CN115792963B - Ionosphere correction method based on GIM model, electronic equipment and storage medium - Google Patents

Ionosphere correction method based on GIM model, electronic equipment and storage medium Download PDF

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CN115792963B
CN115792963B CN202310101658.0A CN202310101658A CN115792963B CN 115792963 B CN115792963 B CN 115792963B CN 202310101658 A CN202310101658 A CN 202310101658A CN 115792963 B CN115792963 B CN 115792963B
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黄满义
付乃峰
王鹏程
郭瑞
邓智博
闫明明
刘永成
哈琳
李峰辉
李兴国
程艳
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Tianjin Yunyao Aerospace Technology Co ltd
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Abstract

The invention provides an ionosphere correction method based on a GIM model, electronic equipment and a storage medium, which comprise the following steps: s1, transmitting GNSS observation data to a global ionosphere model GIM; s2, constructing a three-dimensional ionosphere rapid model through a global ionosphere model GIM and an ionosphere experience model; s3, performing ionosphere correction on the three-dimensional ionosphere rapid model. The invention has the beneficial effects that: ionosphere correction for global satellite navigation observations at different elevation angles on satellite platforms of different orbital heights; the obtained three-dimensional electron density with high precision and high resolution can be used for researching transmission characteristics of radio signals and monitoring electromagnetic environment abnormality.

Description

Ionosphere correction method based on GIM model, electronic equipment and storage medium
Technical Field
The invention belongs to the technical field of satellite navigation, and particularly relates to an ionosphere correction method based on a GIM model, electronic equipment and a storage medium.
Background
Classical ionospheric effect correction methods include two types: 1. for a dual-frequency receiver, the method can be used for constructing a non-ionosphere cancellation ionosphere influence; 2. the total amount of path electrons can be corrected for the ground-based single frequency receiver, typically by combining the global ionosphere model (global ionosphere model, GIM) with the projection function. For ionosphere correction of global satellite navigation (global navigation satellites system, GNSS) observations at different elevation angles on satellite platforms with different orbit heights, the GIM model is not suitable for the ionosphere correction method by combining a projection function, and therefore, the method is proposed to track a path of a transmitting end-receiving end based on a three-dimensional ionosphere grid to obtain the total quantity of electrons so as to carry out subsequent ionosphere influence correction.
Disclosure of Invention
In view of the above, the present invention is directed to an ionospheric correction method, an electronic device and a storage medium based on a GIM model, so as to solve the problem that an ionospheric empirical model such as a global reference ionosphere (intelnational reference ionosphere, IRI) model has a bias in an ionospheric top structure when the GIM model is not adapted to ionospheric data correction under complex conditions in combination with a projection function.
In order to achieve the above purpose, the technical scheme of the invention is realized as follows:
an ionosphere correction method based on a GIM model comprises the following steps:
s1, transmitting GNSS observation data to a global ionosphere model GIM;
s2, constructing a three-dimensional ionosphere rapid model through a global ionosphere model GIM and an ionosphere experience model;
s3, performing ionosphere correction on the three-dimensional ionosphere rapid model.
Further, the ionospheric empirical model in step S2 is an IRI model.
Further, the building of the three-dimensional ionosphere rapid model in step S2 includes the steps of:
s21, obtaining a global ionosphere model GIM real-time product;
s22, calculating and storing a three-dimensional grid time sequence of the IRI model;
s23, combining the global ionosphere model GIM real-time product and the three-dimensional grid time sequence of the IRI model to calculate and obtain the three-dimensional ionosphere rapid model.
