template is
Calculate before and after image filtering each edge half-tone information respectively, the image F statistical informations to be evaluated before filtering process are
Sum_orig, the reference picture F2 statistical informations after filtering process are sum_filter, and specific formula for calculation is as follows:
<mrow>
<mtable>
<mtr>
<mtd>
<mrow>
<mi>s</mi>
<mi>u</mi>
<mi>m</mi>
<mo>_</mo>
<mi>o</mi>
<mi>r</mi>
<mi>i</mi>
<mi>g</mi>
<mo>=</mo>
<mi>w</mi>
<mn>1</mn>
<mo>&times;</mo>
<mrow>
<mo>(</mo>
<mrow>
<mo>|</mo>
<mi>F</mi>
<mrow>
<mo>(</mo>
<mrow>
<mi>i</mi>
<mo>,</mo>
<mi>j</mi>
</mrow>
<mo>)</mo>
</mrow>
<mo>-</mo>
<mi>F</mi>
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<mo>(</mo>
<mrow>
<mi>i</mi>
<mo>-</mo>
<mn>1</mn>
<mo>,</mo>
<mi>j</mi>
</mrow>
<mo>)</mo>
</mrow>
<mo>|</mo>
<mo>+</mo>
<mo>|</mo>
<mi>F</mi>
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</mrow>
<mo>-</mo>
<mi>F</mi>
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<mi>i</mi>
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<mn>1</mn>
</mrow>
<mo>)</mo>
</mrow>
<mo>|</mo>
<mo>+</mo>
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<mi>F</mi>
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<mo>|</mo>
<mi>F</mi>
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</mrow>
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</mrow>
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</mtd>
</mtr>
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<mo>+</mo>
<mi>w</mi>
<mn>2</mn>
<mo>&times;</mo>
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<mi>F</mi>
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<mi>i</mi>
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<mi>j</mi>
</mrow>
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</mrow>
<mo>-</mo>
<mi>F</mi>
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<mo>(</mo>
<mrow>
<mi>i</mi>
<mo>-</mo>
<mn>1</mn>
<mo>,</mo>
<mi>j</mi>
<mo>-</mo>
<mn>1</mn>
</mrow>
<mo>)</mo>
</mrow>
<mo>|</mo>
<mo>+</mo>
<mo>|</mo>
<mi>F</mi>
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<mi>i</mi>
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</mrow>
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</mrow>
<mo>-</mo>
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<mi>i</mi>
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<mn>1</mn>
<mo>,</mo>
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</mrow>
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</mrow>
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</mrow>
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</mrow>
</mrow>
</mtd>
</mtr>
</mtable>
<mo>,</mo>
</mrow>
<mrow>
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<mtd>
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<mi>s</mi>
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<mi>f</mi>
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<mi>w</mi>
<mn>1</mn>
<mo>&times;</mo>
<mrow>
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<mi>F</mi>
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<mrow>
<mi>i</mi>
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<mo>,</mo>
<mi>j</mi>
</mrow>
<mo>)</mo>
</mrow>
<mo>|</mo>
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<mi>F</mi>
<mn>2</mn>
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<mi>i</mi>
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<mrow>
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<mi>i</mi>
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<mi>j</mi>
</mrow>
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<mo>-</mo>
<mi>F</mi>
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</mrow>
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</mrow>
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</mrow>
</mrow>
</mtd>
</mtr>
</mtable>
<mo>,</mo>
</mrow>
Wherein, w1 and w2 is according to from the weights set with a distance from center pixel, w1=1, w2=1/3;
Using the ratio of the image filtering front and rear edges grey-level statistics drawn as fuzziness index, for convenience of evaluating, take compared with
It is big for denominator, less is molecule, keeps the value between (0,1);
A fuzziness indication range [min, max] according to corresponding to being drawn the DMOS scopes of the best visual effect;Draw most
Whole image be shown in on the intelligent terminal screen of normalized module wireless connection;
Calculation of precipitation module, build based on before three layers to the satellite Calculation of precipitation model of type reverse transmittance nerve network, for this
Region Calculation of precipitation, and using the Simulation of Precipitation precision of multi objective system anlysis model;
The multi objective system anlysis model calculation formula
<mrow>
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</mover>
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<mfrac>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>i</mi>
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</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>y</mi>
<mi>i</mi>
</msub>
</mrow>
<mi>m</mi>
</mfrac>
<mo>;</mo>
</mrow>
In formula:--- the average value of meteorological variables in observation period;
yi--- the sampled instantaneous value of i-th of meteorological variables, i.e. sample in observation period, wherein, mistake, suspicious incorrect sample
It should be discarded without in calculating, even yi=0;
N --- the total sample number in observation period, determined by sample frequency peace mean time section;
M --- correct sample number (m≤N) in observation period.
