CN115204317A - Sound velocity profile continuation method and system based on orthogonal empirical function decomposition - Google Patents

Sound velocity profile continuation method and system based on orthogonal empirical function decomposition Download PDF

Info

Publication number
CN115204317A
CN115204317A CN202211118337.3A CN202211118337A CN115204317A CN 115204317 A CN115204317 A CN 115204317A CN 202211118337 A CN202211118337 A CN 202211118337A CN 115204317 A CN115204317 A CN 115204317A
Authority
CN
China
Prior art keywords
sound velocity
velocity profile
depth
sea
full
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Granted
Application number
CN202211118337.3A
Other languages
Chinese (zh)
Other versions
CN115204317B (en
Inventor
徐天河
黄威
高凡
王君婷
刘杨范
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Shandong University
Original Assignee
Shandong University
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Shandong University filed Critical Shandong University
Priority to CN202211118337.3A priority Critical patent/CN115204317B/en
Publication of CN115204317A publication Critical patent/CN115204317A/en
Application granted granted Critical
Publication of CN115204317B publication Critical patent/CN115204317B/en
Active legal-status Critical Current
Anticipated expiration legal-status Critical

Links

Images

Classifications

    • GPHYSICS
    • G06COMPUTING; CALCULATING OR COUNTING
    • G06FELECTRIC DIGITAL DATA PROCESSING
    • G06F17/00Digital computing or data processing equipment or methods, specially adapted for specific functions
    • G06F17/10Complex mathematical operations
    • G06F17/16Matrix or vector computation, e.g. matrix-matrix or matrix-vector multiplication, matrix factorization
    • GPHYSICS
    • G06COMPUTING; CALCULATING OR COUNTING
    • G06FELECTRIC DIGITAL DATA PROCESSING
    • G06F17/00Digital computing or data processing equipment or methods, specially adapted for specific functions
    • G06F17/10Complex mathematical operations
    • G06F17/18Complex mathematical operations for evaluating statistical data, e.g. average values, frequency distributions, probability functions, regression analysis
    • YGENERAL TAGGING OF NEW TECHNOLOGICAL DEVELOPMENTS; GENERAL TAGGING OF CROSS-SECTIONAL TECHNOLOGIES SPANNING OVER SEVERAL SECTIONS OF THE IPC; TECHNICAL SUBJECTS COVERED BY FORMER USPC CROSS-REFERENCE ART COLLECTIONS [XRACs] AND DIGESTS
    • Y02TECHNOLOGIES OR APPLICATIONS FOR MITIGATION OR ADAPTATION AGAINST CLIMATE CHANGE
    • Y02ATECHNOLOGIES FOR ADAPTATION TO CLIMATE CHANGE
    • Y02A90/00Technologies having an indirect contribution to adaptation to climate change
    • Y02A90/10Information and communication technologies [ICT] supporting adaptation to climate change, e.g. for weather forecasting or climate simulation

Landscapes

  • Engineering & Computer Science (AREA)
  • Physics & Mathematics (AREA)
  • General Physics & Mathematics (AREA)
  • Mathematical Physics (AREA)
  • Data Mining & Analysis (AREA)
  • Computational Mathematics (AREA)
  • Mathematical Optimization (AREA)
  • Theoretical Computer Science (AREA)
  • Pure & Applied Mathematics (AREA)
  • Mathematical Analysis (AREA)
  • Algebra (AREA)
  • Databases & Information Systems (AREA)
  • Software Systems (AREA)
  • General Engineering & Computer Science (AREA)
  • Operations Research (AREA)
  • Probability & Statistics with Applications (AREA)
  • Bioinformatics & Cheminformatics (AREA)
  • Bioinformatics & Computational Biology (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Evolutionary Biology (AREA)
  • Computing Systems (AREA)
  • Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)

Abstract

The invention provides a sound velocity profile extension method and system based on orthogonal empirical function decomposition, which relate to the technical field of ocean acoustic application and are used for solving the problem that a deep sea part extended by the existing method does not accord with the real sound velocity distribution rule of the deep sea in a region; and constructing an extended full-sea-depth sound velocity profile according to the characteristic vector coefficients and the sample data of the full-sea-depth historical sound velocity profile, and by the mode, matching the actually measured sound velocity value part of the sound velocity profile to be extended with high precision and ensuring that the sound velocity distribution of the extended part accords with the actual sound velocity distribution rule of the region.