Further, the calculating a three-dimensional ionosphere fast model in step S23 includes the following steps:
s231, integrating to obtain IRI model
Figure SMS_1
In horizontal grid->
Figure SMS_2
Vertical electron count +.>
Figure SMS_3
Figure SMS_4
wherein ,
Figure SMS_5
for IRI model->
Figure SMS_6
In horizontal grid->
Figure SMS_7
Vertical electron total at ∈ ->
Figure SMS_8
Is a grid vertical interval;
s232, calculating the global ionosphere model GIM and IRI model in the horizontal grid
Figure SMS_9
Proportional coefficient between vertical electron totals +.>
Figure SMS_10
Figure SMS_11
wherein ,
Figure SMS_12
for global ionosphere model GIM and IRI model in horizontal grid +.>
Figure SMS_13
Proportional coefficient between vertical electron populations, +.>
Figure SMS_14
Horizontal grid +.>
Figure SMS_15
Vertical electron total amount->
Figure SMS_16
For IRI model->
Figure SMS_17
In horizontal grid->
Figure SMS_18
Vertical electron count at the location;
s233, correcting the IRI model electron density by using the vertical electron total amount proportionality coefficient;
Figure SMS_19
wherein ,
Figure SMS_20
is the ionosphere model under the global ionosphere model GIM auxiliary IRI at fixed moment
Figure SMS_21
Electron density at the grid, +.>
Figure SMS_22
For global ionosphere model GIM and IRI model in horizontal grid +.>
Figure SMS_23
A proportionality coefficient between the vertical electron totals.
Further, the ionospheric correction in step S3 includes the steps of:
s31, at the time t, GNSS radio signals are transmitted from the navigation satellite
Figure SMS_24
Departure from place is at->
Figure SMS_25
A receiver at the location receives;
s32, assume GNSS radio signal slave
Figure SMS_26
To->
Figure SMS_27
The propagation path is not reflected, the GNSS radio signal path is +.>
Figure SMS_28
To->
Figure SMS_29
A straight line between the two;
s33, calculating GNSS radio signal slave at t moment
Figure SMS_30
To->
Figure SMS_31
Ionospheric corrections on the propagation path.
Further, the GNSS radio signal at the time t is calculated in step S33
Figure SMS_32
To->
Figure SMS_33
Ionospheric corrections on the propagation path include the steps of:
s331, searching for the nearest three-dimensional ionosphere grid at t time, assuming that
Figure SMS_34
At moment, obtaining a t moment three-dimensional ionosphere by linear interpolationNet:
Figure SMS_35
;/>
wherein ,
Figure SMS_36
for the three-dimensional ionosphere grid at time t +.>
Figure SMS_37
Is->
Figure SMS_38
A time three-dimensional ionosphere grid,
Figure SMS_39
is->
Figure SMS_40
Three-dimensional ionosphere grid at moment;
s332, integral obtaining
Figure SMS_41
To->
Figure SMS_42
Total amount of oblique electrons on propagation path->
Figure SMS_43
Figure SMS_44
wherein ,
Figure SMS_45
is the total amount of oblique electrons>
Figure SMS_46
For the three-dimensional ionosphere grid at time t +.>
Figure SMS_47
Is that
Figure SMS_48
Signal penetration distance at the grid;
s333, assume signal frequency as
Figure SMS_49
Then the GNSS radio signal at time t is from +.>
Figure SMS_50
To->
Figure SMS_51
Ionospheric correction on propagation path +.>
Figure SMS_52
The method comprises the following steps:
Figure SMS_53
wherein ,
Figure SMS_54
for time t GNSS radio signal from +.>
Figure SMS_55
To->
Figure SMS_56
Ionospheric corrections on the propagation path,
Figure SMS_57
is the total amount of oblique electrons>
Figure SMS_58
Is the signal frequency.
Further, an electronic device includes a processor and a memory communicatively coupled to the processor and configured to store instructions executable by the processor, the memory storing instructions executable by the processor, the processor configured to perform the GIM model-based ionosphere correction method described above.
Further, a computer readable storage medium stores a computer program which when executed by a processor implements the GIM model-based ionosphere correction method.
Compared with the prior art, the ionosphere correction method, the electronic equipment and the storage medium based on the GIM model have the following advantages:
according to the ionosphere correction method, the electronic equipment and the storage medium based on the GIM model, ionosphere correction of global satellite navigation (global navigation satellites system, GNSS) observation at different altitudes on satellite platforms at different orbit heights is realized; the obtained three-dimensional electron density with high precision and high resolution can be used for researching transmission characteristics of radio signals and monitoring electromagnetic environment abnormality.
