CN111162845A - Sea area sight distance channel generation method - Google Patents

Sea area sight distance channel generation method Download PDF

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Publication number
CN111162845A
CN111162845A CN202010039118.0A CN202010039118A CN111162845A CN 111162845 A CN111162845 A CN 111162845A CN 202010039118 A CN202010039118 A CN 202010039118A CN 111162845 A CN111162845 A CN 111162845A
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ray
channel
path
parameters
propagation
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王珏
丁瑞
纪雪飞
李业
孙强
张艳秋
厉凯
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Nantong University
Nantong Research Institute for Advanced Communication Technologies Co Ltd
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Nantong Research Institute for Advanced Communication Technologies Co Ltd
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    • HELECTRICITY
    • H04ELECTRIC COMMUNICATION TECHNIQUE
    • H04BTRANSMISSION
    • H04B13/00Transmission systems characterised by the medium used for transmission, not provided for in groups H04B3/00 - H04B11/00
    • H04B13/02Transmission systems in which the medium consists of the earth or a large mass of water thereon, e.g. earth telegraphy
    • HELECTRICITY
    • H04ELECTRIC COMMUNICATION TECHNIQUE
    • H04BTRANSMISSION
    • H04B17/00Monitoring; Testing
    • H04B17/30Monitoring; Testing of propagation channels
    • H04B17/391Modelling the propagation channel
    • H04B17/3912Simulation models, e.g. distribution of spectral power density or received signal strength indicator [RSSI] for a given geographic region

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  • Computer Networks & Wireless Communication (AREA)
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Abstract

The invention discloses a sea area sight distance channel generation method, which realizes sea area sight distance channel generation through the steps of parameter setting, ray propagation type discrimination, formula rewriting, scattering area generation, height change of a receiving end, parameter calculation, channel generation and the like. The random ray tracing method is used for assuming actual complex factors such as ocean wave change and the like to improve the accuracy of generating the channel, reduce the complexity of generating the channel and enhance the applicability of the ray tracing method, so that the sea area sight distance channel which is more in line with the actual situation is generated.

