CN109975755B - Short-wave multi-station direct positioning method under condition of existence of correction source - Google Patents
Short-wave multi-station direct positioning method under condition of existence of correction source Download PDFInfo
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Abstract
The invention relates to the technical field of short-wave multi-station positioning, and discloses a short-wave multi-station direct positioning method under the condition of a correction source. Due to the existence of the correction source, the method provided by the invention can effectively inhibit the influence of array amplitude-phase errors on the shortwave multi-station positioning accuracy.
Description
Technical Field
The invention relates to the technical field of short-wave multi-station positioning, in particular to a short-wave multi-station direct positioning method under the condition of a correction source.
Background
As is well known, the wireless signal positioning technology is widely applied to the fields of communication, radar, target monitoring, navigation and telemetry, seismic surveying, radio astronomy, emergency rescue, safety management and the like, and plays an important role in industrial production and military application. The positioning (i.e. position parameter estimation) of the target can be accomplished by using active devices such as radar, laser, sonar and the like, which are called as active positioning technologies and have the advantages of all weather, high precision and the like. However, the active positioning system usually needs to transmit a high-power electromagnetic signal to implement, so that the position of the active positioning system is very easy to expose, and the active positioning system is easy to be found by the other party, and is affected by the electronic interference of the other party, so that the positioning performance is greatly deteriorated, and even the safety and reliability of the system are compromised.
Target location may also be achieved using radio signals radiated or scattered by the target (actively), a technique referred to as passive location, which refers to estimating target location parameters by receiving radio signals radiated or scattered by the target without the observation station actively transmitting electromagnetic signals. Compared with an active positioning system, the passive positioning system has the advantages of no active transmission of electromagnetic signals, strong viability, long reconnaissance action distance and the like, thereby obtaining wide attention and deep research of domestic and foreign scholars. The passive positioning system can be divided into a single-station passive positioning system and a multi-station passive positioning system according to the number of observation stations, wherein the multi-station positioning system can provide more observed quantities, so that the target positioning precision is improved.
As is known, short-wave multi-station positioning is an important multi-station passive positioning system which is mainly applied to positioning over-the-horizon long-distance targets. Array amplitude and phase errors are an important factor influencing positioning accuracy, and occur when the array antenna of each observation station is not subjected to channel correction.
On the other hand, most of the existing passive positioning processes can be generalized to a two-step estimation positioning mode, that is, first, positioning parameters (such as azimuth, delay difference, doppler, etc.) are extracted from signal data, and then, based on the parameters, position information of a target is calculated. Although this two-step positioning mode has been widely used in modern positioning systems, israeli a.j.weiss and a.amar have pointed out several drawbacks that exist therein and have proposed the idea of a single-step direct positioning, the basic idea of which is to determine the position parameters of an object directly from acquired signal data without estimating other intermediate positioning parameters. Obviously, the single-step direct positioning mode is also suitable for short-wave multi-station positioning scenes under the condition that array amplitude and phase errors exist, and only the direct positioning method is also influenced by the array amplitude and phase errors, so that larger positioning deviation is generated.
Disclosure of Invention
Aiming at the problem of influence of array amplitude-phase errors, the invention provides a short-wave multi-station direct positioning method under the condition of a correction source, so as to improve the multi-station positioning precision of a short-wave radiation source.
In order to achieve the purpose, the invention adopts the following technical scheme:
a short-wave multi-station direct positioning method under the condition of existence of a correction source comprises the following steps:
step 1: d short wave correction sources with known longitude and latitude are simultaneously placed on the periphery of the area where the short wave target source is located;
step 2: receiving a target source signal and D correction source signals by using N observation stations, wherein each observation station acquires K signal samples by using a uniform circular array which is not corrected by a channel, and establishes an array signal model corresponding to the K signal samples;
and step 3: determining the relationship between the azimuth angle and the elevation angle of a target source signal reaching N observation stations and the longitude and latitude and the virtual height of an ionosphere of the target source respectively;
and 4, step 4: determining the relation between the azimuth angle and the elevation angle of the D correction source signals reaching the N observation stations and the longitude and latitude and the ionospheric virtual height of the D correction source signals;
and 5: each observation station utilizes an array signal model corresponding to the collected K signal samples to construct a covariance matrix, and transmits the covariance matrix to a central station in the N observation stations;
step 6: the central station constructs a cost function for jointly estimating the latitude and longitude of a target source, the ionosphere virtual height and the multi-array amplitude-phase error based on the maximum likelihood criterion by using the covariance matrixes of the N observation stations;
and 7: and performing joint estimation on the longitude and latitude of the target source, the virtual height of the ionized layer and the multi-array amplitude-phase error by using an alternative iterative algorithm according to the relation between the azimuth angle and the elevation angle of the target source signal reaching the N observation stations and the longitude and latitude and the virtual height of the ionized layer of the target source, the relation between the azimuth angle and the elevation angle of the D correction source signal reaching the N observation stations and the longitude and latitude and the virtual height of the D correction source and the virtual height of the ionized layer and the cost function, thereby determining the position information of the target.