2. the GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 1, it is characterised in that
The method of the Threshold segmentation also includes:
Calculate mean μkWith covariance Σk;Change ηkValue and try to achieve accuracy value
3. the GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 1, it is characterised in that
The method of the Threshold segmentation also includes:The value of log-likelihood function is calculated, calculates its changing value
<mrow>
<mfrac>
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</mrow>
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</mrow>
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</mrow>
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<mo><</mo>
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<mrow>
<mo>-</mo>
<mn>5</mn>
</mrow>
</msup>
</mrow>
Or iterations just exits circulate operation more than stated number, initiation parameter step is otherwise performed;
The maximum a posteriori probability of pixel is calculated, the classification of pixel is obtained according to maximum a posteriori probability principle.
4. the GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 1, it is characterised in that
In the value for calculating log-likelihood function, according to the log-likelihood function of whole image
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</mrow>
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</munderover>
<mi>log</mi>
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</mrow>
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<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
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</mrow>
<mi>N</mi>
</munderover>
<mi>l</mi>
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</mrow>
</msub>
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</mover>
<mo>|</mo>
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<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>,</mo>
<msub>
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<mi>k</mi>
</msub>
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<mi>v</mi>
<mi>k</mi>
</msub>
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The complexity of parameter is solved, introduces implicit variable znkSo that log-likelihood function is written as again
<mrow>
<mi>L</mi>
<mrow>
<mo>(</mo>
<mi>&Theta;</mi>
<mo>)</mo>
</mrow>
<mo>=</mo>
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<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>k</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>K</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>{</mo>
<msub>
<mi>log&pi;</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>+</mo>
<mi>log</mi>
<mi> </mi>
<mi>S</mi>
<mi>t</mi>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>|</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>,</mo>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mo>,</mo>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mo>}</mo>
<mo>;</mo>
</mrow>
The internal relation that can be made up of according to student t distributions Gaussian Profile and gamma distribution product, log-likelihood function quilt
It is re-written as following depicted
<mfenced open = "" close = "">
<mtable>
<mtr>
<mtd>
<mrow>
<mi>L</mi>
<mrow>
<mo>(</mo>
<mi>&Theta;</mi>
<mo>)</mo>
</mrow>
<mo>=</mo>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>k</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>K</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>{</mo>
<msub>
<mi>log&pi;</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>-</mo>
<mfrac>
<mi>D</mi>
<mn>2</mn>
</mfrac>
<mi>l</mi>
<mi>o</mi>
<mi>g</mi>
<mrow>
<mo>(</mo>
<mn>2</mn>
<mi>&pi;</mi>
<mo>)</mo>
</mrow>
<mo>+</mo>
<mfrac>
<mn>1</mn>
<mn>2</mn>
</mfrac>
<mi>l</mi>
<mi>o</mi>
<mi>g</mi>
<mo>|</mo>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mo>|</mo>
<mo>-</mo>
<mfrac>
<mn>1</mn>
<mn>2</mn>
</mfrac>
