JPH0766050B2 - Direction measurement method - Google Patents
Direction measurement methodInfo
- Publication number
- JPH0766050B2 JPH0766050B2 JP33838492A JP33838492A JPH0766050B2 JP H0766050 B2 JPH0766050 B2 JP H0766050B2 JP 33838492 A JP33838492 A JP 33838492A JP 33838492 A JP33838492 A JP 33838492A JP H0766050 B2 JPH0766050 B2 JP H0766050B2
- Authority
- JP
- Japan
- Prior art keywords
- hydrophone
- quadrant
- output
- azimuth
- bispectrum
- 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.)
- Expired - Lifetime
Links
- 238000000691 measurement method Methods 0.000 title 1
- 238000000034 method Methods 0.000 claims description 15
- 230000003595 spectral effect Effects 0.000 description 5
- 238000005259 measurement Methods 0.000 description 4
- 230000035945 sensitivity Effects 0.000 description 4
- 238000012935 Averaging Methods 0.000 description 3
- 238000010586 diagram Methods 0.000 description 3
- 238000001228 spectrum Methods 0.000 description 3
- 238000013459 approach Methods 0.000 description 2
- 101100221616 Halobacterium salinarum (strain ATCC 29341 / DSM 671 / R1) cosB gene Proteins 0.000 description 1
- 230000021615 conjugation Effects 0.000 description 1
- 230000000694 effects Effects 0.000 description 1
- 238000012545 processing Methods 0.000 description 1
- 230000002123 temporal effect Effects 0.000 description 1
Landscapes
- Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)
Description
【0001】[0001]
【産業上の利用分野】本発明は、方位測定方式に関し、
特に指向性ソノブイで受信した目標信号の到来方位を測
定する方位測定方式に関する。BACKGROUND OF THE INVENTION The present invention relates to a direction measuring system,
In particular, it relates to an azimuth measuring method for measuring the arrival azimuth of a target signal received by a directional sonobuoy.
【0002】[0002]
【従来の技術】目標信号の到来方位を測定するのに用い
る指向性ソノブイは、全方位にわたって一様な指向性を
有するOMNIハイドロホンと、南北方向に最大受信感
度の8の字形の指向性を有するNSハイドロホンと、東
西方向に最大感度の8の字形指向性を有するEWハイド
ロホンとを備え、これら各ハイドロホンの指向性は図2
に示すようになっている。2. Description of the Related Art Directional sonobuoys used to measure the arrival direction of a target signal have an OMNI hydrophone having a uniform directivity in all directions and an 8-shaped directivity having a maximum receiving sensitivity in the north-south direction. It has an NS hydrophone and an EW hydrophone that has a maximum sensitivity of 8 in the east-west direction. The directivity of each of these hydrophones is shown in FIG.
As shown in.
【0003】即ち、OMNIハイドロホンは図2(a)
に示す如く全方位に一様な指向性、いわゆるOMNI指
向性を有し、NSハイドロホンは図2(b)に示すよう
に南北方向に8の字型指向性の最大感度軸のいわゆるN
S指向性を有し、EWハイドロホンは図2(c)に示す
如く東西方向に8の字形指向性の最大感度軸のいわゆる
EW指向性を有する。That is, the OMNI hydrophone is shown in FIG.
As shown in FIG. 2, the NS hydrophone has a uniform directivity in all directions, so-called OMNI directivity. As shown in FIG. 2 (b), the NS hydrophone has a so-called N-shaped maximum sensitivity axis of the 8-shaped directivity in the north-south direction.
The EW hydrophone has the S directivity, and has the so-called EW directivity, which is the maximum sensitivity axis of the 8-shaped directivity in the east-west direction, as shown in FIG.
【0004】このような指向性を有する指向性ソノブイ
でパッシブ受信により捕捉しようとする目標は360°
の任意の方位に存在するが、図2では第1象限において
磁北Nから東Eに方位角B傾むいた角度方向に目標が存
在するものとして表現している。The target to be acquired by passive reception with a directional sonobuoy having such a directivity is 360 °.
2 exists in any azimuth, but in FIG. 2, the target exists in the angular direction in which the azimuth B is tilted from the magnetic north N to the east E in the first quadrant.
【0005】今、Aを目標信号の強度とし、NOM,
NNS,NEWをそれぞれOMNIハイドロホン,NSハイ
ドロホン及びEWハイドロホンで受信される水中雑音の
強度とするとOMNIハイドロホンの受信信号であるO
MNI受信信号ROMは(1)式で表され、NSハイドロ
ホンの受信信号であるNS受信信号RNSは(2)式で表
され、EWハイドロホンの受信信号であEW受信信号R
EWは(3)式で表される。Now, let A be the strength of the target signal, N OM ,
If N NS and N EW are the intensities of underwater noise received by the OMNI hydrophone, NS hydrophone and EW hydrophone, respectively, the received signal of the OMNI hydrophone is O.