Description

Sound velocity profile continuation method and system based on orthogonal empirical function decomposition
Technical Field
The invention belongs to the technical field of ocean acoustic application, and particularly relates to a sound velocity profile continuation method and system based on orthogonal empirical function decomposition.
Background
The statements in this section merely provide background information related to the present disclosure and may not necessarily constitute prior art that is already known to a person of ordinary skill in the art.
With the development of the underwater sound velocity field construction technology, sound velocity profile extension can be widely applied to application systems which take sound waves as signal carriers, such as underwater communication, positioning, navigation and the like. Under the condition that shallow sea and deep sea sound velocity profile samples coexist, deep sea partial continuation under the condition of high-precision matching of shallow sea actual measurement sound velocity values is carried out on the shallow sea sound velocity profile samples, the number of full-sea deep sound velocity profile reference samples can be increased, and the real-time estimation precision of the regional sound velocity field is improved.
The existing underwater sound velocity profile continuation method comprises the following steps: liu Fu Chen and the like propose a sound velocity profile continuation method based on polynomial fitting, fitting an actually measured shallow sea part sound velocity profile by using a polynomial, and extending in a deep sea area; the method comprises the steps of matching a full-sea deep sound velocity profile sample and a sound velocity profile sample to be extended at a common part of a deep-sea isothermal layer, calculating a structural coefficient of the sound velocity profile to be extended at the deep-sea isothermal layer by combining an empirical orthogonal function reconstruction process of the sound velocity profile, and constructing the distribution condition of the sound velocity profile in the deep-sea isothermal layer; the Drynaudian provides a sound velocity profile complementing method and device based on historical data and machine learning, the historical data is subjected to experience orthogonal function analysis to obtain characteristic vectors and characteristic vector coefficients, neurons representing different reference classification information are obtained through unsupervised learning method training, the association degree between an actually measured sound velocity profile and each neuron is calculated according to Euclidean distance, and the sound velocity profile is reconstructed by using the characteristic vector coefficients corresponding to the neurons with the highest association degree; a sound velocity profile continuation method based on low-rank matrix completion is provided by CaiKujg et al, a to-be-supplemented matrix is constructed by utilizing a to-be-extended sound velocity profile and a historical full-sea deep sound velocity profile, and the to-be-supplemented matrix is supplemented by applying a low-rank matrix completion algorithm, so that sound velocity profile continuation is completed.
Although there are various sound velocity profile continuation methods, the following problems still exist: firstly, the matching precision of the actually measured part of the sound velocity profile to be extended is not high enough; and secondly, the actually measured part of the sound velocity profile is excessively matched, so that the extended deep sea part does not accord with the real sound velocity distribution rule of the regional deep sea.
Disclosure of Invention
In order to solve the problems, the invention provides a sound velocity profile continuation method and a sound velocity profile continuation system based on orthogonal empirical function decomposition, which are used for matching the actually measured sound velocity value part of the sound velocity profile to be continued with high precision, ensuring that the sound velocity distribution of the continuation part accords with the actual sound velocity distribution rule of the region, and providing more and more reliable reference samples for the sound velocity profile inversion.
In order to achieve the above object, the present invention mainly includes the following aspects:
in a first aspect, an embodiment of the present invention provides a sound velocity profile continuation method based on orthogonal empirical function decomposition, including:
acquiring sample data of a sound velocity profile to be extended, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended and historical sound velocity profiles of the whole sea depth;
according to the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended, carrying out depth interception on the sample data of the full-sea-depth historical sound velocity profile to obtain the intercepted data of the historical sound velocity profile sample;
performing empirical orthogonal function decomposition on the sample truncation data of the historical sound velocity profile to obtain a first feature vector of a preset order of the sample truncation data of the historical sound velocity profile, and performing matching field processing on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient corresponding to the sound velocity profile to be extended in the first feature vector;
and constructing an extended full-sea-depth sound velocity profile according to the characteristic vector coefficient and the sample data of the full-sea-depth historical sound velocity profile.
In a possible implementation manner, the obtaining manner of the first feature vector includes:
