Correlation Based Novel Detection Scheme for HF

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Index Terms— Radar detection, high frequency radar, radar clutter.
I. INTRODUCTION
High Frequency Surface Wave Radar (HF SWR) exploits low frequency (3-30 MHz) signals’ ability to propagate well beyond the visible horizon due to the diffraction of the vertically polarized HF wave over conducting sea water. Long range marine surveillance is gaining more importance after the United Nations Convention on the Law of the Sea establishing 200 nautical miles as the Exclusive Economic Zone (EEZ).Hence a HF SWR system is an attractive option for cost effective EEZ surveillance and rescue operations as compared to airborne and space-based techniques.
S(k,α) = F(k)G(α)
(3)
where, F(k) is the non-directional spectra density term. G(Į) is the directional spread of the sea wave energy and is modelled as
G(ș) = A cos2S ¨§ α − șw ¸·
Understanding of the physics of sea clutter can pave way of devising an effective way to optimize the detection algorithm. In the proposed detection scheme, it is assumed that the received second order clutter power along all the azimuth cells over neighboring Doppler cells will not be random but will be correlated. In presence of a target signal this correlation will cease to exist. The assumption has been proven analytically in Section 2 by using the wave height direction model. Oceanographers have been using the wave height directional spectra for extracting the wave parameters like wave height and wave velocity from the HF SWR backscatter [2][4]. Section 3 of the paper will propose the novel detection scheme,
(4)
©2¹
where șw is the direction of propagation of the wind and the parameter S depends on the absolute wind speed and radar operating frequency (for details refer [2]). Two Doppler cells
(7)

Ș = ³ I (k,k´,Ȧ)dk
(8)
−∞
I (k,k´,Ȧ) = A2 Γ2 k F(k) F(k´ ) ∂( ω − m gk − m' gk´ ) (9)
mω1 = mω2 = m &
m' ω1
=
m' ω2
= m'
(5)
Using (3) (4) and (5), (2) is transformed as
ϕ ȥ

σ 2 (ω,ϕ) = Ș ³ h(ϕ,ș) dș
(6)
0
where,
h(ϕ,θ ) = G(θ +ϕ + mπ ) G(θ + ϕ + m'π )
The nature of backscattered signal of HF radar is significantly different from that of typical microwave radar. The major challenge in HF SWR is to detect a target echo within the strong sea backscatter (sea clutter). At HF band the sea clutter dominates the pure receiver noise and the clutter has a characteristic behaviour. Dzvonkovskaya [1] has done significant work in developing constant false-alarm-rate (CFAR) detection procedure in which for each azimuth cell the adaptive threshold is chosen as the maximum of the upper confidence bound value for the power regression curve along range and Doppler cells. It is assumed that the clutter power is randomly distributed along the azimuth cells over various Doppction scheme will be evaluated for a given Chebyshev beamformer and different Signal to Clutter Ratio (SCR), wind speeds and wind directions.
Abstract— The challenge in HF Surface Wave Radar (SWR) lies in the detection of a target signal in the background of a strong sea clutter. A novel detection scheme is proposed which assumes that for a given Range Doppler (RD) cell in absence of a target, the normalized second order sea clutter power along the azimuth cells will be correlated over neighboring Doppler cells. This assumption is proven analytically by using the well established unimodal wave directional spectra. A target within the second order sea clutter can be detected with the price of higher computation cost.
incoherent sum of hydrodynamic and electromagnetic terms and k, k´ Ł wave numbers of the two scattering ocean waves. S(k,ș) Ł directional ocean wave spectrum for wave number k and direction ș. k0 Ł radar wave number and g Ł acceleration due to gravity. The values of m and m´ in (2) define the four possible combinations of directions of the two scattering waves and also the four sidebands that surround the first order peaks (for details refer [3]). HF radar has been using a singlelobe model for the wave directional spread, to estimate wind directions [3]. This technique assumes the spectral density of sea surface gravity waves to be of the form
π
³ ı~2 (Ȧ,ȥ)
=
1 ʌ
2
D (ȥ
−π
−ϕ)
ı2 (Ȧ,ϕ)

(1)
2
2π ∞
σ2(ω,ϕ) = k04 ¦ ³ ³ ī2 S(k,ș +ϕ + mπ)