Description

Sea area sight distance channel generation method
Technical Field
The invention relates to the field of communication, in particular to a sea area line-of-sight channel generation method.
Background
With the ever-increasing marine economy and the increasing activity of marine activities, sea area mobile communication has received a great deal of attention. In order to meet the requirements of future mobile communication applications, high-rate, wide-coverage and low-delay sea communication services need to be developed. As part of basic research, modeling of wireless channels at sea has been studied from different perspectives, and while most of the existing work has focused on studying large-scale propagation path loss in marine-based environments, fast fading channel models have not been well studied and developed.
In the prior art, the channel research is mainly modeled by Ray Tracing (Ray-Tracing). Although ray tracing methods can greatly reduce the complexity of modeling, it is often not possible to accurately describe the propagation path of each ray in a rich scattering environment. But in a marine propagation environment, scattering is typically sparse, which makes it possible to model the channel with low complexity using ray tracing techniques. The ray tracing method can calculate specific ray tracks in the multipath channel modeling, and has obvious advantages for small-scale parameters. Due to the lack of consideration of complex ocean waves on ray tracing method modeling in the prior art, the ray tracing method is still in a blank stage in the sea area sight distance channel modeling field.
Disclosure of Invention
The invention provides a sea area apparent distance channel generation method aiming at solving the technical problem of how to generate a sea area apparent distance channel with low complexity and strong applicability.
In order to solve the technical problems, the technical scheme of the invention is as follows: a method for generating a sea area sight distance channel comprises the following steps:
(1) setting parameters, namely setting natural environment parameters and working system parameters;
(2) judging the ray propagation type, dividing the ray propagation type, determining a ray tracing method calculation formula of each divided type of ray, and performing the next step;
(3) rewriting a formula, namely rewriting a ray tracing method calculation formula of each type of divided ray propagation into a formula taking the moment t as an unknown quantity according to the moving speed of the receiving antenna ship in the ocean;
(4) generating a scattering area, determining the number and the positions of effective scattering points in the sea level, and performing the next step after determining the number and the positions;
(5) the height change of the receiving end is evaluated to the height of the receiving end antenna according to the height change caused by the fluctuation of the sea waves, and the next step is carried out;
(6) calculating parameters, namely calculating to obtain the length of a direct path, the sea level reflection times and the length of a reflection ray propagation path, recording the parameters as the parameters of the Kth reflection arrival path, and performing the next step;
(7) and (4) generating a channel, namely bringing the channel parameters of the arrival path subjected to statistics into a channel generation module to form a sea area line-of-sight channel.
Further, the natural environment parameter includes a wave height.
Further, the working system parameters comprise the height of the transmitting antenna, the height of the receiving antenna, the distance between the transmitting antenna and the receiving antenna and the moving speed of the ship.
Further, the ray tracing method for each type of ray has a calculation formula as follows:
Figure BDA0002367100120000021
wherein d isLOS,dRef,0And dRef,kRespectively representing the lengths of a direct path, a specular reflection path and a scattering path; k is the total number of scattering points;
Figure BDA0002367100120000022
is the phase shift caused by the propagation delay corresponding to the length of each propagation path, f is the carrier frequency, c is the electricalThe magnetic wave propagation speed; gamma is the reflection loss factor, amplitude and the sum factor of gamma
Figure BDA0002367100120000023
In direct proportion.
Further, the effective scattering point position in the step (4) is calculated by the following formula: c. CRef,k(t)=αrcosθu+rsinθu+cRef,0(t) where R is a value of u (0, R), θ is a value of u (0,2 π), α is a compression factor that controls the scattering region.
By adopting the technical scheme, the random ray tracing method is utilized to assume actual complex factors such as ocean wave change and the like so as to improve the accuracy of generating the channel and reduce the complexity of generating the channel; the applicability of the ray tracing method is enhanced, and therefore the sea area sight distance channel which is more in line with the actual situation is generated.
Drawings
FIG. 1 is a schematic flow diagram of the process of the present invention;
FIG. 2 is a diagram illustrating a multipath propagation map of a channel model and a determination of different ray propagation paths according to an embodiment of the present invention;
fig. 3 is a schematic diagram of determining a scattering region according to an embodiment of the present invention.
Detailed Description
The following further describes embodiments of the present invention with reference to the drawings. It should be noted that the description of the embodiments is provided to help understanding of the present invention, but the present invention is not limited thereto. In addition, the technical features involved in the embodiments of the present invention described below may be combined with each other as long as they do not conflict with each other.
Referring to fig. 1, the present embodiment discloses a method for generating a sea-area line-of-sight channel, which includes the following steps:
(1) setting parameters, namely setting natural environment parameters and working system parameters;
(2) judging the ray propagation type, dividing the ray propagation type, determining a ray tracing method calculation formula of each divided type of ray, and performing the next step;
(3) rewriting a formula, namely rewriting a ray tracing method calculation formula of each type of divided ray propagation into a formula taking the moment t as an unknown quantity according to the moving speed of the receiving antenna ship in the ocean;
(4) generating a scattering area, determining the number and the positions of effective scattering points in the sea level, and performing the next step after determining the number and the positions;