determining an average sound velocity profile of the truncated data of the historical sound velocity profile sample according to the truncated data of the historical sound velocity profile sample, and constructing a first residual error matrix;
calculating an autocovariance matrix of the first residual error matrix, and solving an eigenvalue of the autocovariance matrix and a corresponding eigenvector;
and arranging the obtained eigenvalues from big to small, and selecting the eigenvector corresponding to the eigenvalue of the preset order arranged at the front as the first eigenvector.
In a possible implementation manner, the performing matching field processing on the sound velocity profile to be extended by using the first eigenvector to obtain an eigenvector coefficient of the sound velocity profile to be extended corresponding to the first eigenvector includes:
determining a residual vector between the sound velocity profile to be extended and an average sound velocity profile of sample truncation data of the historical sound velocity profile;
and determining a characteristic vector coefficient of the sound velocity profile to be extended corresponding to the first characteristic vector according to the residual vector and the first characteristic vector.
In one possible embodiment, the feature vector coefficients are the product of a transpose of the first feature vector and the residual vector.
In a possible implementation manner, the constructing an extended full-sea-depth acoustic velocity profile according to the eigenvector coefficients and sample data of the full-sea-depth historical acoustic velocity profile includes:
performing empirical orthogonal function decomposition on the sample data of the full-sea-depth historical sound velocity profile to obtain an average sound velocity profile of the full-sea-depth historical sound velocity profile and a second eigenvector of a preset order;
and constructing an extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile.
In a possible implementation manner, the constructing a extended full-sea-depth sound velocity profile according to an average sound velocity profile, a feature vector coefficient, and a second feature vector of the full-sea-depth historical sound velocity profile includes:
and calculating the product of the feature vector coefficient and the second feature vector, and determining the sum of the product and the average sound velocity profile of the whole-sea-depth historical sound velocity profile as the extended whole-sea-depth sound velocity profile.
In a possible implementation manner, the obtaining manner of the second feature vector includes:
determining an average sound velocity profile of the full-sea-depth historical sound velocity profile according to the sample data of the full-sea-depth historical sound velocity profile, and constructing a second residual matrix;
calculating an autocovariance matrix of the second residual error matrix, and solving an eigenvalue of the autocovariance matrix and a corresponding eigenvector;
and arranging the obtained eigenvalues from big to small, and selecting the eigenvector corresponding to the eigenvalue of the preset order arranged at the front as a second eigenvector.
In a possible implementation manner, the method for obtaining the full-sea-depth historical sound velocity profile sample data by preprocessing an acquired full-sea-depth historical sound velocity profile data set specifically includes: and performing depth interception on the full-sea-depth historical sound velocity profile data set according to the maximum depth of the actually measured sound velocity value of the full-sea-depth sound velocity profile to obtain full-sea-depth historical sound velocity profile sample data.
In a second aspect, an embodiment of the present invention provides a sound velocity profile continuation system based on orthogonal empirical function decomposition, including:
the data acquisition module is used for acquiring a sound velocity profile to be extended, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended and historical sound velocity profile sample data of the whole sea depth;
the depth interception module is used for carrying out depth interception on the sample data of the full-sea-depth historical sound velocity profile according to the maximum depth of the actually-measured sound velocity value of the sound velocity profile to be extended to obtain the intercepted data of the historical sound velocity profile sample;
the processing module is used for performing empirical orthogonal function decomposition on the truncated data of the historical sound velocity profile sample to obtain a first feature vector of a preset order of the truncated data of the historical sound velocity profile sample, and performing matching field processing on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector;
and the construction module is used for constructing the extended full-sea-depth sound velocity profile according to the characteristic vector coefficient and the sample data of the full-sea-depth historical sound velocity profile.
In a possible implementation, the building module is specifically configured to: performing empirical orthogonal function decomposition on the sample data of the full-sea-depth historical sound velocity profile to obtain an average sound velocity profile of the full-sea-depth historical sound velocity profile and a second eigenvector of a preset order;
and constructing the extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile.
The above one or more technical solutions have the following beneficial effects:
according to the method, empirical orthogonal function decomposition is carried out on the truncated data of a historical sound velocity profile sample to obtain a first feature vector of a preset order of the truncated data of the historical sound velocity profile sample, and matching field processing is carried out on the sound velocity profile to be extended by utilizing the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector; and constructing a prolonged full-sea deep sound velocity profile according to the characteristic vector coefficient and the sample data of the full-sea deep historical sound velocity profile. By the method, the main characteristics of the sound velocity profile sample to be extended in the cut-off depth of the area in which the sound velocity profile sample is located can be fully captured, the characteristic vector coefficient and the characteristic vector can be used for high-precision matching reconstruction of the sound velocity profile sample to be extended in the cut-off depth area (shallow sea) with obvious sound velocity change, meanwhile, the data of the depth part of the historical full-sea sound velocity profile sample exceeding the sound velocity profile sample to be extended is used as reference constraint, the sound velocity distribution of the extended part is guaranteed to accord with the actual sound velocity distribution rule of the area, and more reliable reference samples are provided for sound velocity profile inversion.
Drawings
The accompanying drawings, which are incorporated in and constitute a part of this specification, are included to provide a further understanding of the invention, and are incorporated in and constitute a part of this specification, illustrate exemplary embodiments of the invention and together with the description serve to explain the invention and not to limit the invention.
FIG. 1 is a flow chart of a method for extending a sound velocity profile based on orthogonal empirical function decomposition according to an embodiment of the present invention;
FIG. 2 is an overall framework diagram of a sound velocity profile continuation method based on orthogonal empirical function decomposition according to an embodiment of the present invention;
fig. 3 is a diagram illustrating a comparison between the sound velocity profile extension and the sound velocity profile extension according to an embodiment of the present invention.
Detailed Description
The invention is further described with reference to the following figures and examples.
It is to be understood that the following detailed description is exemplary and is intended to provide further explanation of the invention as claimed. Unless defined otherwise, all technical and scientific terms used herein have the same meaning as commonly understood by one of ordinary skill in the art to which this invention belongs.
It is noted that the terminology used herein is for the purpose of describing particular embodiments only and is not intended to be limiting of exemplary embodiments according to the invention. As used herein, the singular forms "a", "an", and "the" are intended to include the plural forms as well, and it should be understood that when the terms "comprises" and/or "comprising" are used in this specification, they specify the presence of stated features, steps, operations, devices, components, and/or combinations thereof, unless the context clearly indicates otherwise.
Example one
Referring to fig. 1, the present embodiment provides a sound velocity profile continuation method based on orthogonal empirical function decomposition, which specifically includes the following steps:
s101: and obtaining sample data of the sound velocity profile to be extended, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended and the historical sound velocity profile of the whole sea depth.
In the specific implementation, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended is shallow seawater sound velocity profile data, and the historical sound velocity profile sample data of the full-sea depth comprises complete seawater sound velocity profile data obtained through multiple measurementsOf 1 atiSample data S of sound velocity profile of whole sea i Is represented as follows:
Figure DEST_PATH_IMAGE001
wherein the content of the first and second substances,sin order to be the value of the speed of sound,dfor the purpose of the depth value,d D is the maximum depth of the measured sound velocity value of the full-sea-depth sound velocity profile,s D is the sound velocity value of the sound velocity profile at full depth of sea,Iis the number of samples.
S102: and performing depth interception on the full-sea-depth historical sound velocity profile sample data according to the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended to obtain historical sound velocity profile sample interception data.
In specific implementation, the sound velocity profile sample data S of the whole sea depth history i Performing partial depth 0-d truncation:d d the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended is reserved for the part, the 0-d depth interval part of each historical sound velocity profile sample is reserved, and the truncated data of the historical sound velocity profile sample
Figure 589788DEST_PATH_IMAGE002
Expressed as:
Figure DEST_PATH_IMAGE003
s103: and performing empirical orthogonal function decomposition on the truncated data of the historical sound velocity profile sample to obtain a first feature vector of a preset order of the truncated data of the historical sound velocity profile sample, and performing matching field processing on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector.
In specific implementation, the empirical orthogonal function analysis method is utilized to cut off data of historical sound velocity profile samples
Figure 919750DEST_PATH_IMAGE004