The MNI reception signal R OM is represented by the equation (1), the NS reception signal R NS which is the reception signal of the NS hydrophone is represented by the equation (2), and the EW reception signal R which is the reception signal of the EW hydrophone.
EW is expressed by equation (3).
【0006】ROM=A+NOM …(1) RNS=AcosB+NNS…(2) REW=AsinB+NEW…(3) 指向性ソノブイにより受信された目標信号の到来方位を
測定する従来の方位測定方式は、例えば図3に示すよう
に、象限判定部1と方位決定部2とを備えて構成され
る。R OM = A + N OM (1) R NS = A cos B + N NS (2) R EW = A sin B + N EW (3) Conventional direction measuring method for measuring the arrival direction of the target signal received by the directional sonobuoy For example, as shown in FIG. 3, it is configured to include a quadrant determination unit 1 and an orientation determination unit 2.
【0007】象限判定部1では、指向性ソノブイからO
MNI受信信ROMと、NS受信信号RNSと、EW受信信
号REWとを受けてROMに対するRNS及びREWの位相判定
を行い、その判定結果を象限出力Qとして方位決定部2
に出力する。In the quadrant determination unit 1, the directivity sonobuoy is set to O.
Upon receiving the MNI received signal R OM , the NS received signal R NS, and the EW received signal R EW , the phase determination of R NS and R EW with respect to R OM is performed, and the determination result is used as the quadrant output Q to determine the azimuth determination unit 2
Output to.
【0008】象限出力Qは、次の4通りの位相関係にも
とづいて判定される。即ち、(1)RNS及びREWがROM
と同位相のときはQ=0°で第一象限、(2)RNSがR
OMと同位相のときはQ=90°で第二象限、(3)RNS
とREWがともにROMと逆位相のときはQ=180°で第
三象限、(4)RNSがROMと同位相でREWがROMと逆位
相のときはQ=270°で第4象限と、それぞれ各象限
の始まる角度を示し、象限を考慮しない見掛けの方位角
をいずれかの象限に加算・設定することによって目標信
号の到来方位角が決定する。The quadrant output Q is determined based on the following four phase relationships. That is, (1) R NS and R EW are R OM
When in phase with Q = 0 °, the first quadrant, (2) R NS is R
When in phase with OM , Q = 90 ° and second quadrant, (3) R NS
The third quadrant Q = 180 ° when the R EW are both R OM reverse phase, (4) when R NS is at R OM in phase R EW of R OM and opposite phase Q = 270 ° The arrival azimuth of the target signal is determined by adding and setting the fourth quadrant and the angles at which each quadrant starts, and adding and setting an apparent azimuth that does not take the quadrant into consideration.
【0009】方位決定部2は、象限出力Qと、OMNI
受信信号ROMとNS受信信号RNSと、EW受信信号REW
とに基づき、次の(4)式の演算を実行し、目標信号の
到来方位角BA を算出する。The azimuth determining section 2 outputs the quadrant output Q and OMNI.
Received signal R OM , NS received signal R NS , and EW received signal R EW
Based on the above, the following equation (4) is executed to calculate the arrival azimuth angle B A of the target signal.
【0010】 [0010]
【0011】(4)式のカッコ内の分子と分母の記号−
は、OMNI受信信号ROMにEW受信信号REW及びNS
受信信号RNSを乗じかけたものの時間平均値を表す。こ
れら分子及び分母の時間平均値はそれぞれ次の(5),
(6)式で示される。Symbols of numerator and denominator in parentheses in equation (4)
OMNI received signal R OM to EW received signal R EW and NS
It represents the time average value of the product of the received signal R NS . The time average values of these numerator and denominator are (5) and
It is shown by the equation (6).
【0012】 [0012]
【0013】 [0013]
【0014】(4)式及び(5)式の含む記号−も、そ
れぞれ時間平均値を表わす。The symbols − included in the equations (4) and (5) also represent time average values.
【0015】[0015]
【発明が解決しようとする課題】上述した従来の方位測
定方式において、式(1)、式(2)及び式(3)の含
む水中雑音NOM、NNS及びNEWが互いに無相関な場合
は、式(5)及び式(6)において平均時間を充分長く
とることにより、A・NEW,NOM・AsinB,NOM・
NEW,A・NNS,NOM・AcosB及びNOM・NNSの時
間平均値は、水中雑音NOM、NEW及びNNSの統計的平均
値が零であることから零に漸近する。In the above conventional azimuth measuring method, when the underwater noises N OM , N NS and N EW included in the equations (1), (2) and (3) are uncorrelated with each other. Is obtained by setting the averaging time in equations (5) and (6) to be sufficiently long, so that A · N EW , N OM · AsinB, N OM ·
The time averages of N EW , A · N NS , N OM · Acos B, and N OM · N NS are asymptotic to zero because the statistical mean of the underwater noises N OM , N EW, and N NS is zero.