(5) the height change of the receiving end is evaluated to the height of the receiving end antenna according to the height change caused by the fluctuation of the sea waves, and the next step is carried out;
(6) calculating parameters, namely calculating to obtain the length of a direct path, the sea level reflection times and the length of a reflection ray propagation path, recording the parameters as the parameters of the Kth reflection arrival path, and performing the next step;
(7) and (4) generating a channel, namely bringing the channel parameters of the arrival path subjected to statistics into a channel generation module to form a sea area line-of-sight channel.
Further, the natural environment parameter includes a wave height.
Further, the working system parameters comprise the height of the transmitting antenna, the height of the receiving antenna, the distance between the transmitting antenna and the receiving antenna and the moving speed of the ship.
Further, the ray tracing method for each type of ray has a calculation formula as follows:
Figure BDA0002367100120000031
wherein d isLOS,dRef,0And dRef,kRespectively representing the lengths of a direct path, a specular reflection path and a scattering path; k is the total number of scattering points;
Figure BDA0002367100120000032
is a phase shift caused by propagation delay corresponding to the length of each propagation path, f is the carrier frequency, c is the electromagnetic wave propagation speed; gamma is the reflection loss factor, amplitude and the sum factor of gamma
Figure BDA0002367100120000033
In direct proportion.
Further, the effective scattering point position in the step (4) is calculated by the following formula: c. CRef,k(t)=αrcosθu+rsinθu+cRef,0(t) where R is a value of u (0, R), θ is a value of u (0,2 π), α is a compression factor that controls the scattering region.
In this embodiment, specifically taking the spatial multipath channel (SCM) model as an example, the simulation needs to generate a channel described by the following formula:
Figure BDA0002367100120000034
wherein:
dLOS,dRef,0and dRef,kThe lengths of the direct path, specular reflection path, and scattering path are represented, respectively.
K is the total number of scattering points and is influenced by the height of the transmitting and receiving ends, the distance between the transmitting and receiving ends and the wave factor.
Figure BDA0002367100120000041
Is a phase shift caused by a propagation delay corresponding to the length of each propagation path, f is a carrier frequency, and c is an electromagnetic wave propagation speed.
Gamma is the reflection loss factor, amplitude and the sum factor of gamma
Figure BDA0002367100120000042
In direct proportion.
The multipath propagation diagram of the channel model and the schematic diagram for distinguishing different ray propagation paths shown in fig. 2; under the condition that a single antenna is adopted at both the transmitting end and the receiving end, the method for calculating the positions of the receiving end, the specular reflection point and the scattering point and the lengths of all paths in the sea area stadium channel comprises the following steps:
the method comprises the following steps: coordinates of the transmitting and receiving end positions, defining a transmitting end position C under the three-dimensional coordinatesTX=(xTX,yTX,zTX) Receiving end vessel initial position CRX(0)=(xRX(0),yRX(0),hRX),hRXIs the height of the receiving antenna.
Step two: when the ship moves, the real-time position of the receiving end changes according to the moving speed of the ship as followsRX(t)=CRX(0) + vt, where v ═ v (v)x,vy,0)。
Step three: adding wave factors, wherein the height of the receiving end randomly changes along with the fluctuation of waves:
Figure BDA0002367100120000043
here, the
Figure BDA0002367100120000044
hwaveThe height of the sea wave is represented by,
Figure BDA0002367100120000045
is kept constant over the number M of samples,
Figure BDA0002367100120000046
Twaveis the time-varying scale of the sea wave, tsIs the sampling interval; in the next new set of M samples,
Figure BDA0002367100120000047
will be re-randomly generated.
Step four: position coordinates of specular reflection points, its position CRef,0(t)=(xRef,0(t),yRef,0(t),zRef,0(t)) the coordinates of the transmitting/receiving end positions are calculated by a geometric method:
Figure BDA0002367100120000048
Figure BDA0002367100120000049
zRef,0(t)=0
step five: determining scattering area and scattering point positionThe scattering point area is shown in FIG. 3, the large area is divided into many small areas dA, each dA is accompanied by a random β defined as the angle between the normal vector and the vertical vector on dA, and is Gaussian-distributed, so that when β value is large, the probability that the corresponding dA is effective is small, the scattering point area is roughly an ellipse, and when the transceiving distance is larger, the scattering point area is correspondingly compressed into a narrow band, the K diffuse reflection point coordinates are generated as follows, firstly, the K diffuse reflection point coordinates are expressed in (x) xRef,0(t),yRef,0(t)) as a center, randomly generating a point in a circular area with R as a radius, wherein the value of R determines the size and the boundary of the scattering area; the coordinates of this diffuse reflection point are then at uThe "compression" in the direction, which is a unit vector perpendicular to the TX-RX direction, on the basis of which the coordinates c of the K diffuse reflection points are obtainedRef,k(t)=αrcosθu+rsinθu+cRef,0(t) where R to u (0, R) and θ to u (0,2 π), α are the compression factors that control the shape of this scattering region.
Step six: the length of each propagation path is calculated and can be obtained by the following formula:
dLOS(t)=||cTX-cRX(t)||
dref,k(t)=||cTX-cref,k(t)||+||cRX(t)-cref,k(t)||,k=0,1,...,K.
the random ray tracing method is used for assuming actual complex factors such as ocean wave change and the like to improve the accuracy of generating channels and reduce the complexity of generating the channels. The applicability of the ray tracing method is enhanced, and therefore the sea area sight distance channel which is more in line with the actual situation is generated.
The embodiments of the present invention have been described in detail with reference to the accompanying drawings, but the present invention is not limited to the described embodiments. It will be apparent to those skilled in the art that various changes, modifications, substitutions and alterations can be made in these embodiments without departing from the principles and spirit of the invention, and the scope of protection is still within the scope of the invention.