Performing empirical orthogonal function decomposition to obtain historical sound velocity profileThe method comprises the steps of truncating a first feature vector of a preset order of data by a surface sample, and then carrying out matching field processing on a sound velocity profile to be extended by utilizing the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector.
The obtaining mode of the first feature vector comprises the following steps: determining an average sound velocity profile of the sample truncation data of the historical sound velocity profile according to the sample truncation data of the historical sound velocity profile, and constructing a first residual matrix; calculating an autocovariance matrix of the first residual error matrix, and solving an eigenvalue of the autocovariance matrix and a corresponding eigenvector; and arranging the obtained eigenvalues from big to small, and selecting the eigenvector corresponding to the eigenvalue of the preset order arranged at the front as the first eigenvector.
Specifically, the average sound velocity profile of the truncated data of the historical sound velocity profile sample is as follows:
Figure DEST_PATH_IMAGE005
constructing a first residual matrix:
Figure 671806DEST_PATH_IMAGE006
the autocovariance matrix of the first residual matrix is:
Figure 494268DEST_PATH_IMAGE007
wherein, the first and the second end of the pipe are connected with each other,C S,d for a matrix of (d + 1) × (d + 1) order, calculateC S,d Eigenvalue matrix of
Figure DEST_PATH_IMAGE008
And eigenvector matrix V d And satisfies the following conditions:
Figure 698985DEST_PATH_IMAGE009
wherein the content of the first and second substances,
Figure 897885DEST_PATH_IMAGE008
for the diagonal matrix of order N:
Figure DEST_PATH_IMAGE010
n is the order of the characteristic value, V d Is a (d + 1) x N order matrix, each column of which is a feature vector, V d Can be expressed as
Figure 504447DEST_PATH_IMAGE011
Characteristic value
Figure DEST_PATH_IMAGE012
And feature vector
Figure 435494DEST_PATH_IMAGE013
And (7) corresponding.
Arranging the obtained eigenvalues from big to small, and selecting eigenvectors corresponding to the top n eigenvalues
Figure DEST_PATH_IMAGE014
The first eigenvector of a preset order of the data is truncated for the historical sound velocity profile samples, where the order value is typically an integer between 3-5.
The matching field processing is performed on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector, and the method comprises the following steps: determining a residual vector between the sound velocity profile to be extended and an average sound velocity profile of sample truncation data of the historical sound velocity profile; and determining a characteristic vector coefficient of the sound velocity profile to be extended corresponding to the first characteristic vector according to the residual vector and the first characteristic vector. Optionally, the feature vector coefficient is a product of a transpose of the first feature vector and the residual vector.
In particular, the acoustic velocity profile to be extended may be expressed as
Figure 127506DEST_PATH_IMAGE015
The sound velocity value vector of the sound velocity profile to be extended is expressed as
Figure DEST_PATH_IMAGE016
Wherein, in the step (A),trepresenting the sound velocity profile to be extended as test data, and the residual vector between the test data and the average sound velocity profile of the truncation data of the 0-d depth historical sound velocity profile sampleS X,t Comprises the following steps:
Figure 802201DEST_PATH_IMAGE017
performing a matching field processing process on the sound velocity profile to be extended by utilizing the first n-order eigenvector of the depth from 0 to d, calculating the projection of the sound velocity profile to be extended on the first n-order eigenvector, and acquiring the eigenvector coefficient of the projection of the first n-order eigenvector of the sound velocity profile to be extended on the depth from 0 to dCf d
Figure DEST_PATH_IMAGE018
Here, the number of the first and second electrodes,
Figure 263269DEST_PATH_IMAGE019
is the first feature vector
Figure DEST_PATH_IMAGE020
The transposing of (1).
S104: and constructing a prolonged full-sea deep sound velocity profile according to the characteristic vector coefficient and the sample data of the full-sea deep historical sound velocity profile.
Specifically, in S104, the constructing an extended full-sea-depth sound velocity profile according to the eigenvector coefficients and the sample data of the full-sea-depth historical sound velocity profile includes: performing empirical orthogonal function decomposition on the sample data of the full-sea-depth historical sound velocity profile to obtain an average sound velocity profile of the full-sea-depth historical sound velocity profile and a second feature vector of a preset order; and constructing the extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile.
As shown in fig. 2, preprocessing the acquired full-sea-depth historical sound velocity profile data set to obtain full-sea-depth historical sound velocity profile sample data, specifically including: according to the measured maximum depth of the sound velocity value of the full-sea-depth sound velocity profiled D And carrying out depth interception on the full-sea-depth historical sound velocity profile data set to obtain full-sea-depth historical sound velocity profile sample data, namely reserving 0-D full-sea-depth sound velocity profile sample S in the part i
The second feature vector is obtained in a manner that: determining an average sound velocity profile of the full-sea-depth historical sound velocity profile according to the sample data of the full-sea-depth historical sound velocity profile, and constructing a second residual matrix; calculating an autocovariance matrix of the second residual error matrix, and solving an eigenvalue of the autocovariance matrix and a corresponding eigenvector; and arranging the obtained eigenvalues from large to small, and selecting the eigenvector corresponding to the eigenvalue of the preset order arranged at the front as a second eigenvector.