<msup>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mo>}</mo>
</mrow>
</mtd>
</mtr>
<mtr>
<mtd>
<mrow>
<mo>+</mo>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>k</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>K</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mrow>
<mo>{</mo>
<mrow>
<mo>-</mo>
<mi>log</mi>
<mi>&Gamma;</mi>
<mrow>
<mo>(</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mo>)</mo>
</mrow>
<mo>+</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mi>log</mi>
<mrow>
<mo>(</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mo>)</mo>
</mrow>
<mo>+</mo>
<mrow>
<mo>(</mo>
<mrow>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mo>-</mo>
<mn>1</mn>
</mrow>
<mo>)</mo>
</mrow>
<msub>
<mi>log&eta;</mi>
<mi>k</mi>
</msub>
<mo>-</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>}</mo>
</mrow>
<mo>.</mo>
</mrow>
</mtd>
</mtr>
</mtable>
</mfenced>
5. the GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 4, it is characterised in that
L (Θ) is found a function on parameter ηkDerivative be
<mrow>
<mfrac>
<mrow>
<mo>&part;</mo>
<mi>L</mi>
<mrow>
<mo>(</mo>
<mi>&Theta;</mi>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
<mo>&part;</mo>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mrow>
</mfrac>
<mo>=</mo>
<munderover>
<mi>&Sigma;</mi>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>&lsqb;</mo>
<mfrac>
<mi>D</mi>
<mrow>
<mn>2</mn>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mrow>
</mfrac>
<mo>-</mo>
<mfrac>
<mn>1</mn>
<mn>2</mn>
</mfrac>
<msup>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mo>-</mo>
<mrow>
<mo>(</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mo>-</mo>
<mn>1</mn>
<mo>)</mo>
</mrow>
<mfrac>
<mn>1</mn>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mfrac>
<mo>-</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mo>&rsqb;</mo>
</mrow>
Wherein D represents the dimension of data, image for it is colored when D=3, D=1 during gray scale;SetObtain
<mrow>
<munderover>
<mi>&Sigma;</mi>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mrow>
<mo>&lsqb;</mo>
<mrow>
<mfrac>
<mi>D</mi>
<mrow>
<mn>2</mn>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mrow>
</mfrac>
<mo>-</mo>
<mfrac>
<mn>1</mn>
<mn>2</mn>
</mfrac>
<msup>
<mrow>
<mo>(</mo>
<mrow>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mrow>
<mo>(</mo>
<mrow>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>)</mo>
</mrow>
<mo>-</mo>
<mrow>
<mo>(</mo>
<mrow>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
<mo>-</mo>
<mn>1</mn>
</mrow>
<mo>)</mo>
</mrow>
<mfrac>
<mn>1</mn>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
</mfrac>
<mo>-</mo>
<mfrac>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mn>2</mn>
</mfrac>
</mrow>
<mo>&rsqb;</mo>
</mrow>
<mo>=</mo>
<mn>0</mn>
</mrow>
Try to achieve ηkValue be
<mrow>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
<mo>=</mo>
<mfrac>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mrow>
<mo>(</mo>
<mi>D</mi>
<mo>-</mo>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mo>+</mo>
<mn>2</mn>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>&lsqb;</mo>
<msup>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mo>+</mo>
<msub>
<mi>v</mi>
<mi>k</mi>
</msub>
<mo>&rsqb;</mo>
</mrow>
</mfrac>
<mo>;</mo>
</mrow>
L (Θ) is found a function on parameter ΛkDerivative be
<mrow>
<mfrac>
<mrow>
<mo>&part;</mo>
<mi>L</mi>
<mrow>
<mo>(</mo>
<mi>&Theta;</mi>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
<mo>&part;</mo>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
</mrow>
</mfrac>
<mo>=</mo>
<mfrac>
<mn>1</mn>
<mn>2</mn>
</mfrac>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mrow>
<mo>(</mo>
<msubsup>
<mi>&Lambda;</mi>
<mi>k</mi>
<mrow>
<mo>-</mo>
<mn>1</mn>
</mrow>
</msubsup>
<mo>-</mo>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
<msup>
<mrow>
<mo>(</mo>
<mrow>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<mo>(</mo>
<mrow>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>)</mo>