Further, the array signal model in step 2 is:
in the formula, xn(tk) Receiving signals for a kth array of an nth observation station; sc,n,d(tk) A complex envelope for the d-th corrected source signal to reach the nth observation station; st,n(tk) A complex envelope for the target source signal to reach the nth observation station; epsilonn(tk) Uniform circular array additive noise of the nth observation station;a complex envelope vector for the signal arriving at the nth observation station; h isnIonospheric pseudo-heights experienced by signals arriving at the nth observation station; a isn(ωc,d,ρc,d,hn) For the array manifold vector, ω, of the d-th corrected source signal arriving at the nth observation stationc,dTo correct for source longitude, pc,dTo correct for source latitude, hnIs ionospheric pseudo-height; a isn(ωt,ρt,hn) Array manifold vector, omega, for the arrival of target source signals at the nth observation stationtAs the target source longitude, ρtIs the target source latitude;for the nth observationAn array manifold matrix of stations; gamma-shapednIs the amplitude-phase error matrix of the nth observation station.
Further, the step 3 comprises:
step 3.1: converting the longitude and latitude coordinates of the target source into a horizon coordinate with the observation station as the center according to the formula (2):
in the formula (x)t,n,g,yt,n,g,zt,n,g) Coordinates of the target source under the horizontal coordinate system of the nth observation station are obtained; omegao,nAnd ρo,nLongitude and latitude of the nth observation station respectively; r is the radius of the earth;
step 3.2: obtaining the azimuth angle theta according to the formula (2)t,nAnd longitude ωtLatitude rhotAnd ionospheric pseudo-height hnThe relationship of (1):
step 3.3: a triangle is constructed through the observation station, the sphere center point and the ionized layer, and the elevation angle beta is obtained by utilizing the sine theorem of the triangletAnd longitude ωtLatitude rhotAnd ionospheric pseudo-height h relation:
in the formula (I), the compound is shown in the specification,the internal angle of the triangle with the center point as the vertex is shown.
Further, the step 4 comprises:
step 4.1: converting the longitude and latitude coordinates of the d correction source into a horizon coordinate with the observation station as the center according to the formula (5):
in the formula (x)d,n,g,yd,n,g,zd,n,g) Coordinates of a d correction source target source in a horizontal coordinate system of an nth observation station;
step 4.2: obtaining the azimuth angle theta according to the formula (5)c,d,nAnd longitude ωc,dAnd latitude rhoc,dThe relationship of (1):
step 4.3: using the sine theorem of triangle to obtain the elevation angle betac,d,nAnd longitude ωc,dLatitude rhoc,dAnd ionospheric pseudo-height hnThe relationship of (1):
in the formula (I), the compound is shown in the specification,
further, the step 5 comprises:
step 5.1: the nth observation station utilizes an array signal model { x ] corresponding to the collected K signal samplesn(tk)}1≤k≤KConstructing an array output covariance matrix
Step 5.2: each of the observatory stations communicates the constructed covariance matrix to a central station of the N observatory stations.
Further, the step 6 comprises:
the central station utilizes the covariance matrix of the N observersJoint estimation target source longitude omega based on maximum likelihood criterion constructiontLatitude rhotAnd the ionized layer virtual height { hn}1≤n≤NAnd a multi-array amplitude-phase error matrix { gamman}1≤n≤NThe cost function of (2); the cost function is:
wherein h ═ h1h2…hN]TIndicating ionospheric pseudo-height parameters;representing an array amplitude and phase error parameter; II type⊥[ΓnAn(ωt,ρt,hn)]Representing orthogonal projection matrices, Π⊥[ΓnAn(ωt,ρt,hn)]=I-ΓnAn(ωt,ρt,hn)((ΓnAn(ωt,ρt,hn))HΓnAn(ωt,ρt,hn))-1(ΓnAn(ωt,ρt,hn))H, (1≤n≤N)
Wherein I is an identity matrix.