In specific implementation, the average acoustic velocity profile of the 0-D full-sea deep acoustic velocity profile sample is:
Figure 693114DEST_PATH_IMAGE021
constructing a second residual matrix of the 0-D full-sea sound velocity profile sample:
Figure DEST_PATH_IMAGE022
the autocovariance matrix of the second residual matrix is:
Figure 863633DEST_PATH_IMAGE023
wherein, C S,D For a matrix of order (D + 1) × (D + 1), C is calculated S,D Characteristic value of (2)
Figure DEST_PATH_IMAGE024
And a feature vector V D And satisfies the following conditions:
Figure 76440DEST_PATH_IMAGE025
wherein the characteristic value
Figure 719911DEST_PATH_IMAGE024
For diagonal matrices:
Figure DEST_PATH_IMAGE026
where M is the order of the eigenvalues, V D Is a matrix of order (D + 1) xM, each column of which is a feature vector, V D Can be expressed as
Figure 992760DEST_PATH_IMAGE027
Characteristic value of
Figure DEST_PATH_IMAGE028
And feature vector
Figure 659365DEST_PATH_IMAGE029
And (7) correspondingly.
Arranging the diagonal elements of the eigenvalue matrix of the auto-covariance matrix corresponding to the second residual matrix in the 0-D full sea depth through empirical orthogonal function decomposition from large to small, and selecting the first m-order eigenvector
Figure DEST_PATH_IMAGE030
Here, the preset order m = n takes an integer of 3-5, and in the present embodiment, m = n =3 may be taken.
The method for constructing the extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile comprises the following steps: and calculating the product of the characteristic vector coefficient and the second characteristic vector, and determining the sum of the product and the average sound velocity profile of the whole-sea-depth historical sound velocity profile as the extended whole-sea-depth sound velocity profile.
In the practice, the method utilizesCharacteristic vector coefficient of 0-d depth front n-order characteristic vector during continuation sound velocity profile matchingCf d 0-D average sound velocity profile at full depth
Figure 675863DEST_PATH_IMAGE031
And first m order eigenvectors
Figure DEST_PATH_IMAGE032
Combined construction of extended full-sea deep acoustic velocity profile
Figure 111523DEST_PATH_IMAGE033
The method specifically comprises the following steps:
Figure DEST_PATH_IMAGE034
extended acoustic velocity profile
Figure 820853DEST_PATH_IMAGE035
Expressed as:
Figure DEST_PATH_IMAGE036
the sample before and after the continuation is shown in fig. 3, and by the method, the actually measured sound velocity value part of the sound velocity profile to be continued can be matched with high precision, and meanwhile, the sound velocity distribution of the continuation part is ensured to accord with the actual sound velocity distribution rule of the region.
Example two
The embodiment of the invention also provides a sound velocity profile continuation system based on orthogonal empirical function decomposition, which comprises:
the data acquisition module is used for acquiring a sound velocity profile to be extended, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended and historical sound velocity profile sample data of the whole sea depth;
the depth interception module is used for carrying out depth interception on the sample data of the full-sea-depth historical sound velocity profile according to the maximum depth of the actually-measured sound velocity value of the sound velocity profile to be extended to obtain the intercepted data of the historical sound velocity profile sample;
the processing module is used for performing empirical orthogonal function decomposition on the truncated data of the historical sound velocity profile sample to obtain a first feature vector of a preset order of the truncated data of the historical sound velocity profile sample, and performing matching field processing on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector;
and the construction module is used for constructing the extended full-sea-depth sound velocity profile according to the characteristic vector coefficients and the sample data of the full-sea-depth historical sound velocity profile.
As an optional implementation manner, the building module is specifically configured to: performing empirical orthogonal function decomposition on the sample data of the full-sea-depth historical sound velocity profile to obtain an average sound velocity profile of the full-sea-depth historical sound velocity profile and a second eigenvector of a preset truncation order;
and constructing the extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile.
The sound velocity profile continuation system based on orthogonal empirical function decomposition provided in this embodiment is used to implement the sound velocity profile continuation method based on orthogonal empirical function decomposition, so that a specific implementation manner in the sound velocity profile continuation system based on orthogonal empirical function decomposition may be found in the foregoing example part of the sound velocity profile continuation method based on orthogonal empirical function decomposition, and details are not described here.
The above description is only a preferred embodiment of the present invention and is not intended to limit the present invention, and various modifications and changes may be made by those skilled in the art. Any modification, equivalent replacement, or improvement made within the spirit and principle of the present invention should be included in the protection scope of the present invention.