【0016】従って、所定の平均時間、平均を施すこと
により式(4)は式(7)に近似でき、目標信号の到来
方位BA が算出される。Therefore, the equation (4) can be approximated to the equation (7) by averaging for a predetermined average time, and the arrival direction B A of the target signal is calculated.
【0017】 [0017]
【0018】一方、水中雑音NOMとNNS及びNEW間に海
象条件や海中生物等の発生起因を含む何等かの相関があ
る場合は、式(5)及び式(6)において平均時間を充
分長くとると、A・NEW,NOM・AsinB,A・NNS
及びNOM・sinBの時間平均値は前述と同じ理由によ
り零に漸近するが、NOM・NEW及びNOM・NNSの時間平
均値はそれぞれの相関度によって定まる値に漸近する。
この漸近到達値をそれぞれCEW及びCNSとするの式
(4)は次の式(8)によって表現することができる。On the other hand, if there is any correlation between the underwater noise N OM and N NS and N EW , including the occurrence of marine conditions and marine life, the average time in equations (5) and (6) is If taken long enough, A ・ N EW , N OM , AsinB, A ・ N NS
And the time average values of N OM · sinB are asymptotic to zero for the same reason as described above, but the time average values of N OM · N EW and N OM · N NS are asymptotic to the values determined by the respective degrees of correlation.
Expression (4) in which the asymptotic arrival values are C EW and C NS can be expressed by the following Expression (8).
【0019】 [0019]
【0020】式(8)より目標信号と到来方位角BA が
CEW及びCNSの時間平均値の影響により真の目標方位B
と異なってしまい、発生する誤差は平均時間の伸張では
改善できないという問題点があった。From the equation (8), the target signal and the arrival azimuth angle B A are the true target azimuth B due to the influence of the time average value of C EW and C NS.
However, there is a problem that the generated error cannot be improved by extending the average time.
【0021】本発明の目的は上述した問題点を解決し、
水中雑音NOMとNNS及びNEW間に何等かの相関がある場
合でも誤差の発生を著しく抑圧した方位測定方式を提供
することにある。The object of the present invention is to solve the above-mentioned problems,
An object of the present invention is to provide an azimuth measuring method in which the occurrence of error is significantly suppressed even when there is some correlation between the underwater noise N OM and N NS and N EW .
【0022】[0022]
【課題を解決するための手段】本発明の方式は、全方位
にわたって一様な指向性を有するOMNIハイドロホン
と、南北方向に8の字形の指向性を有するNSハイドロ
ホンと、東西方向に8の字形の指向性を有するEWハイ
ドロホンとを備えて目標の到来方向を知る指向性ソノブ
イの方位測定方式において、前記OMNIハイドロホ
ン,NSハイドロホンおよびEWハイドロホンによる受
信信号を受けてそれぞれの周波数成分を分析し、分析し
た周波数成分のうち位相の時間的変動の少ない2周波に
着目してそれぞれの受信信号のバイスペクトルを推定す
るバイスペクトル推定部と、前記バイスペクトル推定部
の出力にもとづいて前記指向性ソノブイに対する到来音
波の象限を判定し象限出力として送出する象限判定部
と、前記象限判定部の出力と前記バイスペクトル推定部
の出力とにもとづいて前記指向性ソノブイに対する到来
音波の方位を決定する方位決定部とを備えた構成を有す
る。According to the method of the present invention, an OMNI hydrophone having a uniform directivity in all directions, an NS hydrophone having a figure-eight directivity in the north-south direction, and an OMNI hydrophone in the east-west direction. In a directional sonobuy azimuth measuring method that includes an EW hydrophone having a V-shaped directivity and is capable of knowing the direction of arrival of a target, a frequency signal is received by the OMNI hydrophone, the NS hydrophone, and the EW hydrophone. On the basis of the outputs of the bispectrum estimation unit that analyzes the components and estimates the bispectrum of each received signal by paying attention to the two frequencies of the analyzed frequency components in which the phase has little temporal variation. A quadrant determining unit that determines the quadrant of an incoming sound wave for the directional sonobuoy and sends it out as a quadrant output; And it has a configuration in which a direction determination unit that determines the orientation of the incoming waves to said directional sonobuoy based on force and the output of the bispectral estimator.
