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- W2056251911 abstract "This paper describes the use of a conventional X-band radar in determining wave direction characteristics in coastal waters. It is shown that under suitable environmental conditions it is possible to determine a mean wave direction to within an estimated ± 2° and to observe wave refraction and diffraction processes in the vicinity of harbours and on open coastlines. It is also shown that the radar may be used to estimate wave periods and the use of the radar in determining the “annual” wave direction characteristics for a specific location is discussed. Examples of radar imagery are given together with technical details of the radar installations and equipment. Experience in the use of the radar at different sites and on different range settings suggests that the optimum height for the scanner, in this particular application, is in the range 15–20 m above mean sea level. Observations with the radar have been made simultaneously with measurements of the wave height, wave period and wind speed. It has thus been possible to establish some lower limits for the detection of swell waves by radar. In particular it has been found that about 80% of the waves not seen by the radar occur at wind speeds of less than 5 m s−1 and have significant wave heights of less than 1 m. These results are discussed in relation to the mechanism of wind wave generation and Bragg scattering from the sea surface." @default.
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- W2056251911 date "1979-01-01" @default.
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- W2056251911 title "Wave direction estimates in coastal waters using radar" @default.
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- W2056251911 doi "https://doi.org/10.1016/0378-3839(79)90027-9" @default.
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