CN102955152A

Synthetic aperture radar (SAR) signal simulation method for sea waves

Abstract

The invention discloses a synthetic aperture radar (SAR) signal simulation method for sea waves. The SAR signal simulation method comprises the following steps of: S1, modeling the sea waves by adopting a sea wave spectrum, and constructing a three-dimensional sea surface comprising a plurality of surface elements; S2, calculating a scattering field of each surface element, then converting a motion effect of each surface element along the distance direction into excursion along the orientation direction according to a speed beaming model, and generating a sea surface scattering graph according to the scattering fields and the excursion in the orientation direction; and S3, simulating an SAR signal of the sea surface scattering graph for overall motion to obtain an analog SAR signal, and processing the analog SAR signal by an SAR imaging algorithm to obtain the analog SAR image. By the SAR signal simulation method for the sea waves, a Doppler effect caused by sea surface motion is considered, so that SAR signal simulation of the sea waves can be realized under the condition of strong storm, and comprehensive analog data can be supplied to design of an SAR system.

CN102955152A, drawing sheet 1
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8 claims: 5 independent, 3 dependent

  1. 1
    A the SAR signal imitation method of sea wave, a characterised, comprising the following steps:Si: For ocean wave spectrum to the sea wave perform, type structure comprises the multiple of unit area three-dimensional sea surface, 52: Computing each unit area of the scattered field, and according to the speed bunching model collected by the unit area of the distance of a cell the position to the reflecting, and according to the scattered field and reflecting generate sea scattering diagram of a slot;53: To the sea scattering diagram perform mass of the SAR signal imitation obtained SAR analogue signal, and the SAR image algorithm to the analogue signal SAR perform processing obtained simulating SAR image. 1. 一种海浪的SAR信号模拟方法,其特征在于,包括以下步骤: S1:采用海浪谱对海浪进行建模,构造包含多个面元的三维海表面; 52 :计算每个所述面元的散射场,然后根据速度聚束模型将所述面元沿距离向的运动 效应转化为方位向的偏移,并根据所述散射场和所述方位向的偏移生成海面散射图; 53 :对所述海面散射图进行整体运动的SAR信号模拟得到模拟SAR信号,并采用SAR成 像算法对所述模拟SAR信号进行处理得到模拟SAR图像。
  2. 2
    According to the SAR signal imitation method of sea wave claim) that and is characterised, wherein a step SI, wherein sea wave spectrum is a to form accumulate:(W-SHAPED K) is the S K (P) (Θ, K) is W-SHAPED, (K) is a sea wave, spectrum S (K) is a one-dimensional spectrum;the long wave area, (S) CAPABLE of the classical, spectrumThe shortwave, (S) UPON blocking gravity Sgc holder (4 )and S holder. (4 ), And a different wave;the number Ρ (θ, κ) is arranged;function The K is sea wave vector, a K module K is 2 or Λ is a sea wave number, A the sea wave wavelength;Θ and direct type: connecting (Kx=Kco^O (Κ is Κύηθ, Kx is a sea wave vector K the X direction part, Ky is a sea wave vector K of the y direction device. 2. 根据权利要求1所述的海浪的SAR信号模拟方法,其特征在于,所述步骤S1中,所述 海浪谱表示为积的形式: W(K) = S (K) P ( θ , Κ) 其中,W(K)为海浪谱; S(K)是一维谱,在长波区域,S(K)采用经典谱;在短波区域,S(K)分为重力毛细波 Sgc(K)和毛细波Sc(K),分别对应不同的波数; Ρ(Ο,Κ)是扩展函数; κ是海浪波矢,Κ的模Κ = 2π/Α是海浪波数,A是海浪波长; θ通过下式定义: K=Kcos8 < Ky=KsinO 其中,K’是海浪波矢K在X方向的分量,%是海浪波矢K在y方向的分量。
  3. 4
