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样例:粤西长期海流观测揭示的低频流特征及其动力机制分析

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     对粤西茂名竹岛附近海域单点系泊处2000年11月～2001年10月ADP海流观测资料、风场观测资料和多站海流同步周日观测资料进行了统计分析,统计结果表明,该海区天文潮潮流主导方向是ESE—WNW,属不正规半日潮流,最大可能潮流小于50.0cm/s。低频海流中,西向流是全年的主要趋势,无论冬、夏季,西向流的发生频率与强度都大于东向流的频率与强度。全年各月实测海流的最大值,表层在72.7～141.4cm/s之间;中层在 55.8～135.6cm/s之间;底层在41.0～113.2cm/s之间。各月各层最大流速的方向都集中出现在SW～WNW的4个方位,其中以WSW 向的出现频率最高,各月极大流速值主要受到低频流控制。

错误译文

    Statistical analyses are carried out based on the data, which come from the ADP current meter and wind sensor mounted on the single-point mooring pontoon near the Zhu Island, West-Guangdong coast during the period of November 2000 and October 2001, and come from the multiple-station one-day synchronous current observations. Statistics shows that the astronomical tidal current is of an irregular semi-diurnal one; the leading direction of it is ESE-WNW; and the maximum possible current speed is less than 50.0cm/s. About the Low-frequency flow, the westward flow prevails around the year. The occurrence frequency and strength of the westward current are greater than those of the eastward current, no matter when in winter or in summer. The extreme current speed in each month of the year is 72.7cm/s to 141.4cm/s for the surface layer; 55.8 cm/s to 135.6cm/s for the middle layer; and 42.6 cm/s to 113.2cm/s for the bottom layer. The directions corresponding to the extreme current speeds for different layers and different months concentrate in SW to WNW, with the highest frequency in WSW. The extreme current speed for each month is controlled mainly by the speed of low-frequency flow.

修改后译文

     Statistical analyses are carried out based on the data from the ADP current meter and wind sensor mounted on the single-point mooring pontoon near the Maoming Zhu Island of West-Guangdong coast during the period from November 2000 to October 2001, and the data from the multiple-station full-day synchronous current observations. Statistics shows that this area’s astronomical tidal current is of an irregular semi-diurnal one with the leading direction of ESE-WNW and the maximum possible current speed of less than 50.0cm/s. As for the low-frequency flow, the westward flow prevails all around the year. Either the occurrence frequency or intensity of the westward current is greater than those of the eastward current, no matter in winter or summer. The maximum current speed in all months of the year is between 72.7cm/s and 141.4cm/s for the surface layer, 55.8 cm/s and 135.6cm/s for the middle layer and 42.6 cm/s and 113.2cm/s for the bottom layer. The directions corresponding to the extreme current speeds for different layers and different months concentrate in the four directions from SW to WNW, with the highest frequency in WSW. The extreme current speed for each month is mainly controlled by the speed of low-frequency flow.

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