【0023】また本発明の方式は、前記象限判定部で出
力する象限出力は、前記バイスペクトル推定部の出力す
る前記OMNIハイドロホンの受信信号のバイスペクト
ルに対する前記NSハイドロホンおよびEWハイドロホ
ンの受信信号のバイスペクトルの位相が同相であるかも
しくは逆相であるかの状態の組合せにもとづいて判定す
るものとした構成を有する。According to the method of the present invention, the quadrant output output from the quadrant determination unit is the reception of the NS hydrophone and the EW hydrophone with respect to the bispectrum of the reception signal of the OMNI hydrophone output from the bispectrum estimation unit. The configuration is such that the determination is made based on a combination of states in which the phases of the bispectrum of the signals are in-phase or opposite-phase.
【0024】また、本発明の方式は前記方位決定部にお
ける到来音波の方位決定は、前記象限判定部の象限出力
によって指定される象限に、前記バイスペクトル推定部
の出力する前記NSハイドロホンと前記EWハイドロホ
ンによる受信信号のバイスペクトル出力の比にもとづい
て決定する到来音波の象限内方位角を設定するものとし
た構成を有する。Further, according to the method of the present invention, the azimuth determination of the incoming sound wave in the azimuth determining unit is performed in the quadrant designated by the quadrant output of the quadrant determining unit, with the NS hydrophone output from the bispectrum estimating unit and the quadrant. The azimuth angle in the quadrant of the incoming sound wave is determined based on the ratio of the bispectral output of the received signal by the EW hydrophone.
【0025】[0025]
【作用】一般に、水中雑音はガウス性を有し、複数の異
る周波数成分間には相関がない。In general, underwater noise is Gaussian and there is no correlation between different frequency components.
【0026】これに対し、目標の発する信号は、基本波
と高調波間や、複数の周波数成分間の干渉で生ずる周波
数成分など、複数の周波数成分間に相関性を有すること
が多い。On the other hand, the signal emitted by the target often has a correlation between a plurality of frequency components, such as a frequency component caused by interference between the fundamental wave and a harmonic or between a plurality of frequency components.
【0027】本発明の構成要素であるバイスペクトル推
定部で推定するバイスペクトルは、上述した複数の周波
数成分間の相関性を表現するものであり、目標信号を周
波数分析し、位相がほぼ一定している2つの周波数のス
ペクトル強度及び2つの周波数の和の共役スペクトル強
度の積とバイスペクトルの雑音とを含む値として表現さ
れ、ガウス性を有する水中雑音では統計的に零となり、
前述したような相関性を有する目標信号では一定値とな
る性質がある。The bispectrum estimated by the bispectrum estimator, which is a component of the present invention, expresses the correlation between a plurality of frequency components described above, and the target signal is frequency-analyzed to have a substantially constant phase. It is expressed as a value including the product of the spectral intensity of the two frequencies and the conjugate spectral intensity of the sum of the two frequencies and the bispectral noise, and is statistically zero for the underwater noise having Gaussianity,
The target signal having the above-described correlation has a property of having a constant value.
【0028】本発明ではかかるバイスペクトルの性質を
利用し、水中雑音NOM、NNSおよびNEWを目標信号に比
して低減し、水中雑音相互間の相関の影響を抑圧して、
この影響のもたらす方位誤差を低減する。In the present invention, by utilizing the property of the bispectrum, the underwater noises N OM , N NS and N EW are reduced as compared with the target signal, and the influence of the correlation between the underwater noises is suppressed,
The azimuth error caused by this influence is reduced.
【0029】[0029]
【実施例】次に、本発明について図面を参照して説明す
る。DESCRIPTION OF THE PREFERRED EMBODIMENTS Next, the present invention will be described with reference to the drawings.
【0030】図1は、本発明の一実施例の構成を示すブ
ロック図であり、図3に示す従来例の象限判定部1と方
位決定部2のほか、本発明に直接かかわるバイスペクト
ル推定部3を備えた構成を有する。FIG. 1 is a block diagram showing the configuration of an embodiment of the present invention. In addition to the conventional quadrant judging unit 1 and azimuth determining unit 2 shown in FIG. 3, a bispectral estimating unit directly related to the present invention is provided. 3 is provided.
【0031】バイスペクトル推定部3に入力されるOM
NI受信信号ROM、NS受信信号RNS及びEW受信信号
REWはそれぞれ式(1),式(2),式(3)で表現さ
れる。OM input to the bispectrum estimation unit 3
The NI reception signal R OM , the NS reception signal R NS, and the EW reception signal R EW are expressed by equations (1), (2), and (3), respectively.