Drawings
The accompanying drawings, which are included to provide a further understanding of the invention and are incorporated in and constitute a part of this specification, illustrate embodiments of the invention and together with the description serve to explain the invention. In the drawings:
FIG. 1 is a schematic flow chart of an overall method according to an embodiment of the invention;
FIG. 2 is a schematic diagram of the ionospheric vertical electron count of the IRI2016 model according to one embodiment of the present invention;
FIG. 3 is a schematic diagram of the total ionospheric vertical electron count for the GIM model according to the embodiment of the invention;
FIG. 4 is a schematic diagram showing the distribution of the total vertical electron quantity of the improved ionosphere model according to the embodiment of the present invention;
FIG. 5 is a schematic diagram of electron density at 340km of an ionosphere of an IRI2016 model according to an embodiment of the present invention;
FIG. 6 is a schematic view of electron density at 340km of ionosphere of the improved model according to an embodiment of the present invention.
Detailed Description
It should be noted that, without conflict, the embodiments of the present invention and features of the embodiments may be combined with each other.
In the description of the present invention, it should be understood that the terms "center", "longitudinal", "lateral", "upper", "lower", "front", "rear", "left", "right", "vertical", "horizontal", "top", "bottom", "inner", "outer", etc. indicate orientations or positional relationships based on the orientations or positional relationships shown in the drawings, are merely for convenience in describing the present invention and simplifying the description, and do not indicate or imply that the devices or elements referred to must have a specific orientation, be configured and operated in a specific orientation, and thus should not be construed as limiting the present invention. Furthermore, the terms "first," "second," and the like, are used for descriptive purposes only and are not to be construed as indicating or implying a relative importance or implicitly indicating the number of technical features indicated. Thus, a feature defining "a first", "a second", etc. may explicitly or implicitly include one or more such feature. In the description of the present invention, unless otherwise indicated, the meaning of "a plurality" is two or more.
In the description of the present invention, it should be noted that, unless explicitly specified and limited otherwise, the terms "mounted," "connected," and "connected" are to be construed broadly, and may be either fixedly connected, detachably connected, or integrally connected, for example; can be mechanically or electrically connected; can be directly connected or indirectly connected through an intermediate medium, and can be communication between two elements. The specific meaning of the above terms in the present invention can be understood by those of ordinary skill in the art in a specific case.
The invention will be described in detail below with reference to the drawings in connection with embodiments.
As shown in fig. 1, fig. 1 is a method technical roadmap (wherein GNSS observation data is data obtained by processing after a receiver receives a GNSS radio signal, and the receiver processes the GNSS radio signal as a receiver existing processing technology), and an ionosphere correction method based on a GIM model includes the following steps:
constructing a three-dimensional ionosphere rapid grid time sequence:
1. obtaining global ionosphere model GIM post-processing products (namely GNSS observations) through an IGS service center, or obtaining global ionosphere model GIM real-time products (mesh size 71×73, latitude 2.5 °, longitude 5 °);
2. pre-calculating and storing an IRI model three-dimensional grid time sequence for ionosphere real-time correction or post-processing analysis (grid size 71×73×29, latitude 2.5 °, longitude 5 °, altitude is gradient interval based on ionosphere density);
3. the specific calculation method of the ionosphere model under the auxiliary IRI of the GIM model at a certain fixed moment is as follows:
1) Integral obtaining IRI model
Figure SMS_59
In horizontal grid->
Figure SMS_60
Vertical electron count +.>
Figure SMS_61
Figure SMS_62
wherein ,
Figure SMS_63
for IRI model->
Figure SMS_64
In horizontal grid->
Figure SMS_65
Vertical electron total at ∈ ->
Figure SMS_66
Are vertically spaced apart. />
2) Computing global ionosphere model GIM and IRI model in horizontal grid
Figure SMS_67
Proportional coefficient between vertical electron totals +.>
Figure SMS_68
Figure SMS_69
wherein ,
Figure SMS_70
for global ionosphere model GIM and IRI model in horizontal grid +.>
Figure SMS_71
Proportional coefficient between vertical electron populations, +.>
Figure SMS_72
Horizontal grid +.>
Figure SMS_73
Vertical electron total amount->
Figure SMS_74
For IRI model->
Figure SMS_75
In horizontal grid->
Figure SMS_76
Vertical electron count at the location.