Claims (10)

1. A sound velocity profile continuation method based on orthogonal empirical function decomposition is characterized by comprising the following steps:
acquiring sample data of a sound velocity profile to be extended, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended and historical sound velocity profiles of the whole sea depth;
according to the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended, carrying out depth interception on the sample data of the full-sea-depth historical sound velocity profile to obtain the intercepted data of the historical sound velocity profile sample;
performing empirical orthogonal function decomposition on the sample truncation data of the historical sound velocity profile to obtain a first feature vector of a preset order of the sample truncation data of the historical sound velocity profile, and performing matching field processing on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient corresponding to the sound velocity profile to be extended in the first feature vector;
and constructing a prolonged full-sea deep sound velocity profile according to the characteristic vector coefficient and the sample data of the full-sea deep historical sound velocity profile.
2. The method according to claim 1, wherein the obtaining of the first eigenvector comprises:
determining an average sound velocity profile of the truncated data of the historical sound velocity profile sample according to the truncated data of the historical sound velocity profile sample, and constructing a first residual error matrix;
calculating an autocovariance matrix of the first residual error matrix, and solving an eigenvalue of the autocovariance matrix and a corresponding eigenvector;
and arranging the obtained eigenvalues from big to small, and selecting the eigenvector corresponding to the eigenvalue of the preset order arranged at the front as the first eigenvector.
3. The sound velocity profile continuation method based on orthogonal empirical function decomposition according to claim 1, wherein the obtaining a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector by performing matching field processing on the sound velocity profile to be extended by using the first feature vector includes:
determining a residual vector between the sound velocity profile to be extended and an average sound velocity profile of sample truncation data of the historical sound velocity profile;
and determining a characteristic vector coefficient of the sound velocity profile to be extended corresponding to the first characteristic vector according to the residual error vector and the first characteristic vector.
4. The method of claim 3, wherein the eigenvector coefficients are products of transposes of the first eigenvector and residual vectors.
5. The method for extending the sound velocity profile based on the orthogonal empirical function decomposition of claim 1, wherein the constructing an extended full-sea-depth sound velocity profile according to the eigenvector coefficients and the sample data of the full-sea-depth historical sound velocity profile comprises:
performing empirical orthogonal function decomposition on the sample data of the full-sea-depth historical sound velocity profile to obtain an average sound velocity profile of the full-sea-depth historical sound velocity profile and a second feature vector of a preset order;
and constructing the extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile.
6. The method for extending the sound velocity profile based on the orthogonal empirical function decomposition of claim 5, wherein the constructing the extended whole-sea-depth sound velocity profile according to the average sound velocity profile, the eigenvector coefficients and the second eigenvector of the whole-sea-depth historical sound velocity profile comprises:
and calculating the product of the characteristic vector coefficient and the second characteristic vector, and determining the sum of the product and the average sound velocity profile of the whole-sea-depth historical sound velocity profile as the extended whole-sea-depth sound velocity profile.
7. The method according to claim 5, wherein the second eigenvector is obtained by:
determining an average sound velocity profile of the full-sea-depth historical sound velocity profile according to the sample data of the full-sea-depth historical sound velocity profile, and constructing a second residual matrix;
calculating an autocovariance matrix of the second residual error matrix, and solving an eigenvalue of the autocovariance matrix and a corresponding eigenvector;
and arranging the obtained eigenvalues from large to small, and selecting the eigenvector corresponding to the eigenvalue of the preset order arranged at the front as a second eigenvector.
8. The method for extending a sound velocity profile based on orthogonal empirical function decomposition of claim 1, wherein the step of preprocessing the acquired full-sea-depth historical sound velocity profile data set to obtain sample data of the full-sea-depth historical sound velocity profile specifically comprises the steps of: and performing depth interception on the full-sea-depth historical sound velocity profile data set according to the maximum depth of the actually measured sound velocity value of the full-sea-depth sound velocity profile to obtain full-sea-depth historical sound velocity profile sample data.
9. An acoustic velocity profile continuation system based on orthogonal empirical function decomposition, comprising:
the data acquisition module is used for acquiring a sound velocity profile to be extended, the maximum depth of the actually measured sound velocity value of the sound velocity profile to be extended and historical sound velocity profile sample data of the whole sea depth;
the depth interception module is used for carrying out depth interception on the sample data of the full-sea-depth historical sound velocity profile according to the maximum depth of the actually-measured sound velocity value of the sound velocity profile to be extended to obtain the intercepted data of the historical sound velocity profile sample;
the processing module is used for performing empirical orthogonal function decomposition on the sample truncation data of the historical sound velocity profile to obtain a first feature vector of a preset order of the sample truncation data of the historical sound velocity profile, and performing matching field processing on the sound velocity profile to be extended by using the first feature vector to obtain a feature vector coefficient of the sound velocity profile to be extended corresponding to the first feature vector;
and the construction module is used for constructing the extended full-sea-depth sound velocity profile according to the characteristic vector coefficients and the sample data of the full-sea-depth historical sound velocity profile.
10. The orthogonal empirical function decomposition-based sound velocity profile continuation system of claim 9, wherein the construction module is specifically configured to: performing empirical orthogonal function decomposition on the sample data of the full-sea-depth historical sound velocity profile to obtain an average sound velocity profile of the full-sea-depth historical sound velocity profile and a second feature vector of a preset order;
and constructing an extended full-sea-depth sound velocity profile according to the average sound velocity profile, the characteristic vector coefficient and the second characteristic vector of the full-sea-depth historical sound velocity profile.
CN202211118337.3A 2022-09-15 2022-09-15 Sound velocity profile continuation method and system based on orthogonal empirical function decomposition Active CN115204317B (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN202211118337.3A CN115204317B (en) 2022-09-15 2022-09-15 Sound velocity profile continuation method and system based on orthogonal empirical function decomposition