【0032】バイスペクトル推定部1は、これらの受信
信号にもとづいて、OMNI受信信号のバイスペクトル
BOM、NS受信信号のバイスペクトルBNS及びEW受信
信号のバイスペクトルBEWを算出する。これらバイスペ
クトルBOM,及びBEWは、それぞれ式(9),式(1
0)及び式(11)で表現される。The bispectral estimator 1, based on these received signals, calculates the bispectral B EW bispectral B OM, the NS received signal by spectrum B NS and EW received signals OMNI received signal. These bispectrums B OM and B EW are respectively expressed by equation (9) and equation (1
0) and equation (11).
【0033】バイスペクトル推定部3は、入力したOM
NI受信信号ROM、NS受信信号RNS及びEW受信信号
REWにそれぞれフーリェ変換処理を施し、周波数領域デ
ータに変換し、これら周波数領域データの含む周波数成
分のうち位相変動が少なく、かつS/Nが比較的良好な
ものに着目して選択する2周波f1 とf2 、およびこれ
ら2つの周波数の和f1 +f2 の3周波数成分のスペク
トル及び雑音にもとづいてOMNI受信信号のバイスペ
クトルBOM、NS受信信号のバイスペクトルBNS及びE
W受信信号のバイスペクトルBEWをそれぞれ次の式
(9),式(10)および式(11)の如く推定する。The bispectrum estimation unit 3 receives the input OM.
The NI reception signal R OM , the NS reception signal R NS, and the EW reception signal R EW are each subjected to Fourier transform processing to be converted into frequency domain data, and the phase variation is small among the frequency components included in these frequency domain data, and S / The bispectrum B of the OMNI received signal is based on the two frequencies f 1 and f 2 which are selected by focusing on the one having a relatively good N, and the spectrum and noise of the three frequency components of the sum f 1 + f 2 of these two frequencies. OM , NS bi-spectral of received signal B NS and E
The bispectrum B EW of the W received signal is estimated as in the following equations (9), (10) and (11).
【0034】 BOM=X(f1 )・X(f2 )・X* (f1 +f2 )+NBOM …(9) BNS=X(f1 )・X(f2 )・X* (f1 +f2 )cos3 B+NBNS …(10) BEW=X(f1 )・X(f2 )・X* (f1 +f2 )sin3 B+NBEW …(11) 式(9),(10)及び(11)において、X(f1
)、X(f2 )及びX(f1 +f2 )はそれぞれ、目
標信号強度Aの周波数f1 、f2 及びf1 +f2 におけ
るスペクトル強度を表わし、また記号*は共役を示す。
また、NBOM 、NBNS 及びNBEW はそれぞれ雑音成分を
示す。B OM = X (f 1 ) × X (f 2 ) × X (f 1 + f 2 ) + N BOM (9) B NS = X (f 1 ) × X (f 2 ) × X ( f 1 + f 2 ) cos 3 B + N BNS (10) B EW = X (f 1 ) · X (f 2 ) · X * (f 1 + f 2 ) sin 3 B + N BEW (11) Formulas (9) and (9) In 10) and (11), X (f1
), X (f2) and X (f1 + f2) represent the spectral intensities of the target signal intensity A at frequencies f1, f2 and f1 + f2, respectively, and the symbol * indicates conjugation.
Further, N BOM , N BNS and N BEW each represent a noise component.