Further, the step 7 includes:
step 7.1: will omegat、ρtAnd { hn}1≤n≤NAs a first set of parameters, { Γn}1≤n≤NAs a second set of parameters, the second set of parameters is fixed to the current update value, i.e. { Γ }n}1≤n≤NIs fixed toFix g asEstimating a first group of parameters according to a relation between an azimuth angle and an elevation angle of a target source signal reaching N observation stations and a longitude and latitude and an ionospheric virtual height of the target source respectively, a relation between an azimuth angle and an elevation angle of D correction source signals reaching N observation stations and a longitude and latitude and a virtual height of the ionospheric layer respectively, and the cost function according to an equation (10):
wherein mu is a step factor, mu is more than 0 and less than 1, muiIs the ith iteration step size factor;and h(i)Are all the ith iteration result;and h(i+1)All are the (i +1) th iteration results;is a gradient vector;is a Hessian matrix;
wherein the expressions of the elements are respectively
In the formula (I), the compound is shown in the specification,
in the formula InIs the radius of the uniform circular array of the nth observation station, lambda is the signal wavelength,is the last column vector in the (D +1) × (D +1) order identity matrix;
step 7.2: fixing the first set of parameters to the current update value, i.e. ωt、ρtAnd h are eachIs fixed toAndaccording to the relation between the azimuth angle and the elevation angle of the target source signal reaching the N observation stations and the longitude and latitude and the virtual height of the ionized layer, the relation between the azimuth angle and the elevation angle of the D correction source signal reaching the N observation stations and the longitude and latitude and the virtual height of the ionized layer and the cost function, the second group of parameters are optimized and solved according to the formula (11):
in the formula, g(i)Is the result of the ith iteration; g(i+1)Is the (i +1) th iteration result;is a gradient vector;is a Hessian matrix;
wherein the expressions of the elements are respectively
Step 7.3: and (3) alternately carrying out optimization solution on the first set of parameters and the second set of parameters according to the formula (10) and the formula (11) until iteration converges.
Compared with the prior art, the invention has the following beneficial effects:
the method comprises the steps of firstly, simultaneously placing a plurality of short wave correction sources with known positions near a short wave target source, receiving short wave signal data (simultaneously containing a target source signal and a correction source signal) by utilizing uniform circular arrays in a plurality of observation stations, then determining the relation between azimuth angles and elevation angles of signals reaching different observation stations, longitude and latitude degrees and ionospheric virtual height parameters of the signals, then constructing a cost function for jointly estimating the longitude and latitude degrees, ionospheric virtual height parameters and multi-array amplitude-phase errors of the target source by utilizing a maximum likelihood criterion, and finally, jointly estimating the longitude and latitude degrees, ionospheric virtual height and multi-array amplitude-phase errors of the target source by utilizing an alternating iterative algorithm, thereby determining the position information of the target. Based on the basic idea of direct positioning, the short-wave signal source is positioned by utilizing a correction source with accurately known position, and the positioning deviation caused by the amplitude-phase error of multiple arrays can be effectively eliminated, so that the short-wave multi-station positioning accuracy is improved.
Drawings
Fig. 1 is a flowchart of a shortwave multi-station direct positioning method in the presence of a calibration source according to an embodiment of the present invention.
FIG. 2 is a schematic diagram of coordinate system transformation according to an embodiment of the present invention.
Fig. 3 is a schematic diagram of a triangle for determining an elevation expression according to an embodiment of the present invention.
Fig. 4 is a diagram illustrating multi-station data transmission according to an embodiment of the present invention.
FIG. 5 is a graph of RMS error versus SNR for a target source in accordance with an embodiment of the present invention.
Fig. 6 is a graph of variation of the ionospheric pseudo-high estimated root mean square error with the target source signal-to-noise ratio according to an embodiment of the present invention.
FIG. 7 is a graph showing the variation of the RMS error of the array amplitude-phase error estimate with the SNR of the target source according to an embodiment of the present invention.
FIG. 8 is a graph of root mean square error versus radius of a circular array for target source positioning according to an embodiment of the present invention.
Fig. 9 is a graph of variation of the ionospheric pseudo-height estimated root mean square error with the ratio of the radius of the circular array to the wavelength, in accordance with an embodiment of the present invention.