3) Correcting the IRI model electron density by using the vertical electron total amount proportionality coefficient;
Figure SMS_77
wherein ,
Figure SMS_78
is the ionosphere model under the auxiliary IRI of the GIM model at fixed time>
Figure SMS_79
Electron density at the grid, +.>
Figure SMS_80
For global ionosphere model GIM and IRI model in horizontal grid +.>
Figure SMS_81
A proportionality coefficient between the vertical electron totals.
Ionospheric correction under complex paths:
at a given time t, a GNSS radio signal is transmitted from the navigation satellite
Figure SMS_83
Departure from place is at->
Figure SMS_85
A receiver at the location receives. Suppose that GNSS radio signal is from +.>
Figure SMS_87
To->
Figure SMS_82
No reflection (especially GNSS reflection event) occurs on the propagation path, which can be considered +.>
Figure SMS_86
To->
Figure SMS_88
Straight line between. The GNSS radio signal at time t can be calculated from +.>
Figure SMS_89
To->
Figure SMS_84
Ionospheric effects on propagation paths:
1) Finding the nearest three-dimensional ionosphere grid at time t (assumed to be
Figure SMS_90
Time of day), a three-dimensional ionosphere grid at time t can be obtained by linear interpolation:
Figure SMS_91
wherein ,
Figure SMS_92
for the three-dimensional ionosphere grid at time t +.>
Figure SMS_93
Is->
Figure SMS_94
A time three-dimensional ionosphere grid,
Figure SMS_95
is->
Figure SMS_96
Three-dimensional ionosphere grid at the moment. />
2) Integral acquisition
Figure SMS_97
To->
Figure SMS_98
Total amount of oblique electrons on propagation path->
Figure SMS_99
Figure SMS_100
wherein ,
Figure SMS_101
is the total amount of oblique electrons>
Figure SMS_102
For the three-dimensional ionosphere grid at time t +.>
Figure SMS_103
Is that
Figure SMS_104
Signal penetration distance at the mesh.
3) Assuming signal frequency
Figure SMS_105
Then the GNSS radio signal at time t is from +.>
Figure SMS_106
To->
Figure SMS_107
Ionospheric correction on propagation path +.>
Figure SMS_108
The method comprises the following steps:
Figure SMS_109
wherein ,
Figure SMS_110
for time t GNSS radio signal from +.>
Figure SMS_111
To->
Figure SMS_112
Ionospheric corrections on the propagation path,
Figure SMS_113
is the total amount of oblique electrons>
Figure SMS_114
Is the signal frequency.
In a preferred embodiment of the present invention, an electronic device is provided that includes a processor and a memory communicatively coupled to the processor for storing instructions executable by the processor, the memory storing instructions executable by the processor for performing the GIM model-based ionosphere correction method described above.
In a preferred embodiment of the present invention, a computer readable storage medium is provided, storing a computer program which, when executed by a processor, implements the GIM model-based ionosphere correction method.
In the invention, although the GIM model is combined with the projection function mode and is not suitable for ionosphere correction under complex conditions, the single GIM model can provide ionosphere vertical electron total amount horizontal and horizontal gradient information; on the other hand, the global reference ionosphere (intelnational reference ionosphere, IRI) model can provide an ionosphere vertical structure based on experimental information such as E, F and the like such as layer peak heights, peak densities, elevations and the like. And combining the characteristics of the GIM and the IRI models to construct a three-dimensional ionosphere rapid grid time sequence, and then tracking a path of a transmitting end and a receiving end to obtain the total quantity of electrons to carry out subsequent ionosphere influence correction.