Claims (5)

1. A method for generating a sea area line-of-sight channel is characterized by comprising the following steps:
(1) setting parameters, namely setting natural environment parameters and working system parameters;
(2) judging the ray propagation type, dividing the ray propagation type, determining a ray tracing method calculation formula of each divided type of ray, and performing the next step;
(3) rewriting a formula, namely rewriting a ray tracing method calculation formula of divided three types of ray propagation into a formula taking the moment t as an unknown quantity according to the moving speed of the receiving antenna ship in the ocean;
(4) generating a scattering area, determining the number and the positions of effective scattering points in the sea level, and performing the next step after determining the number and the positions;
(5) assigning the height change caused by the fluctuation of the sea waves into the height of the receiving end antenna according to the height change of the receiving end, and carrying out the next step;
(6) calculating parameters, namely calculating to obtain the length of a direct path, the sea level reflection times and the length of a reflection ray propagation path, recording the parameters as the parameters of the Kth reflection arrival path, and performing the next step;
(7) and (4) generating a channel, namely bringing the channel parameters of the arrival path subjected to statistics into a channel generation module to form a sea area line-of-sight channel.
2. The method according to claim 1, wherein the natural environment parameter comprises sea wave height.
3. The method as claimed in claim 2, wherein the operating system parameters include transmitting antenna height, receiving antenna height, transmitting and receiving antenna spacing and vessel moving speed.
4. The method as claimed in claim 3, wherein the ray tracing method for each type of ray has a formula:
Figure FDA0002367100110000011
wherein d isLOS,dRef,0And dRef,kRespectively representing the lengths of a direct path, a specular reflection path and a scattering path; k is the total number of scattering points;
Figure FDA0002367100110000012
is a phase shift caused by propagation delay corresponding to the length of each propagation path, f is the carrier frequency, c is the electromagnetic wave propagation speed; gamma is the reflection loss factor, amplitude and the sum factor of gamma
Figure FDA0002367100110000013
In direct proportion.
5. The method according to claim 4, wherein the effective scattering point position in step (4) is calculated by the following formula: c. CRef,k(t)=αrcosθu+rsinθu+cRef,0(t) where R is a value of u (0, R), θ is a value of u (0,2 π), α is a compression factor that controls the scattering region.
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Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN114244459A (en) * 2021-11-29 2022-03-25 西安电子科技大学 Method, system, medium, equipment and terminal for simulating wireless channel in marine environment

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CN104656078A (en) * 2013-11-25 2015-05-27 北京环境特性研究所 Sea surface ship method based on ray tracing
CN105388465A (en) * 2015-12-17 2016-03-09 西安电子科技大学 Sea clutter simulation method based on sea wave spectrum model
CN108540248A (en) * 2018-03-16 2018-09-14 西安电子科技大学 Maritime wireless communication dynamic multi-path channel model and method, wireless communication system
CN109408919A (en) * 2018-10-11 2019-03-01 南通先进通信技术研究院有限公司 A kind of sea area evaporation waveguide channel generation method
CN110208764A (en) * 2019-05-05 2019-09-06 南京航空航天大学 Dynamic sea large scene echo simulation method based on electromagnetism Scattering Calculation

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Publication number Priority date Publication date Assignee Title
CN104656078A (en) * 2013-11-25 2015-05-27 北京环境特性研究所 Sea surface ship method based on ray tracing
KR101504289B1 (en) * 2014-02-26 2015-03-30 연세대학교 산학협력단 Apparatus and method for generating underwater channel response
CN105388465A (en) * 2015-12-17 2016-03-09 西安电子科技大学 Sea clutter simulation method based on sea wave spectrum model
CN108540248A (en) * 2018-03-16 2018-09-14 西安电子科技大学 Maritime wireless communication dynamic multi-path channel model and method, wireless communication system
CN109408919A (en) * 2018-10-11 2019-03-01 南通先进通信技术研究院有限公司 A kind of sea area evaporation waveguide channel generation method
CN110208764A (en) * 2019-05-05 2019-09-06 南京航空航天大学 Dynamic sea large scene echo simulation method based on electromagnetism Scattering Calculation

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN114244459A (en) * 2021-11-29 2022-03-25 西安电子科技大学 Method, system, medium, equipment and terminal for simulating wireless channel in marine environment

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Application publication date: 20200515