FIG. 10 is a graph showing the variation of the estimated root mean square error of the array amplitude-phase error with the ratio of the radius of the circular array to the wavelength according to the embodiment of the present invention.
Detailed Description
The invention is further illustrated by the following examples in conjunction with the accompanying drawings:
the first embodiment is as follows:
as shown in fig. 1, a short-wave multi-station direct positioning method in the presence of a calibration source includes the following steps:
step S101: d short wave correction sources with known longitude and latitude are simultaneously placed on the periphery of the area where the short wave target source is located;
step S102: receiving a target source signal and D correction source signals by using N observation stations, wherein each observation station acquires K signal samples by using a uniform circular array which is not corrected by a channel, and establishes an array signal model corresponding to the K signal samples;
step S103: determining the relationship between the azimuth angle and the elevation angle of a target source signal reaching N observation stations and the longitude and latitude and the virtual height of an ionosphere of the target source respectively;
step S104: determining the relation between the azimuth angle and the elevation angle of the D correction source signals reaching the N observation stations and the longitude and latitude and the ionospheric virtual height of the D correction source signals;
step S105: each observation station utilizes an array signal model corresponding to the collected K signal samples to construct a covariance matrix, and transmits the covariance matrix to a central station in the N observation stations;
step S106: the central station constructs a cost function for jointly estimating the latitude and longitude of a target source, the ionosphere virtual height and the multi-array amplitude-phase error based on the maximum likelihood criterion by using the covariance matrixes of the N observation stations;
step S107: and performing joint estimation on the longitude and latitude of the target source, the virtual height of the ionized layer and the multi-array amplitude-phase error by using an alternative iterative algorithm according to the relation between the azimuth angle and the elevation angle of the target source signal reaching the N observation stations and the longitude and latitude and the virtual height of the ionized layer of the target source, the relation between the azimuth angle and the elevation angle of the D correction source signal reaching the N observation stations and the longitude and latitude and the virtual height of the D correction source and the virtual height of the ionized layer and the cost function, thereby determining the position information of the target.
Specifically, in step S101, D short-wave calibration sources with accurately known longitude and latitude are simultaneously placed around the area where the short-wave target source is located, where the longitude of the target source is ωtLatitude is rhotThe longitude of the D (1 ≦ D ≦ D) th correction source is ωc,dLatitude is rhoc,d。
Specifically, in step S102, D +1 short-wave signals (including D correction source signals and 1 target source signal) reach N observation stations after being subjected to ionospheric scattering, each observation station receives the short-wave signals by using a uniform circular array that is not subjected to channel correction, and acquires K signal samples in total, so that an array signal model of the nth observation station in the presence of an array amplitude-phase error is:
in the formula, xn(tk) Receiving signals for a kth array of an nth observation station; sc,n,d(tk) A complex envelope for the d-th corrected source signal to reach the nth observation station; st,n(tk) A complex envelope for the target source signal to reach the nth observation station; epsilonn(tk) Uniform circular array additive noise of the nth observation station;a complex envelope vector for the signal arriving at the nth observation station; h isnIonospheric pseudo-heights experienced by signals arriving at the nth observation station; a isn(ωc,d,ρc,d,hn) For the array manifold vector of the d-th corrected source signal arriving at the nth observation stationSimultaneously with the correction of the source longitude omegac,dLatitude rhoc,dAnd ionospheric pseudo-height hnA total of 3 parameters are related; a isn(ωt,ρt,hn) Array manifold vector for target source signal to reach nth observation station, which is simultaneously with target source longitude omegatLatitude rhotAnd ionospheric pseudo-height hnA total of 3 parameters are related;for the array manifold matrix of the nth observation station, since the correction source longitude and latitude are precisely known, it is only considered as being with respect to the target source longitude ωtLatitude rhotAnd ionospheric pseudo-height hnA function of (a); gamma-shapednThe amplitude-phase error matrix for the nth observation station is a diagonal matrix, and the first diagonal element can be set to 1.