Many IGS stations and occultation satellites now provide dual-frequency positioning antennas and occultation antenna observations that can obtain ionosphere data for satellites ranging from negative altitudes (typically from the time of occultation of the satellite near the ground) to positive altitudes. Based on the orbits of the satellites and the navigation ephemeris, we can integrate the electron density along the path of the GNSS radio signal from the transmitting end to the receiving end based on the three-dimensional electron density fast model (the path bending of the ionosphere part can be ignored) to obtain the total electron quantity at the observation time. And analyzing the relation between the precision and the satellite orbit height, the signal transmission altitude angle, the local time, the annual product day and the receiver latitude by counting the deviation between the electronic total amount obtained by the actual measurement data and the model data.
Example 1
To verify the superiority of the improved model algorithm obtained by assisting the IRI2016 model with the GIM model, a four-dimensional ionosphere model of 1 month and 1 day is generated through the algorithm, the spatial resolution selects an IRI basic model (2.5 degrees by 2.5 degrees, and the vertical direction is divided into 29 layers according to electron density), and the time resolution is 1 hour. Figures 2-3 show the ionospheric vertical electron count for the IRI2016 and GIM models at zero at 1/2020, it can be seen that the GIM model has more ionospheric fine structure than the IRI2016 model.
And (5) performing ionosphere three-dimensional model reconstruction by using the GIM model to assist the IRI2016 model to obtain an improved model. Fig. 4 shows the vertical electron population distribution of the modified ionosphere model. Comparing fig. 4 with fig. 3, it can be seen that the improved model, in the case of obtaining the vertical structure of the IRI2016 model, the vertical electron population is consistent with the GIM model distribution.
By comparing the electron density at 340km (near ionospheric peak height), it can be found that the vertical electron population two-dimensional structure of the GIM model is transferred near the ionospheric peak height by the algorithm herein, improving the electron population at this height. As shown in fig. 5-6, fig. 5-6 show the electron density at ionosphere 340km for IRI2016 model and improved model at time 1 month 1 day zero 2020.
And selecting RINEX data of the IGS station on the same day, and obtaining the actual measurement ionosphere oblique electron total quantity of each station of the IGS through ionoab software. The observed model result corresponding to the IRI2016 model and the improved model can be obtained through integration along the path, and the poor total amount of the oblique electrons is obtained through statistics of actual measurement data and model integration, so that a conclusion is obtained. From the conclusion, the improved model is worse in the total amount of oblique electrons and more approaching 0 TECu than the IRI2016 model, and the error statistical result is shown as sharp Gaussian distribution. Through statistics, the root mean square error of the IRI2016 model is 5TECu, and the improved model is reduced to be within 3 TECu.
The invention has the advantages that: ionospheric corrections for different elevation angle global satellite navigation (global navigation satellites system, GNSS) observations on satellite platforms of different orbital heights; the obtained three-dimensional electron density with high precision and high resolution can be used for researching transmission characteristics of radio signals and monitoring electromagnetic environment abnormality.
The foregoing description of the preferred embodiments of the invention is not intended to be limiting, but rather is intended to cover all modifications, equivalents, alternatives, and improvements that fall within the spirit and scope of the invention.