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN202211118337.3A CN115204317B (en) 2022-09-15 2022-09-15 Sound velocity profile continuation method and system based on orthogonal empirical function decomposition

Publications (2)

Publication Number Publication Date
CN115204317A true CN115204317A (en) 2022-10-18
CN115204317B CN115204317B (en) 2022-11-25

Family

ID=83573525

Family Applications (1)

Application Number Title Priority Date Filing Date
CN202211118337.3A Active CN115204317B (en) 2022-09-15 2022-09-15 Sound velocity profile continuation method and system based on orthogonal empirical function decomposition

Country Status (1)

Country Link
CN (1) CN115204317B (en)

Citations (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH1062543A (en) * 1996-08-26 1998-03-06 Oki Electric Ind Co Ltd Development function generation method and apparatus for ocean acoustic tomography
CN111307266A (en) * 2020-02-21 2020-06-19 山东大学 Sound velocity obtaining method and global ocean sound velocity field construction method based on same
CN112964231A (en) * 2021-02-03 2021-06-15 广东海洋大学 Method for obtaining depth of ocean mixing layer based on sound velocity disturbance modal matching
CN113051260A (en) * 2021-04-27 2021-06-29 中国人民解放军国防科技大学 High-resolution sound velocity profile data compression method based on empirical orthogonal function decomposition
CN113218493A (en) * 2021-04-08 2021-08-06 中国人民解放军国防科技大学 Sound velocity profile inversion method based on empirical orthogonal function method

Patent Citations (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
JPH1062543A (en) * 1996-08-26 1998-03-06 Oki Electric Ind Co Ltd Development function generation method and apparatus for ocean acoustic tomography
CN111307266A (en) * 2020-02-21 2020-06-19 山东大学 Sound velocity obtaining method and global ocean sound velocity field construction method based on same
CN112964231A (en) * 2021-02-03 2021-06-15 广东海洋大学 Method for obtaining depth of ocean mixing layer based on sound velocity disturbance modal matching
CN113218493A (en) * 2021-04-08 2021-08-06 中国人民解放军国防科技大学 Sound velocity profile inversion method based on empirical orthogonal function method
CN113051260A (en) * 2021-04-27 2021-06-29 中国人民解放军国防科技大学 High-resolution sound velocity profile data compression method based on empirical orthogonal function decomposition

Non-Patent Citations (2)

* Cited by examiner, † Cited by third party
Title
FANLIN YANG等: "Precise Positioning of Underwater Static Objects without Sound Speed Profile", 《MARINE GEODESY》 *
高茹茹: "水下声学定位关键技术问题研究", 《万方数据》 *

Also Published As

Publication number Publication date
CN115204317B (en) 2022-11-25

Similar Documents

Publication Publication Date Title
CN109410917B (en) Voice data classification method based on improved capsule network
CN101272168B (en) Signal sources estimation method and its DOA estimation method
CN108364659B (en) Frequency domain convolution blind signal separation method based on multi-objective optimization
Ma et al. Efficient method to determine diagonal loading value
CN106093921B (en) Acoustic vector sensor array broadband direction-finding method based on sparse resolution theory
CN107221336A (en) It is a kind of to strengthen the devices and methods therefor of target voice
US8270632B2 (en) Sound source localization system and method
CN109884591B (en) Microphone array-based multi-rotor unmanned aerial vehicle acoustic signal enhancement method
WO2018133056A1 (en) Method and apparatus for locating sound source
CN112526451A (en) Compressed beam forming and system based on microphone array imaging
JP7027365B2 (en) Signal processing equipment, signal processing methods and programs
CN114972339B (en) Data enhancement system for bulldozer structural member production abnormity detection
CN113822284A (en) RGBD image semantic segmentation method based on boundary attention
WO2021013345A1 (en) Audio processing apparatus and method for denoising a multi-channel audio signal
CN110709929A (en) Processing sound data to separate sound sources in a multi-channel signal
CN113109759A (en) Underwater sound array signal direction-of-arrival estimation method based on wavelet transformation and convolutional neural network
CN110716203A (en) Time-frequency analysis and tracking method of passive sonar target
CN103837858A (en) Far field direction of arrival estimation method applied to plane array and system thereof
CN115278496A (en) Sparse sound source identification method and system for microphone array measurement
CN115204317B (en) Sound velocity profile continuation method and system based on orthogonal empirical function decomposition
CN111929641B (en) Rapid indoor fingerprint positioning method based on width learning
CN115014313B (en) Polarized light compass heading error processing method based on parallel multi-scale
Goto et al. Quasi-newton adversarial attacks on speaker verification systems
CN114283082A (en) Infrared small target detection method based on attention mechanism
CN107085832A (en) A kind of Fast implementation of the non local average denoising of digital picture

Legal Events

Date Code Title Description
PB01 Publication
PB01 Publication
SE01 Entry into force of request for substantive examination
SE01 Entry into force of request for substantive examination
GR01 Patent grant
GR01 Patent grant