Specifically, the step S103 includes:
step S103.1: converting the longitude and latitude coordinates of the target source into a horizon coordinate with the observation station as the center according to the formula (2), as shown in fig. 2:
in the formula (x)t,n,g,yt,n,g,zt,n,g) Coordinates of the target source under the horizontal coordinate system of the nth observation station are obtained; omegao,nAnd ρo,nLongitude and latitude of the nth observation station respectively; r is the radius of the earth;
step S103.2: obtaining the azimuth angle theta according to the formula (2)t,nAnd longitude ωtLatitude rhotAnd ionospheric pseudo-height hnThe relationship of (1):
step S103.3: a triangle is constructed through the observation station, the sphere center point and the ionosphere, the triangle is shown as delta ABC in figure 3, and the elevation angle beta is obtained by utilizing the sine theorem of the triangletAnd longitude ωtLatitude rhotAnd ionospheric pseudo-height h relation:
in the formula (I), the compound is shown in the specification,the internal angle of the triangle with the center point as the vertex is shown.
Specifically, the step S104 includes:
step S104.1: converting the longitude and latitude coordinates of the d correction source into a horizon coordinate with the observation station as the center according to the formula (5):
in the formula (x)d,n,g,yd,n,g,zd,n,g) Coordinates of a d correction source target source in a horizontal coordinate system of an nth observation station;
step S104.2: obtaining the azimuth angle theta according to the formula (5)c,d,nAnd longitude ωc,dAnd latitude rhoc,dThe relationship of (1):
step S104.3: from Δ ABC shown in FIG. 3, the elevation angle β is obtained by using the sine theorem of trianglesc,d,nAnd longitude ωc,dLatitude rhoc,dAnd ionospheric pseudo-height hnThe relationship of (1):
in the formula (I), the compound is shown in the specification,
specifically, the step S105 includes:
step S105.1: the nth observation station utilizes an array signal model { x ] corresponding to the collected K signal samplesn(tk)}1≤k≤KConstructing an array output covariance matrix
Step S105.2: each of the observers transmits the constructed covariance matrix to a central station of the N observers, as shown in fig. 4, wherein the 1 st observer station (observer station 1) is the central station, and the other observers transmit the constructed covariance matrix to the 1 st observer station.
Specifically, the step S106 includes:
the central station utilizes the covariance matrix of the N observersJoint estimation target source longitude omega based on maximum likelihood criterion constructiontLatitude rhotAnd the ionized layer virtual height { hn}1≤n≤NAnd a multi-array amplitude-phase error matrix { gamman}1≤n≤NThe cost function of (2); the cost function is:
wherein h ═ h1h2…hN]TIndicating ionospheric pseudo-height parameters;representing array amplitude-phase error parameters, wherein vecd () represents that diagonal elements of a diagonal matrix are extracted to form vectors; II type⊥[ΓnAn(ωt,ρt,hn)]A matrix of orthogonal projections is represented which,
Π⊥[ΓnAn(ωt,ρt,hn)]=I-ΓnAn(ωt,ρt,hn)((ΓnAn(ωt,ρt,hn))HΓnAn(ωt,ρt,hn))-1(ΓnAn(ωt,ρt,hn))H, (1≤n≤N)
wherein I is an identity matrix.
Specifically, the step S107 includes:
step S107.1: will omegat、ρtAnd { hn}1≤n≤NAs a first set of parameters, { Γn}1≤n≤NAs a second set of parameters, the second set of parameters is fixed to the current update value, i.e. { Γ }n}1≤n≤NIs fixed toFix g asEstimating a first group of parameters according to a relation between an azimuth angle and an elevation angle of a target source signal reaching N observation stations and a longitude and latitude and an ionospheric virtual height of the target source respectively, a relation between an azimuth angle and an elevation angle of D correction source signals reaching N observation stations and a longitude and latitude and a virtual height of the ionospheric layer respectively, and the cost function according to an equation (10):
wherein mu is a step factor, mu is more than 0 and less than 1, muiIs the ith iteration step size factor;and h(i)Are all the ith iteration result;and h(i+1)All are the (i +1) th iteration results;is a gradient vector;is a Hessian matrix;andare respectively expressed as
Wherein the expressions of the elements are respectively
In the formula, n1Representing the n-th matrix1Line, n2Representing the n-th matrix2Columns;
it is worth mentioning that it is possible to show,andandthe expressions of the elements are respectively the same;
in the formula InIs the radius of the uniform circular array of the nth observation station, lambda is the signal wavelength,is the last column vector in the (D +1) × (D +1) identity matrix.