【0035】つまり、バイスペクトルは、目標が発する
と推定される2周波、並びにこの2周波の和の周波数の
スペクトル強度及び共役スペクトル強度と、これら周波
数成分に関する雑音とによって表現される。また、バイ
スペクトルレベルの雑音NBOM 、NBNS 及びNBEW はそ
れぞれ式(12)、式(13)及び式(14)により表
わされる。 NBOM =X(f1 )X* (f1 +f2 )NOM(f2 ) +X(f2 )X* (f1 +f2 )NOM(f1 ) +X* (f1 +f2 )NOM(f1 )NOM(f2 ) +X(f1 )X(f2 )NOM * (f1 +f2 ) +X(f1 )NOM(f2 )NOM * (f1 +f2 ) +X(f2 )NOM(f1 )NOM * (f1 +f2 ) +NOM(f1 )NOM(f2 )NOM * (f1 +f2 )…(12) NBNS =(X(f1 )X* (f1 +f2 )NNS(f2 ) +X(f2 )X* (f1 +f2 )NNS(f1 ) +X(f1 )X(f2 )N* NS(f1 +f2 ))cos2 B +(X* (f1 +f2 )NNS(f1 )NNS(f2 ) +X(f1 )NNS(f2 )N* NS(f1 +f2 ) +X(f2 )NNS(f1 )N* NS(f1 +f2 ))cosB +NNS(f1 )NNS(f2 )N* NS (f1 +f2 )…(13) NBEU =(X(f1 )X* (f1 +f2 )NEW(f2 ) +X(f2 )X* (f1 +f2 )NEW(f1 ) +X(f1 )X(f2 )N* EW (f1 +f2 ))sin2 B +(X*(f1 +f2 )NEW(f1 )NEW(f2 ) +X(f1 )NEW(f2 )N* (f1 +f2 ) +X(f2 )NEW(f1 )N* (f1 +f2 ))sinB +NEW(f1 )NEW(f2 )N* EW (f1 +f2 )…(14) ここで、NOM(f)、NNS(f)及びNEW(f)はそれ
ぞれOMNI受信信号ROM、NS受信RNS及びEW受信
信号REWに含まれる水中雑音NOM、NNS及びNEWの周波
数fにおけるスペクトル強度である。That is, the bispectrum is represented by the two frequencies estimated to be emitted by the target, the spectral intensities and conjugate spectral intensities of the frequency of the sum of these two frequencies, and the noise related to these frequency components. Further, the bispectral level noises N BOM , N BNS, and N BEW are expressed by equations (12), (13), and (14), respectively. N BOM = X (f 1) X * (f 1 + f 2) N OM (f 2) + X (f 2) X * (f 1 + f 2) N OM (f 1) + X * (f 1 + f 2) N OM (f 1 ) N OM (f 2 ) + X (f 1 ) X (f 2 ) N OM * (f 1 + f 2 ) + X (f 1 ) N OM (f 2 ) N OM * (f 1 + f 2 ) + X (f 2 ) N OM (f 1 ) N OM * (f 1 + f 2 ) + N OM (f 1 ) N OM (f 2 ) N OM * (f 1 + f 2 ) ... (12) NBNS = (X (F 1 ) X * (f 1 + f 2 ) N NS (f 2 ) + X (f 2 ) X * (f 1 + f 2 ) N NS (f 1 ) + X (f 1 ) X (f 2 ) N * NS (f 1 + f 2 )) cos 2 B + (X * (f 1 + f 2 ) N NS (f 1 ) N NS (f 2 ) + X (f 1 ) N NS (f 2 ) N * NS (f 1 + f 2 ) + X (f 2 ) N NS (f 1 ) N * NS (f 1 + f 2 )) cosB + N NS (f 1 ) N NS (f 2 ) N * NS (f 1 + f 2 ) ... (13) N BEU = (X (f 1 ) X * (f 1 + f 2 ) N EW (f 2 ) + X (f 2 ) X * (f 1 + f 2 ) N EW (f 1 ) + X (F 1 ) X (f 2 ) N * EW (f 1 + f 2 )) sin 2 B + (X * (f 1 + f 2 ) N EW (f 1 ) N EW (f 2 ) + X (f 1 ) N EW (f 2 ) N * (f 1 + f 2 ) + X (f 2 ) N EW (f 1 ) N * (f 1 + f 2 )) sinB + N EW (f 1 ) N EW (f 2 ) N * EW ( f 1 + f 2 ) ... (14) Here, N OM (f), N NS (f) and N EW (f) are included in the OMNI received signal R OM , NS received R NS and EW received signal R EW , respectively. It is the spectrum intensity at frequency f of underwater noise N OM , N NS and N EW .
【0036】象限判定部1は、バイスペクトル推定部3
からOMNI受信信号、NS受信信号及びEW受信信号
のバイスペクトルBOM、BNS及びBEWを受け、OMNI
受信信号のバイスペクトルBOMに対するBNS、BEWの位
相が同相か逆相かの判定にもとづく象限判定を行い、そ
の判定結果を象限出力Qとして方位決定部2に出力す
る。The quadrant judging unit 1 is a bispectral estimating unit 3
From the OMNI received signal, NS received signal and EW received signal bispectrum B OM , B NS and B EW ,
The quadrant determination is performed based on the determination whether the phases of B NS and B EW with respect to the bispectrum B OM of the received signal are in-phase or anti-phase, and the determination result is output to the azimuth determination unit 2 as a quadrant output Q.
【0037】象限出力Qの出力内容は次の4通りであ
る。即ち(1)BNS及びBEWがBOMと同意相のときはQ
=0°で第1象限、(2)BNSがBOMと逆位相でBEWが
BOMと同位相のときはQ=90°で第2象限、(3)B
NSとBEWがともにBOMと逆位相のときはQ=180°で
第3象限、(4)BNSがBOMと同位相でBEWがBOMと逆
位相のときはQ=270°で第4象限をそれぞれ指定す
る。The quadrant output Q has the following four output contents. (1) When B NS and B EW are in agreement with B OM , Q
= 0 first quadrant °, (2) B NS second quadrant in the Q = 90 ° when B EW in B OM and opposite phase of the B OM in phase, (3) B
Q = 180 ° when NS and B EW both have opposite phases to B OM, and (4) Q = 270 ° when B NS has the same phase as B OM and B EW has opposite phases to B OM . Specify each of the 4th quadrants with.