<mo>)</mo>
</mrow>
</mrow>
SetObtain equation
<mrow>
<mfrac>
<mn>1</mn>
<mn>2</mn>
</mfrac>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mrow>
<mo>(</mo>
<msubsup>
<mi>&Lambda;</mi>
<mi>k</mi>
<mrow>
<mo>-</mo>
<mn>1</mn>
</mrow>
</msubsup>
<mo>-</mo>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
<msup>
<mrow>
<mo>(</mo>
<mrow>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<mo>(</mo>
<mrow>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
<mo>)</mo>
<mo>)</mo>
</mrow>
<mo>=</mo>
<mn>0</mn>
</mrow>
Try to achieve ΛkValue be
<mrow>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mo>=</mo>
<msup>
<mrow>
<mo>&lsqb;</mo>
<mfrac>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<msub>
<mi>&eta;</mi>
<mi>k</mi>
</msub>
<msup>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mi>T</mi>
</msup>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
</mrow>
</mfrac>
<mo>&rsqb;</mo>
</mrow>
<mrow>
<mo>-</mo>
<mn>1</mn>
</mrow>
</msup>
<mo>.</mo>
</mrow>
6. the GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 5, it is characterised in that
L (Θ) is found a function on parameter μkDerivative be
<mrow>
<mfrac>
<mrow>
<mo>&part;</mo>
<mi>L</mi>
<mrow>
<mo>(</mo>
<mi>&Theta;</mi>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
<mo>&part;</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
</mfrac>
<mo>=</mo>
<mo>-</mo>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>&lsqb;</mo>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mo>&rsqb;</mo>
</mrow>
Set
<mrow>
<mfrac>
<mrow>
<mo>&part;</mo>
<mi>L</mi>
<mrow>
<mo>(</mo>
<mi>&Theta;</mi>
<mo>)</mo>
</mrow>
</mrow>
<mrow>
<mo>&part;</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
</mrow>
</mfrac>
<mo>=</mo>
<mn>0</mn>
<mo>,</mo>
</mrow>
Obtain equation,
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>&lsqb;</mo>
<msub>
<mi>&Lambda;</mi>
<mi>k</mi>
</msub>
<mrow>
<mo>(</mo>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
<mo>-</mo>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>)</mo>
</mrow>
<mo>&rsqb;</mo>
<mo>=</mo>
<mn>0</mn>
</mrow>
Try to achieve μkValue be
<mrow>
<msub>
<mi>&mu;</mi>
<mi>k</mi>
</msub>
<mo>=</mo>
<mfrac>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mover>
<msub>
<mi>x</mi>
<mi>n</mi>
</msub>
<mo>&OverBar;</mo>
</mover>
</mrow>
<mrow>
<munderover>
<mo>&Sigma;</mo>
<mrow>
<mi>n</mi>
<mo>=</mo>
<mn>1</mn>
</mrow>
<mi>N</mi>
</munderover>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
</mrow>
</mfrac>
<mo>.</mo>
</mrow>
7. the GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 3, it is characterised in that
After the cycle-index that the rate of change of log-likelihood function value reaches certain limit or iteration reaches certain input, according to maximum
Posterior probability criterion
<mrow>
<mi>arg</mi>
<munder>
<mrow>
<mi>m</mi>
<mi>a</mi>
<mi>x</mi>
</mrow>
<mi>k</mi>
</munder>
<mo>{</mo>
<msub>
<mi>z</mi>
<mrow>
<mi>n</mi>
<mi>k</mi>
</mrow>
</msub>
<mo>}</mo>
</mrow>
Obtain the mark of pixel.
8. a kind of GMS Calculation of precipitation system based on cloud mass changing features as claimed in claim 1 based on cloud mass
The GMS Calculation of precipitation method of changing features, it is characterised in that the static meteorology based on cloud mass changing features
Satellite Calculation of precipitation method comprises the following steps:
Step 1, satellite Simulation of Precipitation parameter attribute collection is obtained to portray the generation of cloud precipitation and evolution, is returned from most value
Different dimension Cloud-Picture Characteristics parameters are normalized one change method;
Step 2, build based on to the satellite Calculation of precipitation model of type reverse transmittance nerve network, being dropped before three layers for the region
Water is estimated, and uses the Simulation of Precipitation precision of multi objective system anlysis model.
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