2004
DOI: 10.1109/joe.2004.834175
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Measuring Surface Wind Direction by Monostatic HF Ground-Wave Radar at the Eastern China Sea

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Cited by 42 publications
(31 citation statements)
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“…The β parameter obtained from the ACMB algorithms is different from the LSMB algorithm, which may be one reason for the results of the ACMB and LSMB are different obviously. The RMSE of 24.8° is low compared the results given by [6,10,11] and close the mean difference 20° by Huang et al [4]. Only considering from the aspects of sea state environment, there are two factors resulting in the low RMSE.…”
Section: Data Processing and Analysis With The Algorithmssupporting
confidence: 70%
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“…The β parameter obtained from the ACMB algorithms is different from the LSMB algorithm, which may be one reason for the results of the ACMB and LSMB are different obviously. The RMSE of 24.8° is low compared the results given by [6,10,11] and close the mean difference 20° by Huang et al [4]. Only considering from the aspects of sea state environment, there are two factors resulting in the low RMSE.…”
Section: Data Processing and Analysis With The Algorithmssupporting
confidence: 70%
“…Both theory simulations and experiments confirm that the ratio of spectral power density of the positive and negative Bragg peaks is highly sensitive to the wind direction and so this can be used to extract wind direction [1][2][3][4]. However, for the monostatic radar, there exists a directional ambiguity as the radar cannot tell if the wind is from the right of the radar beam or the left.…”
Section: Introductionmentioning
confidence: 82%
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“…4. The response of the first-order radar cross sections to the change of wind direction has been explained in, for example, [23]. The barge motion peaks behave similarly as the Bragg peaks.…”
Section: Simulation and Discussionmentioning
confidence: 99%
“…Of course, the well-known Hasselmann term arising from a single scatter from second-order ocean waves may also be significant, and it will be considered in a related publication on the second-order spectrum. Having specified the time-varying scattering surface, the next step in deriving the desired cross section requires the determination of the an autocorrelation of the electric field (see [3] or [8] for example) whose form is given by (23) in which the receiving antenna area where is the gain of the receiving antenna, is the time shift between measurements, and indicates complex conjugation. Applying this to (20) gives (24) If we assume the motion of the antenna is independent of the sea state at the remote scattering "patch," then (25) A Fourier transform of (25) with respect to gives the received Doppler power density spectrum It will prove convenient to express the power spectral density for first-order gravity waves (see, e.g., [16]) in generalized form as…”
Section: E Pulse To Pulse Time Variation and The First-order Cross Smentioning
confidence: 99%