Step S107.2: fixing the first set of parameters to the current update value, i.e. ωt、ρtAnd h are respectively fixed toAndaccording to the relation between the azimuth angle and the elevation angle of the target source signal reaching the N observation stations and the longitude and latitude and the virtual height of the ionized layer, the relation between the azimuth angle and the elevation angle of the D correction source signal reaching the N observation stations and the longitude and latitude and the virtual height of the ionized layer and the cost function, the second group of parameters are optimized and solved according to the formula (11):
in the formula, g(i)Is the result of the ith iteration; g(i+1)Is the (i +1) th iteration result;is a gradient vector;is a Hessian matrix;
wherein the expressions of the elements are respectively
Step S107.3: and (3) alternately carrying out optimization solution on the first set of parameters and the second set of parameters according to the formula (10) and the formula (11) until iteration converges.
To verify the effect of the present invention, the following experimental data are provided.
Assuming that 3 observation stations are used for positioning the short-wave target source, the longitude of the 1 st observation station is 124.49 degrees of east longitude, the latitude of the 1 st observation station is 40.75 degrees of north latitude, the longitude of the 2 nd observation station is 114.04 degrees of east longitude, the latitude of the 2 nd observation station is 34.68 degrees of north latitude, the longitude of the 3 rd observation station is 118.30 degrees of east longitude, and the latitude of the 3 rd observation station is 26.80 degrees of north latitude, wherein the 1 st observation station is defaulted as a central station; the longitude of the short wave target source is 122.46 degrees, and the latitude is 27.82 degrees; now two short wave correction sources are placed, the longitude of the 1 st correction source is 123.62 degrees for east longitude, 28.68 degrees for latitude for north latitude, the longitude of the 2 nd correction source is 124.54 degrees for east longitude, and 29.96 degrees for latitude for north latitude. Even circular arrays are installed on 3 observation stations, each circular array comprises 10 antennas, the number of signal sample points for direct positioning is 500, the ionospheric virtual heights of short-wave target source signals and correction source signals reaching the 3 observation stations are 270 kilometers, 310 kilometers and 360 kilometers respectively, and the target source signal-to-noise ratio and the correction source signal-to-noise ratio are assumed to be equal.
Firstly, fixing the ratio of the radius to the wavelength of the circular array to be 1.5, and respectively giving variation curves of the target source positioning root mean square error, the ionized layer virtual height estimation root mean square error and the array amplitude phase error estimation root mean square error along with the signal-to-noise ratio of the target source in the graphs from 5 to 7; then, the signal-to-noise ratio of the target source is fixed to be 10dB, and the variation curves of the target source positioning root-mean-square error, the ionosphere virtual height estimation root-mean-square error and the array amplitude phase error estimation root-mean-square error along with the ratio of the circle array radius to the wavelength are respectively given in the graphs from fig. 8 to fig. 10.
The advantages of the disclosed method can be seen in fig. 5-10, and are significantly improved as the target source signal-to-noise ratio increases.
The above shows only the preferred embodiments of the present invention, and it should be noted that it is obvious to those skilled in the art that various modifications and improvements can be made without departing from the principle of the present invention, and these modifications and improvements should also be considered as the protection scope of the present invention.
Claims (5)
1. A short-wave multi-station direct positioning method under the condition of existence of a correction source is characterized by comprising the following steps:
step 1: d short wave correction sources with known longitude and latitude are simultaneously placed on the periphery of the area where the short wave target source is located;
step 2: receiving a target source signal and D correction source signals by using N observation stations, wherein each observation station acquires K signal samples by using a uniform circular array which is not corrected by a channel, and establishes an array signal model corresponding to the K signal samples;
and step 3: determining the relation between the azimuth angle of a target source signal reaching N observation stations and the longitude and latitude of a target source respectively, and determining the relation between the elevation angle of the target source signal reaching the N observation stations and the longitude and latitude of the target source and the virtual height of an ionized layer respectively;
and 4, step 4: determining the relation between the azimuth angle of the D-th correction source signal reaching the N observation stations and the longitude and latitude of the D-th correction source respectively, and determining the relation between the elevation angle of the D-th correction source signal reaching the N observation stations and the longitude and latitude of the D-th correction source and the virtual height of an ionized layer respectively, wherein D is more than or equal to 1 and less than or equal to D;
and 5: each observation station utilizes an array signal model corresponding to the collected K signal samples to construct a covariance matrix, and transmits the covariance matrix to a central station in the N observation stations;
step 6: the central station constructs a cost function of a joint estimation target source longitude and latitude, ionosphere height and multi-array amplitude-phase error matrix based on a maximum likelihood criterion by using covariance matrixes of N observation stations;
the step 6 comprises the following steps:
the central station utilizes the covariance matrix of the N observersJoint estimation target source longitude omega based on maximum likelihood criterion constructiontLatitude rhotAnd the ionized layer virtual height { hn}1≤n≤NAnd a multi-array amplitude-phase error matrix { gamman}1≤n≤NThe cost function of (2); the cost function is:
wherein h ═ h1 h2 … hN]TIndicating ionospheric pseudo-height parameters;representing an array amplitude and phase error parameter; II type⊥[ΓnAn(ωt,ρt,hn)]Representing orthogonal projection matrices, Π⊥[ΓnAn(ωt,ρt,hn)]=I-ΓnAn(ωt,ρt,hn)((ΓnAn(ωt,ρt,hn))HΓnAn(ωt,ρt,hn))-1(ΓnAn(ωt,ρt,hn))H,1≤n≤N
Wherein I is an identity matrix;An(ωt,ρt,hn) For the array manifold matrix of the nth observation station, vecd () represents that the diagonal elements of the diagonal matrix are extracted to form a vector;
and 7: according to the relation between the azimuth angle of a target source signal reaching N observation stations and the longitude and latitude of a target source, the relation between the elevation angle of the target source signal reaching N observation stations and the longitude and latitude of the target source and the virtual height of an ionized layer, the relation between the azimuth angle of a d correction source signal reaching N observation stations and the longitude and latitude of a d correction source, the relation between the elevation angle of the d correction source signal reaching N observation stations and the longitude and latitude of the d correction source and the virtual height of the ionized layer and the cost function, joint estimation is carried out on the longitude and latitude of the target source, the virtual height of the ionized layer and multi-array amplitude-phase errors by using an alternating iteration algorithm, so that the position information of the target is determined;
the step 7 comprises the following steps:
step 7.1: will omegat、ρtAnd { hn}1≤n≤NAs a first set of parameters, { Γn}1≤n≤NAs a second set of parameters, the second set of parameters is fixed to the current update value, i.e. { Γ }n}1≤n≤NIs fixed toFix g asEstimating a first group of parameters according to a relation between azimuth angles of a target source signal reaching N observation stations and longitude and latitude of a target source, a relation between elevation angles of the target source signal reaching the N observation stations and longitude and latitude of the target source and virtual height of an ionized layer, a relation between azimuth angles of a d correction source signal reaching the N observation stations and longitude and latitude of a d correction source, a relation between elevation angles of the d correction source signal reaching the N observation stations and longitude and latitude of the d correction source and virtual height of the ionized layer and the cost function, wherein the first group of parameters are estimated according to a formula (10):
where μ is the step factor, 0<μ<1,μiIs the ith iteration step size factor;and h(i)Are all the ith iteration result;and h(i+1)All are the (i +1) th iteration results;is a gradient vector;is a Hessian matrix;
wherein the expressions of the elements are respectively
In the formula (I), the compound is shown in the specification,
in the formula InIs the radius of the uniform circular array of the nth observation station, lambda is the signal wavelength,last column vector, n, in order identity matrix1Representing the n-th matrix1Line, n2Representing the n-th matrix2The columns of the image data are,is n th1The current update value of the amplitude-phase error matrix of the individual observation stations,is n th1An array manifold matrix of individual observation stations,for the signal to reach the n-th1Ionospheric pseudo-height, a, experienced by an observer stationn(ωt,ρt,hn) Array manifold vector for target source signal arriving at nth observation stationt,nFor the azimuth angle, beta, of the target source signal arriving at the nth observation stationt,nFor the elevation angle, beta, of the target source signal to the nth observation stationc,1,nCorrecting the elevation angle, omega, of the source signal arriving at the nth observation station for the 1 stc,1Longitude, p, for the 1 st correction sourcec,1Is the latitude, beta, of the 1 st correction sourcec,D,nCorrecting the elevation angle, omega, of the source signal arriving at the nth observation station for the Dc,DLongitude, p, for the Dth correction sourcec,DFor the latitude, ω, of the D-th correction sourcec,dLongitude, p, for the d correction sourcec,dIs the latitude, θ, of the d-th correction sourcec,d,nFor the d-th corrected source signal to the nth observation stationc,d,nFor the d-th corrected source signal to the nth observation station in terms of elevation angle, ωo,nLongitude, p, for the nth observation stationo,nAs is the latitude of the nth observation station, r is the radius of the earth;
step 7.2: fixing the first set of parameters to the current update value, i.e. ωt、ρtAnd h are respectively fixed toAndaccording to the relation between the azimuth angle of the target source signal reaching N observation stations and the longitude and latitude of the target source, the relation between the elevation angle of the target source signal reaching N observation stations and the longitude and latitude of the target source and the virtual height of the ionized layer, the relation between the azimuth angle of the d correction source signal reaching N observation stations and the longitude and latitude of the d correction source, the relation between the elevation angle of the d correction source signal reaching N observation stations and the longitude and latitude of the d correction source and the virtual height of the ionized layer and the cost function, the second group of parameters are optimized and solved according to the formula (11):
in the formula, g(i)Is the result of the ith iteration; g(i+1)Is the (i +1) th iteration result;is a gradient vector;is a Hessian matrix;
wherein the expressions of the elements are respectively
step 7.3: and (3) alternately carrying out optimization solution on the first set of parameters and the second set of parameters according to the formula (10) and the formula (11) until iteration converges.