    According to the SAR signal imitation method of sea wave claim) that and is characterised, wherein a step SI, a criteria two sea surface model constructions to the three-dimensional sea surface; the specifcially is:The long wave communication circuit criterion's outline, wherein the SAR resolution ratio unit is thinner, and is greater than electromagnetic wave the plane of unit area is similar, generating random sea surface;Shortwave the small criterion's any is rough, and gravity holder or ripple's wave form approximate;The gravity holder or ripple's wave form lines;the plane of unit area with sea surface model. 4. 根据权利要求1所述的海浪的SAR信号模拟方法,其特征在于,所述步骤S1中,采用 二尺度的海洋表面模型构造所述三维海表面,具体为:长波对应大尺度的轮廓,通过比SAR 分辨率单元小且远大于电磁波长的平面面元近似,生成随机海面;短波对应小尺度的随机 粗糙,通过重力毛细波或毛细波的波形近似;所述重力毛细波或毛细波的波形叠加在所述 平面面元上形成海表面模型。
  4. 6
    According to the SAR signal imitation method of sea wave claim) that and is characterised, wherein a step S2, each unit area of the scattered field is a direct type:a, A £;Is the incidence field, type fully and scattered field, IT is a unit of the central point distance flying of;the k=Ikl =2 π/λ is electromagnetic wave number, k is the incidence electromagnetic wave vector, λ is an wavelength;Subscript H and V respectively arranged behalf of horizontal and vertical polarization part;Superscript) and s is incident field and dispersion-type field;The X-RAY matrix is backscattering coefficient, j is the baseboard. 6. 根据权利要求1所述的海浪的SAR信号模拟方法,其特征在于,所述步骤S2中,每个 所述面元的散射场采用下式计算: esh K Ε'η Ε; 其中,碼和Ε;是入射场,碼和是散射场,R是面元中心点到飞行航线之间的距离;k =kl =2π/λ是电磁波数,k是入射电磁波矢,λ是电磁波长;下标Η和V分别代表水 平和垂直极化部分;上标i和s分别表示入射场和散射场;矩阵X表示后向散射系数,j为 虚数单位。 7.根据权利要求6所述的海浪的SAR信号模拟方法,其特征在于,所述矩阵χ由下式 给出: X = FD( θ ί,δ χ, δ y) 其中,兀是雷达入射角,X和X是面元沿着方位向χ和地距方向y的面元斜率; 矩阵F表示雷达后向散射由于面元方向和电磁参量依赖引起的极化效应; 标量D表示为: D(°i,δχ» 8 y) = f Aexp(j2k · ρ ) dA 其中,k是入射电磁波矢,A是面元投影到(x,y)平面的面元面积,而P为从面元中心 点到面元上任一点的径向矢量; p = (x-x0)x + (y-y0)y + (z(x,y)-z0)z 其中,(χ。,y(), ζ。)是面元的中心坐标,步,2分别为χ, y, ζ方向的单位矢量。 z(x,y) = ζ0+ δ x (x-x0) + δ y (y-y0) +zs (x, y),其中,6 % 和 6 y 是面元沿着方位向 x 和地 距方向y的面元斜率;z,x, y)是符合短波谱的随机过程。 &根据权利要求1所述的海浪的SAR信号模拟方法,其特征在于,所述步骤S2中,根据 速度聚束模型将所述面元沿距离向的运动效应转化为方位向的偏移具体为: 散射面元根据距离向的速度分量进行方位向的调整: 其中,R是传感器到所述散射面元的距离,V是传感器速度; 根据海面面元的运动速度,方位向坐标为χ的散射面元将会映射到 而散射面元沿电磁波传播方向的速度为: V (〃) = Σ (Q 同)cos (Q) sin (Kw -劲 + 5) 其中,ω是海浪频率,W,K)是长波谱,K是海浪波矢;/(0,仇)=Jl + tanpsin^ , δ =tanptan 0 [Sin 0 ο),兀是雷达入射角,0()是飞行方向与海浪波矢K在海表面方向的夹 角;r代表海浪在水平方向的位置,其包含χ和y两个方向上的位置信息。
  5. 8
    According to the SAR signal imitation method of sea wave claim) that and is characterised, wherein a step S2, collected by the unit of the surface and a speed bunching model along the movement a cell of the slot is a reflecting specifcially with a slot is:The head inclination adjusting according to the scattering of unit area close to the device of a perform position of range: , IT is the sensor is provided with a scattering unit area of the distance;the processor is a speed sensor;According to the speed of movement of sea of unit area;the position and map to the plate of unit area is χ's scattering of unit area of the axes of the electromagnetic wave propagation direction speed is: , ω is a sea wave frequency, Wl (K) is a long spectrum, a K is a sea wave vector small is + tan2 Asin2A, δ =tan-1 (tan the Θ iSin θ 0), 01 of the radar incidence angle, Θ is a black direction and current emitting test vector K of the sea surface of the included angle;composed of behalf of the sea wave the horizontal direction, comprising χ and position information and y two direction.