Claims (5)

1. The ionosphere correction method based on the GIM model is characterized by comprising the following steps of: the method comprises the following steps:
s1, transmitting GNSS observation data to a global ionosphere model GIM;
s2, constructing a three-dimensional ionosphere rapid model through a global ionosphere model GIM and an ionosphere experience model;
s3, performing ionosphere correction on the three-dimensional ionosphere rapid model;
the ionospheric empirical model in step S2 is an IRI model;
the construction of the three-dimensional ionosphere rapid model in step S2 comprises the steps of:
s21, obtaining a global ionosphere model GIM real-time product;
s22, calculating and storing a three-dimensional grid time sequence of the IRI model;
s23, calculating a three-dimensional ionosphere rapid model by combining a three-dimensional grid time sequence of a global ionosphere model GIM real-time product and an IRI model;
the calculation in step S23 results in a three-dimensional ionosphere fast model comprising the steps of:
s231, integral obtaining IRI model Ne IRI Vertical electron count at horizontal grid i, j
Figure FDA0004155128850000011
Figure FDA0004155128850000012
wherein ,
Figure FDA0004155128850000013
for IRI model Ne IRI The total number of vertical electrons, Δh, at horizontal grid i, j k Is a grid vertical interval;
s232, calculating a ratio coefficient R between the total vertical electron quantity of the global ionosphere model GIM and the IRI model at the horizontal grid i, j i,j
Figure FDA0004155128850000021
wherein ,Ri,j For the proportionality coefficient between the global ionosphere model GIM and the IRI model in the vertical electron population at the horizontal grid i, j,
Figure FDA0004155128850000022
vertical electron population at horizontal grid i, j for global ionosphere model GIM, +.>
Figure FDA0004155128850000023
For IRI model Ne IRI The total number of vertical electrons at horizontal grid i, j;
s233, correcting the IRI model electron density by using the vertical electron total amount proportionality coefficient;
Ne i,j,k cor =R i,j ·Ne i,j,k IRI
wherein ,Nei,j,k cor Is the electron density of the ionosphere model at the i, j, k grids under the assistance of the global ionosphere model GIM at fixed time and R i,j Is the proportionality coefficient between the global ionosphere model GIM and the IRI model in the vertical electron population at the horizontal grid i, j.
2. The ionospheric correction method based on GIM model as claimed in claim 1, wherein: the ionosphere correction in step S3 includes the steps of:
s31, at time t, GNSS radio signal is transmitted from navigation satellite X T Is started at X R A receiver at the location receives;
s32, assume GNSS radio signal slave X T To X R The propagation path is not reflected, the GNSS radio signal path is X T To X R A straight line between the two;
s33, calculating GNSS radio signal slave X at t moment T To X R Ionospheric corrections on the propagation path.
3. The GIM model-based GIM of claim 2The ionosphere correction method is characterized in that: the GNSS radio signal slave X at time t is calculated in step S33 T To X R Ionospheric corrections on the propagation path include the steps of:
s331, searching for the nearest three-dimensional ionosphere grid at t time, assuming t 0 ,t 1 At moment, obtaining a three-dimensional ionosphere grid at t moment through linear interpolation:
Figure FDA0004155128850000031
wherein ,Nei,j,k t For a three-dimensional ionosphere grid at time t,
Figure FDA0004155128850000034
at t 0 Time three-dimensional ionosphere grid->
Figure FDA0004155128850000035
At t 1 Three-dimensional ionosphere grid at moment;
s332, integrating to obtain X T To X R Total amount of oblique electrons sTec on propagation path t
Figure FDA0004155128850000032
Wherein sTec t Ne is the total amount of oblique electrons i,j,k t For a three-dimensional ionosphere grid at time t, deltas i,j,k The signal penetration distance at the grid of i, j and k is;
s333, assuming that the signal frequency is f, the GNSS radio signal at time t is derived from X T To X R Ionospheric correction on propagation path
Figure FDA0004155128850000033
The method comprises the following steps:
Figure FDA0004155128850000041
wherein ,
Figure FDA0004155128850000042
for time t GNSS radio signal slave X T To X R Ionospheric correction on propagation path, sTec t And f is the signal frequency, which is the total amount of oblique electrons.
4. An electronic device comprising a processor and a memory communicatively coupled to the processor for storing processor-executable instructions, characterized in that: the memory stores instructions executable by the processor for performing the GIM model-based ionosphere correction method of any one of claims 1-3.
5. A computer-readable storage medium storing a computer program, characterized in that: the computer program, when executed by a processor, implements the GIM model-based ionosphere correction method of any of claims 1-3.
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