【0038】方位決定部2では、象限出力Qと、NS受
信信号のバイスペクトルBNSと、EW受信信号のバイス
ペクトルBEWに基づき、式(15)の演算を実行し目標
信号の到来方位をBAを算出する。The azimuth determining unit 2 executes the calculation of the equation (15) based on the quadrant output Q, the bispectrum B NS of the NS received signal, and the bispectrum B EW of the EW received signal to determine the arrival direction of the target signal. Calculate BA.
【0039】 [0039]
【0040】ここで記号−は、EW及びNS受信信号の
バイスペクトルの時間平均値を示す。Here, the symbol-indicates the time average value of the bispectrum of the EW and NS received signals.
【0041】ところで、目標が周波数f1 とf2 の信号
を発生しており、この2信号が干渉して和の周波数f1
+f2 が発生している場合や、さらにはf1 とf2 が等
しい場合の高調波成分の場合には、f1 、f2 及びf1
+f2 の3つの各周波数成分間にはほぼ一定の位相関係
があり、従って式(9)、(10)及び(11)のX
(f1 )・X(f2 )・X* (f1 +f2 )の時間平均
値は、平均時間の伸長とともに一定値に漸近する。By the way, the target generates signals of frequencies f 1 and f 2 , and these two signals interfere with each other to generate the sum frequency f 1
When + f 2 is generated, or when the harmonic components are when f 1 and f 2 are equal, f 1 , f 2 and f 1
There is a substantially constant phase relationship between the three frequency components + f 2 and, therefore, X in equations (9), (10) and (11)
The time average value of (f 1 ) · X (f 2 ) · X * (f 1 + f 2 ) gradually approaches a constant value as the average time lengthens.
【0042】また、水中雑音は一般にガウス性を有して
おり、異なる周波数における雑音成分は相関を持たない
ことから式(12)、(13)及び(14)で示される
雑音の平均時間は平均時間の伸長とともに零に漸近す
る。従って、所定の時間、平均を行うことにより式(1
5)、式(16)に近似でき、目標信号の到来方位が算
出される。Further, underwater noise generally has Gaussianity, and noise components at different frequencies have no correlation. Therefore, the average time of noise represented by the equations (12), (13) and (14) is average. It asymptotically approaches zero with the extension of time. Therefore, by averaging for a predetermined time, the formula (1
5) can be approximated to the equation (16), and the arrival direction of the target signal is calculated.
【0043】 [0043]
【0044】こうして、バイスペクトルによる目標方位
測定においては、水中雑音NOM、NNS及びNEW間の相関
性の有無に関係なく測定結果に影響を与えないですむ。In this way, in the measurement of the target azimuth by the bispectrum, the measurement result is not affected regardless of the correlation between the underwater noises N OM , N NS and N EW .
【0045】[0045]
【発明の効果】以上説明したように本発明は、目標信号
の到来方向の算出にバイスペクトルを利用することによ
り、海中雑音が方位測定に与える影響を著しく抑圧し、
方位測定誤差を著しく小さくすることができるという効
果がある。As described above, the present invention remarkably suppresses the influence of underwater noise on the azimuth measurement by utilizing the bispectrum for calculating the arrival direction of the target signal.
This has the effect of significantly reducing the azimuth measurement error.
【図面の簡単な説明】[Brief description of drawings]
【図1】本発明の一実施例の方位測定方式の構成を示す
ブロック図である。FIG. 1 is a block diagram showing a configuration of an azimuth measuring method according to an embodiment of the present invention.
【図2】指向性ソノブイのOMNI指向性(a)、NS
指向性(b)およびEW指向性を示す図である。FIG. 2 Directional Sonobui OMNI directivity (a), NS
It is a figure which shows directivity (b) and EW directivity.
【図3】従来の方位測定方式の構成を示すブロック図で
ある。FIG. 3 is a block diagram showing a configuration of a conventional azimuth measuring method.