2. The shortwave multi-station direct positioning method under the condition of existence of the correction source as claimed in claim 1, wherein the array signal model in the step 2 is:
in the formula, xn(tk) Receiving signals for a kth array of an nth observation station; sc,n,d(tk) A complex envelope for the d-th corrected source signal to reach the nth observation station; st,n(tk) A complex envelope for the target source signal to reach the nth observation station; epsilonn(tk) Uniform circular array additive noise of the nth observation station;a complex envelope vector for the signal arriving at the nth observation station; h isnIonospheric pseudo-heights experienced by signals arriving at the nth observation station; a isn(ωc,d,ρc,d,hn) For the array manifold vector, ω, of the d-th corrected source signal arriving at the nth observation stationc,dTo correct for source longitude, pc,dCorrecting the source latitude; a isn(ωt,ρt,hn) Array manifold vector, omega, for the arrival of target source signals at the nth observation stationtAs the target source longitude, ρtIs the target source latitude;an array manifold matrix for an nth observation station; gamma-shapednIs the amplitude-phase error matrix of the nth observation station.
3. The shortwave multi-station direct positioning method in the presence of a correction source according to claim 1, characterized in that said step 3 comprises:
step 3.1: converting the longitude and latitude coordinates of the target source into a horizon coordinate with the observation station as the center according to the formula (2):
in the formula (x)t,n,g,yt,n,g,zt,n,g) Coordinates of the target source under the horizontal coordinate system of the nth observation station are obtained; omegao,nAnd ρo,nLongitude and latitude of the nth observation station respectively; r is the radius of the earth;
step 3.2: obtaining the azimuth angle theta according to the formula (2)t,nAnd longitude ωtLatitude rhotThe relationship of (1):
Step 3.3: a triangle is constructed through the observation station, the sphere center point and the ionized layer, and the elevation angle beta is obtained by utilizing the sine theorem of the trianglet,nAnd longitude ωtLatitude rhotAnd ionospheric pseudo-height hnThe relationship of (1):
4. The shortwave multi-station direct positioning method in the presence of a correction source according to claim 1, characterized in that said step 4 comprises:
step 4.1: converting the longitude and latitude coordinates of the d correction source into a horizon coordinate with the observation station as the center according to the formula (5):
in the formula (x)d,n,g,yd,n,g,zd,n,g) Coordinates of the d correction source in a horizontal coordinate system of the nth observation station;
step 4.2: obtaining the azimuth angle theta according to the formula (5)c,d,nAnd longitude ωc,dAnd latitude rhoc,dThe relationship of (1):
step 4.3: using the sine theorem of triangle to obtain the elevation angle betac,d,nAnd longitude ωc,dLatitude rhoc,dAnd ionospheric pseudo-height hnThe relationship of (1):
in the formula (I), the compound is shown in the specification,
5. the shortwave multi-station direct positioning method in the presence of a correction source according to claim 2, characterized in that said step 5 comprises:
step 5.1: the nth observation station utilizes an array signal model { x ] corresponding to the collected K signal samplesn(tk)}1≤k≤KConstructing an array output covariance matrix
Step 5.2: each of the observatory stations communicates the constructed covariance matrix to a central station of the N observatory stations.
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