1 象限判定部 2 方位決定部 3 バイスペクトル推定部 1 quadrant determination unit 2 azimuth determination unit 3 bispectral estimation unit
Claims (3)
OMNIハイドロホンと、南北方向に8の字形の指向性
を有するNSハイドロホンと、東西方向に8の字形の指
向性を有するEWハイドロホンとを備えて目標の到来方
向を知る指向性ソノブイの方位測定方式において、前記
OMNIハイドロホン,NSハイドロホンおよびEWハ
イドロホンによる受信信号を受けてそれぞれの周波数成
分を分析し、分析した周波数成分のうち位相の時間的変
動の少ない2周波に着目してそれぞれの受信信号のバイ
スペクトルを推定するバイスペクトル推定部と、前記バ
イスペクトル推定部の出力にもとづいて前記指向性ソノ
ブイに対する到来音波の象限を判定し象限出力として送
出する象限判定部と、前記象限判定部の出力と前記バイ
スペクトル推定部の出力とにもとづいて前記指向性ソノ
ブイに対する到来音波の方位を決定する方位決定部とを
備えることを特徴とする方位測定方式。1. An OMNI hydrophone having a uniform directivity in all directions, an NS hydrophone having an 8-shaped directivity in the north-south direction, and an EW hydrophone having an 8-shaped directivity in the east-west direction. In the directional sonobuy direction measuring method for determining the direction of arrival of a target, the respective frequency components are analyzed by receiving the reception signals from the OMNI hydrophone, NS hydrophone and EW hydrophone, and the analyzed frequency components Of these, a bispectrum estimation unit that estimates the bispectrum of each received signal by focusing on two frequencies whose phase fluctuations are small, and a quadrant of an incoming sound wave for the directional sonobuoy based on the output of the bispectrum estimation unit. A quadrant determining unit for determining and transmitting as a quadrant output, an output of the quadrant determining unit and a bispectral estimating unit. An azimuth measuring method, comprising: an azimuth determining unit that determines the azimuth of an incoming sound wave with respect to the directional sonobuoy based on the output.
前記バイスペクトル推定部の出力する前記OMNIハイ
ドロホンの受信信号のバイスペクトルに対する前記NS
ハイドロホンおよびEWハイドロホンの受信信号のバイ
スペクトルの位相が同相であるかもしくは逆相であるか
の状態の組合せにもとづいて判定することを特徴とする
請求項1記載の方位測定方式。2. The quadrant output output by the quadrant determining section is:
The NS for the bispectrum of the received signal of the OMNI hydrophone output by the bispectrum estimation unit
The azimuth measuring method according to claim 1, wherein the determination is made based on a combination of states in which the phases of the bispectrum of the reception signals of the hydrophone and the EW hydrophone are in-phase or in-phase.
決定は、前記象限判定部の象限出力によって指定される
象限に、前記バイスペクトル推定部の出力する前記NS
ハイドロホンと前記EWハイドロホンによる受信信号の
バイスペクトル出力の比にもとづいて決定する到来音波
の象限内方位角を設定することによって行なうことを特
徴とする請求項1記載の方位測定方式。3. The azimuth determination of the incoming sound wave in the azimuth determination unit is performed by the NS output from the bispectral estimation unit in a quadrant designated by the quadrant output of the quadrant determination unit.
The azimuth measuring method according to claim 1, wherein the azimuth measuring method is performed by setting an in-quadrant azimuth angle of an incoming sound wave determined based on a ratio of a bispectral output of a reception signal by the hydrophone and the EW hydrophone.
Priority Applications (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP33838492A JPH0766050B2 (en) | 1992-12-18 | 1992-12-18 | Direction measurement method |
Applications Claiming Priority (1)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| JP33838492A JPH0766050B2 (en) | 1992-12-18 | 1992-12-18 | Direction measurement method |
Publications (2)
| Publication Number | Publication Date |
|---|---|
| JPH06201811A JPH06201811A (en) | 1994-07-22 |
| JPH0766050B2 true JPH0766050B2 (en) | 1995-07-19 |
Family
ID=18317651
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| JP33838492A Expired - Lifetime JPH0766050B2 (en) | 1992-12-18 | 1992-12-18 | Direction measurement method |
Country Status (1)
| Country | Link |
|---|---|
| JP (1) | JPH0766050B2 (en) |
Families Citing this family (3)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| JP2852196B2 (en) * | 1995-02-16 | 1999-01-27 | 防衛庁技術研究本部長 | Underwater acoustic signal direction calculator |
| JP4011395B2 (en) * | 2002-05-10 | 2007-11-21 | 株式会社ケンウッド | Microphone device and sound source direction determination device |
| JP6862799B2 (en) * | 2016-11-30 | 2021-04-21 | 日本電気株式会社 | Signal processing device, directional calculation method and directional calculation program |
-
1992
- 1992-12-18 JP JP33838492A patent/JPH0766050B2/en not_active Expired - Lifetime
Also Published As
| Publication number | Publication date |
|---|---|
| JPH06201811A (en) | 1994-07-22 |
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